2008 EXPLORATION REPORT

on the

EL SOL IRON PROJECT

Northwestern Ontario NTS 52K/15, 52K/16

92˚ 15” West 50˚ 45’ North

for

RAYTEC MINING CORPORATION

(now LION ENERGY CORPORATION)

November 20th, 2009 J. Fingler, M.Sc., P.Geo

J. Fingler Geological

TABLE OF CONTENTS Page

1. SUMMARY............................................................................................................................................................................................ 1

2. INTRODUCTION ....................................................................................................................... 4

3. PROPERTY DESCRIPTION AND LOCATION ................................................................... 5

4. ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY……………………………………………………………............................. 9

5. HISTORY...................................................................................................................................... 10

6. GEOLOGICAL SETTING ........................................................................................................ 16 6.1 REGIONAL GEOLOGY ....................................................................................................... 16 6.2 PROPERTY GEOLOGY ....................................................................................................... 18

7. DEPOSIT TYPES........................................................................................................................ 24

8. 2008 EXPLORATION PROGRAM.......................................................................................... 25 8.1 GROUND GEOPHYSICAL METHODS and RESULTS……………………………… 26 8.2 DIAMOND DRILLING METHODS.................................................................................... 27

9. DIAMOND DRILLING RESULTS ......................................................................................... 33 9.1 GEOLOGY RESULTS............................................................................................................ 33 9.2 ANALYTICAL RESULTS .................................................................................................... 36 9.3 BULK DENSITY-SG RESULTS ......................................................................................... 38 9.4 2008 DRILLHOLE SUMMARIES ....................................................................................... 40

10. METALLURGICAL RESULTS .............................................................................................. 49

11. QA-QC PROGRAM AND RESULTS ..................................................................................... 53

12. INTERPRETATION AND CONCLUSIONS ........................................................................ 63

13. RECOMMENDATIONS............................................................................................................ 66

14. REFERENCES ............................................................................................................................ 69

15. SIGNATURE PAGE ................................................................................................................... 71

CERTIFICATE .................................................................................................................................. 72

LIST OF FIGURES

Figure 1: Property Location .............................................................................................................. 7

Figure 2: Claim Holdings ..................................................................................................................... 8

Figure 3: Regional Geology ............................................................................................................... 17

Figure 4: Property Geology ............................................................................................................... 19

Figure 5a: Ground Geophysics-Total Field Magnetics (TMI) (in pocket) .......................................

Figure 5b: Ground Geophysics-Horizontal Derivative of TMI (in pocket) ......................................

Figure 6: Compilation of Results (in pocket).....................................................................................

Figures 7a-h: 2008 Diamond Drill Sections (in pocket) ...................................................................

Figure 8: Graph of TFe% vs FeMt% by Lithology .................................................................... 37

Figure 9a: Graph of Bulk Density, Specific Gravity vs TFe% ................................................... 39

Figure 9b: Graph of Bulk Density, Specific Gravity vs FeMt%................................................. 39

Figure 10: Graph of Fe% for Hicks vs Lurgi Composites ............................................................ 50

Figure 11a: Graph of QAQC Fe2O3 Lab Duplicates vs Originals ............................................. 56

Figure 11b: Graph of QAQC SiO2 Lab Duplicates vs Originals ..............................................56

Figure 12a: Graph of QAQC Fe2O3 Prep Duplicates vs Originals ............................................ 57

Figure 12b: Graph of QAQC SiO2 Prep Duplicates vs Originals ............................................ 57

Figure 13a: Graph of QAQC Fe2O3 Field Duplicates vs Originals ........................................... 58

Figure 13b: Graph of QAQC SiO2 Field Duplicates vs Originals ........................................... 58

Figure 14a: Graph of QAQC Standard Checks for Fe2O3 .......................................................... 60

Figure 14b: Graph of QAQC Standard Checks for Fe2++ in FeO.............................................. 60

Figure 15a: Graph of QAQC Satmagan Lab Duplicates vs Originals ........................................ 61

Figure 15b: Graph of QAQC Satmagan Prep Duplicates vs Originals ...................................... 62

Figure 15c: Graph of QAQC Satmagan Field Duplicates vs Originals...................................... 62

LIST OF TABLES

Table 1: Summary of Abbreviations and Units............................................................................. 5

Table 2: Status of Claim Holdings.................................................................................................... 6

Table 3: Property Stratigraphy ........................................................................................................ 20

Table 4: 2008 Diamond Drilling Summary ................................................................................... 27

Table 5: Stratigraphic Column of Drilled Sections ...................................................................... 34

Table 6: Average of Results by Lithology..................................................................................... 37

Table 7: Summary of Bulk Density-Specific Gravity Results .................................................... 38

Table 8: Composite Results for 2008 Drillholes........................................................................... 41

Table 9: Summary of Results for Davis Tube Feed...................................................................... 51

Table 10: Summary of Results for Davis Tube Products ............................................................... 52

Table 11: Summary of QA-QC Sampling ........................................................................................ 55

Table 12: Summary of Lab Standard Results for Iron.................................................................... 59

Table 13: Proposed 2010 Budget ...................................................................................................... 68

LIST OF APPENDICES

Appendix 1: Listing of Contractors and Services Used

Appendix 2: Statement of Costs

Appendix 3: Clearview Geophysics Ltd. Geophysical Survey Report

Appendix 4: SGS Lakefield Metallurgical and Analytical Report

Appendix 5: Diamond Drill Logs

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1. SUMMARY Raytec Metals Corp. (Raytec) recently underwent a name change to Lion Energy Corporation (Lion Energy). All references to Raytec, in this report, therefore apply to Lion Energy. The earlier nomenclature has been retained for continuity of reporting of results from several sources. The El Sol property is located approximately 68 kilometres northeast of the town of Ear Falls in Northwestern Ontario. Access to the property is along the Wenasaga logging road which heads northeast from Highway 105, near Ear Falls. The property occupies an area of 1024 hectares as four contiguous mineral claims on claim map sheet G-1734 (Avis Lake), within the Red Lake Mining Division. Raytec holds an option to acquire a 100% interest in the claim holdings of the project, from a group of five parties: Skyridge Consulting Inc., Jason Gigliotti, Negar Towfigh, Minegate Resources Captial Group Inc. and 1544230 Ontario Inc. (a company owned by P. English). Raytec may earn a 100% interest in the property within 3 years from the time of exchange acceptance, through a series of staged cash payments ($160,000), share issuances (1.25 million shares) and exploration work commitments ($3,000,000). The terms of the agreement allow for the purchase of a 2 % NSR to be bought by Raytec, as well. To date, Raytec has completed the total cash payment and share issuance obligations and two years of the required exploration expenditures. The rocks underlying the property lie near the contact between the Mesoarchean to Neoarchean metavolcanic terrane of the Uchi Subprovince, to the north, and the metasedimentary terrane of the Neoarchean English River Subprovince, to the south. The central part of the property is dominanted by a sedimentary succession of greywacke, argillite, conglomerate and iron formation, which is flanked by intermediate to mafic volcanics. The area has been affected by a minimum of four deformational phases, included three major folding episodes (D1,D2, and D4) and later (D5) ductile shearing related to the regional Sydney Lake Fault structure. Elements of these events are preserved as property and drillhole scale structures. The stratigraphy of the El Sol property is mostly EW and WSW-ENE trending, and is inclined steeply to the south. The claims are centered on an approximately four kilometre long trend comprised of two main panels of iron formation, and several smaller ones. The main zones, A and B, represent the opposite limbs of a D4 synclinal fold structure which converge to the southwest of Kesaka Lake. The smaller zones internal to this structure may be the remnants of D2 fold repetitions of the same iron formation horizon comprising Zones A and B. During the 1956-1957 seasons, the project was the subject of an aggressive exploration campaign which included geological mapping, geophysical surveying, trenching and diamond drilling. The historical results available from this work are mostly incomplete. A total of 33,998 feet (10,363 metres) was drilled in 67 drill holes, along the two main subparallel horizons of iron formation referred to as the A and B Zones. Zone A has been traced over a length of 12,800 feet (3900 metres), and Zone B has been traced over length of 6800 feet (2070 metres). Historical drillholes intersected vertical to steeply south dipping panels of iron formation which averaged 44 metres in thickness.

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Local increased thicknesses are due to folding. The iron formation is described as alternating cm to mm scale bands of fine grained magnetite and white to grey chert and jasper bands. Local silicate or sediment dominant bands are also common, and specular hematite is reported. Based on the results of this initial drilling program, H. Brodie Hicks (1958) calculated an “Ore Reserve” of 312 million tons at a grade of 31.1% iron (%Fe), to a depth of 1000 feet (305 metres). This historical estimate was prepared prior to the classification and the reporting requirements dictated by the implementation of the National Instrument NI43-101 standards of the Canadian Securities Administrators. There lacks sufficient background data from the original drilling project for the author to be able to attempt to classify the historical estimate according the NI43-101 standards. The estimate should therefore be considered historical in nature and cannot be relied upon. It is, however, referred to, as the author considers it to be relevant to current exploration planning for the project. Subsequent metallurgical testing in 1957-58, by Lakefield Research Ltd. (Lakefield) and Lurgi Gesellschaft fur Chemie (Lurgi), determined that most of the iron was contained within magnetite, and reported that a …“a final concentrate assay of 70.8% iron and 2.0% silica” was obtained from a grind of 100% passing -325 mesh. The concentrate was also reported to be relatively clean and lacked significant amounts of deleterious elements. The goal of the 2008 program was to test various aspects of the historic work through the following activities:

test the extent and width of part of the A zone, in the area of historic drill holes compare the iron grade of composites of iron formation with historical results characterize the iron formation with preliminary optimization testwork

(including grind and Davis Tube tests) and geochemical analyses

The location and strike extent of the A Zone was confirmed through ground geophysics and through the drilling of a total of 2301 metres in eleven holes. The horizon is vertical to steeply inclined to the south. Horizontal thicknesses of iron formation within the 10 holes easternmost drillholes, ranged between 42 and 68 metres. Local internal dilution was due to infolded sections of quartz porphyry and/or sediments. The 2008 drillholes encountered similar stratigraphy and facies of iron formation, as documented in historical work. Composite grades ranged up to 29.39% magnetic iron (FeMt%) over a drilled length of 131.85 metres, or a horizontal width of 68.30 metres. While the width and grade of iron mineralization within the 2008 drillholes varied with the proportion of internal dilution, the overall results were relatively consistent with those documented by Hicks (1958).

Similar to historical records, the 2008 analytical results and Satmagan determinations confirmed that iron mostly occurs at magnetite, with only minor local hematite and iron silicates. Davis tube tests of three grind products (-200, -325, -400 mesh) from 5 representative samples found that concentrates of 63.7% to 70.6% Fe, with good weight recoveries of 43.5% to 57.2% were possible. The results showed that while the liberation of the silicates from concentrates improved with finer grinds; however, the required grind times were long, to reach the target of 4% silica. It was suggested that other beneficiation methods could be tested, to reduce silica contents while reducing grind times and related costs.

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The combined results from historical work and the 2008 program, have demonstrated the potential of the property to host an iron resource which could generate a metallurgically desirable product. Iron mines are usually large scale operations, with an economy of scale that can overcome expensive transportation and processing. Marketing of a product, therefore, also depends on several resource factors which include the size and grade of the resource, as well as the characteristics of the ore. The tested strike and width extent of the iron formation on the El Sol property suggests that an open pittable resource would be relatively small, in comparison to global iron ore operations. Additional iron resources could be developed from other occurrences of iron formation in the vicinity, to provide infrastructure and marketing synergy.

A budget of CDN $1.5 million is proposed for the 2010 exploration program on the El Sol property. The program would include continued metallurgical testwork to determine an optimal benefication method and a second phase of exploration drilling and geophysics. This work would be best executed during the first quarter of 2010, to test the A and B Zone horizons under the lake and in areas of seasonally wet ground conditions. A minimum of 4000 metres of drilling should be focused on the central and western part of the A Zone, as well as on the B Zone. Additional drilling would be required for full definition of an iron resource.

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2. INTRODUCTION This report was prepared for Raytec Metals Corp. (now Lion Energy) by J. Fingler. It presents the results of the 2008 exploration program conducted on the El Sol iron project. Exploration activities included ground magnetic surveying, drilling of 2301 metres in 11 holes, and preliminary metallurgical testing. The objective of the program was to collect sufficient preliminary data to assess three aspects of the El Sol iron formation:

1) To investigate the general extent and thickness of the iron formation in a series of widely spaced drill holes along the A Zone.

2) To conduct initial analyses and metallurgical testing to obtain an overview of the chemical

characteristics and distribution of iron and silica, as well as possible deleterious elements, within the iron formation.

3) To conduct an initial metallurgical test program on 5 core samples, to investigate an

optimum grind for favorable iron and silica liberation, to determine preparation and analytical methods for future drill core samples.

UNITS AND CURRENCY This report documents the results of the 2008 exploration program, but also makes reference to compiled historical data. While the current program refers to metric units, historical information from both government and corporate exploration programs is documented in imperial units. Conversions of units from imperial, when warranted, are shown together with the original imperial unit. The currency referred to in this report is Canadian dollars. The geographical coordinates referred to in this report are UTM (Universal Transverse Mercator) based, using the datum of NAD 83, Zone 15. The units commonly expressed for samples of iron mineralization can be diverse and somewhat inconsistent. The below explanation of units used during this program is an adaptation from a report by R.Risto (2008) of Watts, Griffis and McOuat. Units described are listed in Table 1. The results for the 2008 program are based on samples which were analyzed by several methods to make determinations on the various species of iron present as oxide (magnetite and hematite), silicate (ie. amphiboles, chlorite), and carbonate (ie. siderite).

• Whole rock analysis (WRA) using XRF methods to determine total iron as Fe2O3 • Satmagan measurement of magnetite content • Acid Digestion and Potassium Dichromate Titration to determine Fe2++

From this information, total iron (TFe) is calculated from Fe2O3 by dividing the measured value by the wt % value (for Fe2O3) of 1.4295. In the metallurgical testing, SGS refers to this as Fe.

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The Satmagan method uses an electromagnetic field to measure the magnetic content (Mt%) of a sample. This may include iron contributions as Fe2+ and Fe3+ . If is assumed that the iron from magnetic sources is only ferric iron Fe3++ , the total iron from magnetite can be calculated as FeMt% by dividing by the wt% value (for Fe3O4) of 1.3812. From the acid digestion and titration, the ferrous iron Fe2+ as FeO is determined. From this result, Fe3+ can calculated by subtracting the Fe2+ value from the total iron obtained from the WRA. During the 2008 program, preliminary grind test and David Tube determinations were conducted on 5 of the drill core samples. The Davis tube procedure provides an estimate of the magnetite content (%Mt or %MtDT) by separation of the magnetic fraction from a sample pulp. The sample pulp is referred to as the Head sample, while the two resultant fractions from the procedure are referred to as a concentrate and tailings. The weight percent of the amount of material recovered in the concentrate is referred to as (%Wt (recovery) or %WtDT). The percentage of magnetic iron (%FeMt or %FeMtDT) can be calculated by multiplying the %Wt recovery by the %TFe, or %TFeDT, determined by XRF analysis of the magnetic concentrate. The original drilling program on the property was conducted during the late 1950’s. Sample results on drill logs from this program are indicated as %Fe. There is no documentation of the analytical method used; however, at this time, iron samples were typically analyzed for acid-soluble iron content (%SFe). Historical Fe% results are therefore assumed to be a determination of soluble iron. They are here within referred to as %Fe, to maintain continuity with the data as originally recorded. Soluble iron includes iron from oxide and hydroxide sources, but does not include iron from silicates. In the absence of significant hematite, limonite and carbonate content, it should closely approximate magnetic iron content (%FeMt), rather than total iron (%TFe).

TABLE 1: SUMMARY OF ABBREVIATIONS AND UNITS

Abbreviation Term % or Wt% Weight Percent

Head Non-concentrated material Concentrate Concentrated material (eg. Magnetic fraction)

Tailings Remaining non-magnetic fraction %TFe % Total Iron calculated from Fe2O3 of WRA %SFe % Soluble Iron determined for historical samples %Fe % Iron, Fe, TFe% and SFe%

%FeMt % Magnetic Fe, calculated from Satmagan %Mt, %Mt_SAT, %Mt_cal % Magnetite, measured from Satmagan

%Hm, %Hm_cal % Hematite, calculated by WGM %PFeOther, %PFeOther_cal % Proportion of Total Fe in Other Iron minerals, calc'd by WGM

%PFeHm, %PFeHm_cal % Proportion of Total Fe in Hematite, calc'd WGM %PFeMt, %PFeMt_cal % Proportion of Total Fe in Magnetite, calc'd by WGM

%PFeOther_n, %PFeOther_nor % Proportion of Total Fe (normalized) in Other Iron minerals %PFeHm_n, %PFeHm_nor % Proportion of Total Fe (normalized) in Hematite %PFeMt_n, %PFeMt_nor % Proportion of Total Fe (normalized) in Magnetite

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3. PROPERTY DESCRIPTION and LOCATION The El Sol Iron project is located approximately 100 km east of Red Lake and 68 km northeast of Ear Falls in Northwestern Ontario (Figure 1). The property is centered at 92o 15’’W longitude, 50o 45’N latitude and UTM (NAD83 zone 15 datum) coordinates of 542200 mE 5644200 mN. The property straddles the 52K/15 and 52K/16 national topographic map sheets (NTS). The project occupies an area of 1024 hectares as four contiguous mineral claims on claim map sheet G-1734 (Avis Lake), within the Red Lake Mining Division (Figure 2). The westernmost three claims were the subject of the original agreement and the easternmost claim was staked and recorded during this program. These claims are all currently recorded in the name of Mr. Perry English. The three original claims are in good standing until May 2nd, 2012; however claim KRL 4241201 requires work assessment to the minimum value of $ 6,400 to be applied before the anniversary date of October 17th, 2010. The status of the claims, as shown in Table 2, shows the date the claims will be good until, assuming the acceptance of eligible assessment credits. Mr. English has authorized Raytec Metals Corp. and representatives of Raytec to act as agents on behalf of the collective owners of the property, and to file relevant assessment reports.

TABLE 2: STATUS OF EL SOL PROPERTY HOLDINGS

CLAIM # UnitsArea

HectaresDate

RecordedDate

Good To** Work Total

Work Applied

Work Reserve*

KRL 3019665 16 256 2-May-2005 2-May-2016 $ 69,444 $ 32,000 $ 40,425 KRL 3019666 16 256 2-May-2005 2-May-2016 $ 147,569 $ 32,000 $ 117,123 KRL 3019667 16 256 2-May-2005 2-May-2016 $ 651,041 $ 32,000 $ 582,195 KRL 4241201 16 256 17-Oct-2008 17-Oct-2015 $ - $ 38,400 $ -

** Date Good To is pending acceptance of assessment filing* Work Reserve amount includes pre-existing reserve in bankWork applied to KRL 4241201 from KRL 3019667 (contiguous claims)

Raytec (now Lion Energy) holds an option to acquire a 100% interest in the claim holdings of the project, from a group of five parties: Skyridge Consulting Inc., Jason Gigliotti, Negar Towfigh, Minegate Resources Captial Group Inc. and 1544230 Ontario Inc. (a company owned by P. English). Raytec may earn a 100% interest in the property within 3 years from the time of exchange acceptance, through a series of staged cash payments ($160,000), share issuances (1.25 million shares) and exploration work commitments ($3,000,000). The terms of the agreement allow for the purchase of a 2 % NSR to be bought by Raytec, as well. To date, Raytec has completed the total cash payment and share issuance obligations and two years of the required exploration expenditures.

There are no surface owners within the claims area and hence a “Notice of Intention to Perform Assessment Work” was not required. The claims lie within the Lac Seul First Nation traditional territory (Treaty 3). Raytec provided the Lac Seul First Nations band with advance notice of its exploration plans.

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4. ACCESS, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE and PHYSIOGRAPHY

The El Sol property is located approximately 68 kilometres northeast of the town of Ear Falls in Northwestern Ontario (Figure 1). Access to the property is along the Wenasaga logging road which heads northeast from Highway 105, near Ear Falls. At 70 kilometres along the road, immediately past a radio tower, a forest access road heads off to the east for about 3 kilometres. A cut trail beyond this road continues about 5 kilometres to the northwest side of Kesaka Lake (Figure 2). Further along Wenesaga road, a right turn along Maskooch road leads to a broad clear cut area which is suitable for staging of equipment and supplies into the property by helicopter.

The property is also accessible by float plane from the towns of Ear Falls and Red Lake. Kesaka Lake, in the western part of the property, is very shallow but a small plane such as a Cessna 180 can land there. Jean Lake (formerly Crossley Lake), on the eastern side of the property is deeper and can be accessed by larger float planes. During this program, a helicopter was used to move crews and supplies. Some drilling supplies were also transported by truck to a staging area 4 km to the north of the property and were slung in by helicopter as required. Winter access into the area may allow a camp site to be established closer to the property. The El Sol property is situated between two major drainage systems along the Wenesaga River, to the north, and the Papaonga River, to the south. Throughout the area, the maximum relief is 100m with normal variations less than 30m. The property is centered on an east-west trending creek and flanking bog area between Kesaka and Jean Lakes. The central and southern part of the property area is dominated by marsh and spruce bog with very limited outcrop. To the west and north, the topography rises into a series of isolated outcrop mounds and broad deposits of coarse glacial debris. Outside of the central marsh, the property is treed with mostly spruce, poplar and aspen, with low lying shrubs and moss cover. A dense stand of immature spruce is dominant in the western area of the property. The physiology of the area consists of ridges of gravel, boulders and rock which separate low lying drainages and muskeg swamps. Diamond drill hole records indicate that overburden varies from 1 to 3 metres in the northern part of the area and from 3 to 10 metres in the southern part. Overburden type is variable from organically derived muskeg and peat deposits to glacial and lacustrine clay, sand and gravel deposits and local metre scale erratics. To the northeast of Kesaka Lake, a series of transverse glacial moraines trend northwesterly into a logged area off Mascooch Road. The climate of northwestern Ontario is mid latitude continental. Summers of moderate to hot weather extend from May to October, with moderate rainfall. Winters are cold and receive substantial snow, but also allow easier overland access over frozen terrain. The close location of the property to the town of Ear Falls is favorable as a source of several resources. The hydro power dam at Ear Falls was recently upgraded and could provide a link into the provincial grid.

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5. HISTORY (adapted from Hicks, 1958 and Bowen, 1984) The history of the El Sol property is based on a report by H.Brodie Hicks (1958), compiled information reported by R.P.Bowen (1984, 1989) and additional records available through the Ontario Assessment Files and the office of the Resident geology in Red Lake, Ontario. The first detailed geological study of the area was undertaken in 1938 by J.D. Bateman, for the Ontario Department of Mines (Bateman 1940). In 1959, an airborne magnetic survey was undertaken jointly by the Ontario Department of mines and the Geological Survey of Canada. A series of aeromagnetic maps were published in 1960. In 1975, the map area south of 51 degrees North latitude was included in a helicopter reconnaissance mapping program by the Ontario Division Of Mines and is published as Preliminary Map P 1200 (Breaks et al.1976). In 1980, geological mapping of the Slate Lake area at a scale of 1 inch to ½ mile (1:31,680) was completed by R.P. Bowen of the Ontario Geological Survey. The results of this work were published in 1984 as OGS Open File Report 5471 and in 1989 as OGS Report 256 and Map 2517. HISTORICAL EXPLORATION Recorded exploration in the area of the El Sol project began during 1955-1956 when Capital Lithium Mines Ltd., a company controlled by Continental Mining Exploration, began appraising other resources to support their lithium deposit. An 800 square mile (2000 sq km) airborne magnetic and electromagnetic survey funded by the company detected several anomalies which were staked and assigned to various companies. The claims of the El Sol property were acquired in 1956 by El Sol Gold Mines Ltd. (El Sol Mines), as one of five of their iron exploration projects in the region. The original holdings of 124 individual, 40 acre mining claims, covered a much larger area than the current property. Newkirk Mining Corporation Ltd. (“Newkirk”) has been reported as taken over by Continental Mining in 1957 and contracted Aeromagnetic Surveys Ltd. in 1956 to conduct an airborne magnetic survey over a 172 km x 1.6 km area which included the El Sol property. The survey detected several anomalies of interest and additional claims were staked to cover these prospective features. Continental was then taken over by Augustus Exploration Ltd. in 1957. Most of the historical exploration on the property was conducted by El Sol Mines and during the late 1950’s, sufficient work was done to bring 124 contiguous claims to lease. The company contracted the Geo-Technical Development Company Limited to assess the property through geological mapping, ground magnetic and dip-needle surveying, surface sampling and trenching. This work was focused on 67 claims of the original group. The property-wide ground magnetic surveys detected 7 zones of possible iron formation within an east-west trending corridor straddling Kesaka and Crossley (Jean) Lakes. The most prominent of these features are the A and B Zones, which both trend parallel to the eastward regional trend of the underlying geological units. The A Zone is an east-west trending horizon which extends over a 13,200 ft (4023 m) strike length from the western shore of Kesaka Lake, to Jean Lake, in the east. The B Zone is a parallel horizon located between 500 to 1800 m south of the A Zone.

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It extends eastward over a 7200 ft (2195 m) strike length from the southwest corner of Kesaka Lake. A series of smaller Zones C,D,E,F and G, ranging between 600 to 1500 ft (183-457 m) in length, were also detected between the A and B Zones. Two much smaller anomalies, H and I, were also detected to the northwest of the A Zone at Kesaka Lake. Small surface exposures of the A Zone iron formation were mapped near the northwestern shore of Kesaka Lake. In 1956, a channel sample was cut across one of the exposures and composited sample results returned 31.74 % Fe over 26.5 feet (8.08m), with check assays of 31.8 % Fe. A broad area was trenched and blasted across the A Zone horizon, to the west of Jean Lake. A 50 ton bulk sample was extracted and stored at the western shore of Jean Lake. There is no record of results from this sample. During the winter of 1956-1957, the extent of the A and B Zone horizons were tested by a total of 33,998 feet (10,423 m) of drilling in 67 holes. Most holes were drilled on 400 foot (122 m) spaced sections, at inclinations of -45°, and all but 1 hole was drilled to the north. Multiple holes were drilled along selected 200 foot spaced sections, as well. The holes were mostly 400 to 600 feet (122-183 m) long , with 2 steeper inclined holes greater than 1600 feet (488 m) long. The vertical depth drilled was typically 250-300 feet (75-90 m). Subsequent to the initial drilling campaign, a historical mineral resource estimate was completed by H. Brodie Hicks, and various mineralogical, metallurgical and engineering studies were undertaken. The original analyses for samples from the program were completed by Thomas Heys and Sons, Toronto. While the results are sporadically reported on drill logs, no methods are described. Brodie Hicks based his calculations on these numbers, but noted that 13 samples of the samples which were also analyzed by Lurgi Laboratories returned iron values averaging 4.1% higher. In 1958, H. Brodie Hicks, P.Eng., prepared a preliminary engineering study for the property and calculated a historical mineral resource estimate of 312 million tons (284 million tonnes) grading 31.1% iron, to a depth of 1,000 feet (305 metres). The maximum vertical depth was encountered by the 2 deeper drill holes along the trend. Hicks used a tonnage factor of 312,550 tons per vertical foot in his tonnage estimate and suggested a mining scenario combining open pit and underground mining to depths of 400 feet (122m) and 1000 feet (305m), respectively. This estimate was prepared before implementation of the standards of National Instrument (“NI”) 43-101 and should not be relied upon. The specific data used to calculate these tonnages and grades is incomplete and/or not available and has not been confirmed by Raytec. A Qualified Person has not done sufficient work to classify the historical estimate as current mineral resources under NI43-101. Raytec therefore is not treating the estimate as current mineral resources as defined by NI43-101, but considers the information to be relevant to exploration of the property.

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METALLURGICAL TESTING

Metallurgical results were reported by H.U. Ross, in January 1957, for preliminary tests conducted for Newkirk Mining. The 4.5 kilogram sample was believed to have been of obtained from surface exposures. Two grind products (100 and 200 mesh) from a Braun disc pulverizer were passed through a Davis Tube Magnetic Separator to yield a concentrate, a middling and a tail, using different electric current intensities to adjust the magnetic strength and using different treatment times. The results, while preliminary, indicated that the grade for the rough concentrate did not improve appreciably by removing middlings. Iron recovery was very good, at 95%. These results suggested that iron was present mostly as magnetite, rather than hematite or limonite. Ross (1957b) indicated that a finer grind could improve results, however, and that better results could be obtained by successive screening and regrinding of the oversize.

In a second round of tests supervised by Ross, three composites from 8 drill core samples were subjected to Davis Tube separation tests as in the previous study, with screen analyses of the resulting concentrates. Concentrates were analyzed for iron and silica. Tailings and head samples were analyzed for iron only. The results indicated that a finer grind was warranted to lower the SiO2 content to desirable levels. Iron recoveries (>95% and >85%) and weight recoveries (>50% and >44%) were both very good.

More extensive metallurgical testing on large volumes of sample rejects from diamond drilling was subsequently performed by Lakefield Research Limited (Lakefield) of Lakefield, Ontario and Lurgi Gesellschaft fur Chemie (Lurgi), of Germany.

At Lakefield, the combined assay sample rejects from 7 drillholes (ES056-01,02,11,13,14,16,18) were stage crushed to -10 mesh, mixed, quartered and riffled into 4000 gram samples. An analysis of a composite head sample returned the following results:

Fe % (total) 33.86 %

SFe % (acid soluble) 31.20 % Cu % 0.016 % S % 0.260 % P % 0.084 %

TiO2 % 0.210 %

Lakefield reported that two test samples were crushed to different finenesses (100 and 200 mesh) with a ball mill and were concentrated with a wet-belt magnetic separator +/- Wilfley shaking table. Three and four cleaning operations were used for the tests, and the field intensity was decreased with the finer grind test.

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In Progress Report #2, the results of the second, finer grind test with lower field intensity and four cleanings showed that at despite a low recovery, the final concentrate was only 58.8% SFe, or 80% magnetite. Wyslousil (February, 1957) suggested that additional cleaning could bring the grade to over 60% SFe. Microscopic review of the products indicated the presence of several middling particles of mixed gangue-magnetite which could account for lower recoveries of soluble iron. Wyslousil suggested that grinding to much finer than 325 mesh may be required to obtain complete liberation. Further investigations were recommended, to assess: (1) finer primary grinding (-200 mesh) (2) finer grinding of primary concentrate (-325 mesh) and (3) flotation to remove siliceous gangue from the final concentrate.

It was also noted that the treatment of fine ore on the wet separator belt was more difficult than coarser ore. With the finer grind, the concentrate contained free gangue, and fine magnetite tended to pass into the tailings. This resulted in lower grades and recoveries. Additional tests documented in Progress Report #3 (April, 1957) focused on variables associated with the magnetic separator: It was found that the speed of the belt and the rate of feed were important factors for improved success. For these tests, the same assay rejects as in the test for Report #2 were used. The results of the tests indicated that an improved concentrate grade of 63.18 % SFe with a recovery of 83% was possible with a 200 mesh primary grind, wet separation and a deslimed, reground -325 mesh concentrate which was subjected to 2 stages of cleaning with slow flow rates of feed. The retreatment of the primary tailing and the first cleaner tailing improved recovery significantly.

In Progress Report #4, three variable grind time tests were conducted on the same sample material, to compare the resultant grade of concentrates. Grinding times varied between 40 and 80 minutes and the products were then treated as in the previous tests. The tests indicated that while the concentrate grade SFe% increased with finer grinding of the ore, the concentrate still did not exceed 64%, with feed finer than 10 microns. Such grinding times were 4 times longer than that needed to yield 95% +200 mesh and would result in excessive grinding costs.

The intimate association of magnetite and gangue was again confirmed from this test. Investigations are recommended to test the following treatment of the ore: grind the ore to 90-95% -200 mesh, do magnetic separation and treat the concentrate by flotation to remove the silica. Another test is recommended with the concentrate passed through a demagnetizing coil before each stage of retreatment on the separator (Wyslousil, June 1957)

Between July and November 1957, Lurgi conducted extensive reviews which included microscopic reviews of polished thin sections, Davis Tube separation tests to generate concentrates, and pelletizing tests on these concentrates. The samples provided for these studies consisted of 725 assay office rejects representing 6,900 feet (2103 metres) of diamond drill core with a total weight of 4,750 pounds (2155 kilograms). Although is not mentioned in legible sections of the report, the tests appear to have been completed on 40 different composites derived from drillholes on the property. The numbering of these samples is assumed to indicate the source drillhole.

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Brodie Hicks (1958) indicated the following excerpts from the Lurgi (1957) reports on Davis tube separating tests: that “… magnetite is the primary iron-bearing substance which, when grinding raw ore to 100% -325 mesh can be enriched with concentrations of 70% or more. The obtainable iron recovery differs due to the portion of hematite or ferrous hornblendes…”, also that “…final concentrate assay was 70.8% iron and 2.0% silica and pellets assay 68.39% iron and 2.2% silica. Grind was 100% -325 mesh.” Mineralogical reports suggest that “The examined ore samples almost exclusively contained magnetite as a recoverable iron-bearing component…88-90% of the Fe could be recovered.”

These historical metallurgical results suggested that a premium product could be generated from magnetic concentration of the magnetite feed and subsequent pelletization. About 85-90 % of the iron could be recovered with a concentrate grade in the order of 70 % iron. El-Sol Gold Mines Limited subsequently became controlled by Augustus Exploration Limited in 1962 and was reorganized as Tex-Sol Exploration Limited in 1964. Limited engineering reviews of mining and transportation scenarios for the project were later conducted during the 1960’s. No further assessment work was applied to the holdings since this time and all leased claims were allowed to lapse. RECENT EXPLORATION Three mineral claims of the current property were staked in 2005, to cover much of the iron formation explored by previous workers. During the early winter of 2007, a brief program of outcrop stripping and trenching was conducted in two areas to the west of Kesaka Lake. The program failed to expose iron formation.

Raytec Metals Corp. optioned the property in November 2007. A program of linecutting and ground geophysics was conducted during the early summer of 2008, to ground truth the extent of El Sol iron formation. The results of this program have been previously documented in an assessment report by G. Allen (2008), who supervised the program. Progress was delayed by poor weather conditions which made access challenging. A total of 68.5 kilometres of linecutting was completed by personnel of Ackewance Exploration Services Ltd., of Red Lake, Ontario. A 4.5 kilometre long baseline was centered on the property, between the two main iron formation trends, and a 100 metre spaced cut lines with 25 metre stations were cut north-south, to the property boundary. Portions of the central grid were not completed due to time and access limitations. Dan Patrie Exploration Ltd. was contracted to conduct GPS surveying of grid stations, and ground magnetic and VLF-EM surveying along 58 kilometres of the cut lines. The UTM coordinates of the picketed stations of the lines were also collected for spatial plotting of the geophysical data. The surveys were carried out using a Scintrex Envi combined magnetometer and VLF-EM receiver. The VLF-EM survey collecting readings using both the transmitter at Cutler, Maine, USA (24.0 hz) and the transmitter at Seattle, Wash., USA (24.8 hz). At all stations transmitters, both the in-phase and out-of-phase (quadrature) of the resultant electromagnetic field were measured. Processing and imaging of the data was conducted by Roman Tykajlo.

15

The proton procession magnetometer used during this survey is not accurate in areas of high magnetic gradient such as at the El Sol property. The instrument identified a series of magnetic lows, which represent reversed polarity. The analytical signal of the total magnetic field gives a closer approximation to axes of magnetic highs; however data issues with both the widely spaced grid and station coordinates were encountered. It was therefore recommended by R. Tykajlo that better and more accurate positioning and collection of magnetic data could be obtained from a continuous reading “walking magnetometer” (such as a cesium vapour or an Overhauser GEM GSM-19). The total magnetic field results defined linear trends of high magnetic susceptibility, which converge to the southwest of Kesaka Lake. The trends generally outline the distribution of horizons of iron formation; however, the accuracy of the magnetic lows and axis of the analytic signal was uncertain. A series of short length VLF-EM conductors were mapped by the survey. Some appear to be closely coincident with sections of the iron formation, while others do not. The response could reflect areas of conductive magnetite within the iron formation and/or argillaceous interbeds.

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6.0 GEOLOGICAL SETTING

6.1 REGIONAL GEOLOGY (adapted from R.P.Bowen, 1989) The El Sol Iron Property lies near the interface between two geological domains referred to as the Uchi Subprovince and the English River Subprovince. Rocks representative of both of these Archean domains occur in the property area. The Uchi Subprovince, located mostly to the north of the property, is underlain by volcano-sedimentary sequences of the Birch-Uchi greenstone belt, as well as intervening granitoid plutons. The English River Subprovince, which comprises much of the area to the south, is underlain by a variably migmatized sedimentary flysch sequence which is cut by peraluminous and metaluminous plutons. A series of late to post-tectonic intermediate plutons of sanukitoid affinity cut the successions of both subprovinces, near their boundary. The regional geology of the area is shown in Figure 3. The Birch-Uchi greenstone belt is dominated by the Confederation volcanic assemblage within which, three cycles of volcanism have been defined as arc-like tholeiitic to calc-alkaline sequences of mafic to felsic rocks. Each sequence has been interpreted to be separated from each other by east-ward-dipping thrusts or high-angle reverse faults (Rogers, 2002). The English River assemblage consists of quartzo-feldspathic, pelitic, and migmatitic rocks that represent variably metamorphosed wacke and mudstone with local iron formation. Migmatitic rocks include metatexite (<70% melt segregations in pelitic layers), inhomogeneous diatexite (70-90% partial melt segregations) and homogeneous diatexite (90% granitic leucosome). The latter unit forms garnet-bearing plutons and cordierite-biotite granitic bodies. The metasedimentary rocks of the assemblage are cut by a series of younger, 2698 Ma, gneissic dioritic to granodioritic stocks and batholiths that have been affected by both regional metamorphism and deformation. In the southern Uchi Subprovince, successive events of deformation and plutonism generated a series of semi-continuous panels of supracrustal rocks as domal structures within a broad tonalitic domain. These interleaved panels represent a transitional zone into the English River Subprovince, in the area of the property. There is neither a sharp change in rock type nor metamorphic grade across a major structure (i.e. Sydney Lake-Lake St. Joseph fault zone), as noted in other areas of the boundary. The Birch-Uchi belt has been affected by a minimum of two penetrative regional deformation events (D1, D2). Regional D1 fabrics are characterized by north trending folds and fabrics with a steep lineation. These are consistent with formation during a post-2372 Ma east-west shortening and near-vertical extension event. Regional D2 fabrics are characterized by east-northeast trending, moderately to steeply south dipping foliations, strong lineations, and local parallel deformation zones. The El Sol property lies on the southern limb of a regional D2 synformal fold.

17

FIGURE 3: REGIONAL GEOLOGY

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The main fabric forming event to affect the metasediments of the English River Subprovince and some of the southern Uchi Subprovince, occurred at ca.2691, during a period of metamorphism that reached up to granulite facies level and anatexis (Corfu et al., 1995). The most prominent fabric is east-trending, moderate to steep south-dipping foliation with a moderately east-plunging mineral lineation. These structures are considered to have developed in response to a (D3) post-collisional, subhorizontal south-directed thrusting event. All of the earlier formed structures and their related fabrics have also been locally deflected and warped during later stage emplacement of plutons of various suites. The entire volcanic-sedimentary sequence has been subjected to regional metamorphism. The grade of metamorphism increases in a southward direction, from lower greenschist to upper amphibolite. The felsic and mafic plutons have not been subjected to significant metamorphism; however, synvolcanic mafic dykes show signs of recrystallization. Near the contacts of the plutons, metamorphic grade is mainly albite-epidote-hornfels facies.

6.2 PROPERTY GEOLOGY (adapted from R.P.Bowen, 1989)

The geology of the El Sol property was first mapped in detail by El Sol Mines, as part of their 1956-1957 exploration program. The results of this work were subsequently incorporated into regional maps completed by government surveys. Descriptions of the geology, based on this work with additional field checks and analyses, were documented by Bowen (1984) in OGS Report 256.Since the entire succession has been metamorphosed, the suffix meta- has been omitted for all references to geological units. The property geology is shown in Figure 4.

The El Sol property lies within the boundary zone between the Uchi and English River subprovinces. The geology of the property preserves volcanic and sedimentary rocks for each of these domains, and late to post tectonic plutons which intrude them. The property is centered on an east-west trending corridor of narrow horizons of iron formation within a succession of pelitic and argillaceous sediments. This succession is flanked, to the north and the south, by panels of mafic to intermediate volcanic flows and volcaniclastic debris. Late to post-tectonic plutons cut the succession in the west (Tepeka Lake Stock) and in the southeast (Papaonga Lake Pluton). The current claim group is underlain by a sequence of clastic sediments with local horizons of iron formation, which are flanked by horizons of mafic to intermediate volcanic flows, volcaniclastics and amphibolite. The clastic sediments vary from wacke to arkose in composition and are locally intercalated with argillite and iron formation. Local formations of polymictic conglomerate have also been documented. The volcano-sedimentary succession generally trend northeastward to eastward in the western part of the claim group and trend eastward to southeastward in the eastern part of the claim group. The panels dip vertically to steeply south. The distribution of iron formation within the succession outlines an east-west trending fold structure which converges towards the southwest of Kesaka Lake. The gross repetition of stratigraphy from pelitic to argillaceous sediments with iron formation in the core of the structure flanked by intermediate and mafic volcanics to both the north and south, is consistent with a property scale synclinal fold structure.

Avis Lake

Lake

Jean Lake

Kesaka

M M

M

M

F

F

F

KRL 3019665

KRL 3019666

KRL 3019667

KRL 4241201

ES08-001

ES08-003ES08-004ES08-005

ES08-006

ES08-007ES08-008

ES08-009 ES08-010

ES08-011 ES08-002

540,000m.E

5,64

3,00

0m.N

5,64

5,00

0m.N

542,000m.E 544,000m.E 546,000m.E

540,000m.E 542,000m.E 544,000m.E 546,000m.E

5,643,000m.N

5,645,000m.N

RAY REV / RAY_05_Prop_Geol.cdrLast revision date: Thursday 26 November 2009

Graphics by Watts, Griffis and McOuat Limited Adapted from OSG Map 2517 (Bowen, 1980)

MetresUTM NAD83 Zone 15N

200 1,0000

Scale 1 : 20,000

N

LION ENERGY CORP.

El Sol Iron Project

Property Geology

Ontario, Canada

Figure 4.

Felsic Volcanics

Amphibolite

Mafic Volcanics

Iron Formation

Conglomerate

Granodiorite

Fault inferred

Syncline

Anticline

Property outline

M

F

Legend:

Intermediate Volcanics

Greywacke, Argillite

Diorite

2008 Drill hole

Historical drill hole

Zone nameA

El Sol IronProperty

A

B

C

D

E

F

GB

B

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Indicators of stratigraphic tops within mafic pillowed flows in the southern part of the property show younger lithologies to south. However, the succession drilled on the A and B zones, together with observed cross bedding in sediments near the iron formation indicates tops are to the south, along the northern limb and north, along the southern limb. Polyphase folding could explain for the apparent discrepancy between tops indicators. Table 3, below, presents a listing of lithologies identified on the property, as well as their relative position in the stratigraphy.

TABLE 3: STRATIGRAPHIC UNITS on the EL SOL PROPERTY (Does not imply order of units for intervals 6,5,4,1)

Code Unit Codes Used in Core Logging 8 BD Biotite Dyke BD

7 GD Granite or Aplite Dyke GD, AD

6b QPM Quartz Porphyry with Iron Formation IMCQP, QPM

6a QP Quartz Porphyry QP, QFP, QBP, QDP, QPBX

5g IFMR Magnetite+/-Chlorite Iron Formation + grunerite overprint IMCR, IMCLR

5f IFMS Magnetite Iron Formation + Sediment Interbeds

IMCLS, IMCS, ISMC, ICMS, ILSCM, ISMLC, ILSMC

5e IFMJ Magnetite-Jasper Iron Formation IMCJ, IMJC, IMJ, IMCJh, IMJCh, IMJ

5d IFM Magnetite Iron Formation IMC

5c IFML Magnetite-Chlorite Iron Formation ILMC, IMCL, IMCLJ, ICMLgt, ILMCgt, ICMLgt

5b IFLM Lean Iron Formation+/-garnet ILC, ILCM, ICMLgt, ILCMgt, ILSCM, ILCMS

5a IFL Silicate Iron Formation +/- sediment interbeds

ICL, ILC, ILCgt, ILS, ILCS, ISLC, GHS, HS

4e CONG Conglomerate CONG

4d ARG Argillite ARG, ARGc

4c GWK Greywacke BWK, GWK, GWKa

4b PG Paragneiss PG

4a QBS Quartz Biotite Schist QBS

3 FV Felsic Volcanics FV

2 IV Intermediate Volcanics IV

1a AMPH Amphibolite AMPH

1 MV Mafic Volcanics MV

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Along the southern edge of the property, there is an east-west trending sequence of pillowed mafic volcanics which is 200-300m wide. To the immediate north of the property, there is also a broad, 300m wide section of highly metamorphosed mafic to ultramafic volcanics. This corridor consists of coarse grained, garnetiferous amphibolite and a garnet-rich, banded unit, with alternating layers of amphibolite and feldspar-rich sandstone. Garnets up to 1mm in size are common, and locally form bands which are highly contorted. Bowen(1989) suggest that these units may have volcanic flow and volcaniclastic members as protoliths. Immediately south of the amphibolite, and in the northern part of the property, is a 500 metre thick section of intermediate volcaniclastics of tuff to tuff-breccia. Bowen described outcrop exposures of these rocks as light to medium grey, with 15-20% biotite. Primary bedding planes are discernable. Late veins and fracture-fillings of albite and epidote are common. The central part of the property is underlain by a broad section of clastic sediments and iron formation. The outer part of the fold structure defined by iron formation is considered to be the base of the sedimentary succession. Below the iron formation, the sequence is dominated by a coarser section of greywacke with local conglomeratic horizons. Thin, discontinuous horizons of argillite (grey to black) locally flank the iron formation, but are more common near its the base. Above the iron formation, the sequence becomes finer and consists mostly of greywacke and arkose. The conglomerate consists of lens shaped clasts of mostly mafic to felsic volcanics and sediments, within a wacke matrix. The local presence of iron formation clasts in conglomerate beds suggest they may be intraformational. Conglomeratic horizons are repeated within the succession and outline a series of isoclinal folds. Discontinuous, thin horizons of argillite (grey to black mudstone) within the greywacke flank the iron formation, but are more common nears its base. They occur as thin, submm laminae to 10cm beds, and are locally carbonaceous. With increasing metamorphic grade, local anatexis of the clastic metasediments has generated migmatitic textures. Such sections have been logged as paragneiss and quartz biotite schist, and are more common near Jean Lake and west of Kesaka Lake. The iron formation was first identified by airborne magnetic surveys and later defined by diamond drilling. It consists of 2 main zones and several smaller ones, which converge into an EW trending fold closure to the southwest of Kesaka Lake. The larger zone passing through the north end of Kesaka Lake is about 4000 m long (A Zone) while the one through the southern end of the lake is 2200 m long (B Zone). The unit is up to 85 metres thick. The iron formation is a meta-taconite of the Algoma type. It is characterized by alternating bands of magnetite and recrystallized chert +/- jasper, chloritic mudstone which range in thickness from sub-millimetre to metre scale. Internal variants are common, with varying proportions of the above four components: from silicate and lean iron formation, to magnetite-chlorite and magnetite jasper dominant types. The unit consists of fine grained argillaceous to medium grained granular magnetite bands which are interbedded with white to medium grey chert and jasper. Thin sections reviews indicated the presence of chlorite, hornblende, grunerite and hematite within the iron formation (Bowen, 1989, Lurgi).

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To the west and south east of the property, the volcano-sedimentary succession has been cut by the syn to post-tectonic Tepeka Lake stock and the Papaonga Lake, respectively. The Tepaka Lake stock is a small, oval shaped dioritic intrusive body. The Papaonga Lake Pluton is larger, and displays internal zoning which has been described as tonalitic to granodioritic in composition. Within the drilled sections, three varieties of pre- to syn-tectonic dykes cut the sequence: quartz porphyry (QP), lamprophyre (BD), granite to aplite (GD). The quartz +/- feldspar porphyry dykes occur as typically decimeter to metre scale dykes which mostly cut sections of iron formation along subparallel to parallel trends. Their intrusive contacts and internal cleavage are consistent with that of the host unit. The lamprophyre dykes are usually only decimeter scale, but also cut the iron formation along subparallel to parallel trends. The dykes are a distinctive grey-brown, strongly biotitic, and are loci for higher strain. The rocks of the El Sol property have been subjected to upper greenschist to amphibolite faces of metamorphism. The higher grade is recognized as the development of garnets and amphiboles within the northern amphibolite, and within chloritic mudstone of the sedimentary sequence. Elevated temperature and pressure conditions also generated concentrations of biotite and local migmatization of greywacke. STRUCTURE The area has been subjected to high levels of predominantly D2 or D3 ductile strain, resulting in property scale folding and strong cleavage development. Indications of strain are best preserved within bedded units such as conglomerate, argillite and iron formation. The observance of decimeter scale refolded folds in iron formation suggests that polyphase folding of several orders has occurred. Tight, isoclinal to asymmetrical folds and straight to attenuated bands of magnetite-chert indicate that the iron formation has been highly transposed. The plunge of these folds is generally steeply, to the west. This deformation is also recognizable in map patterns of the iron formation. With such high levels of strain, it is possible that the iron formation segments may be remnants of a semi-continuous horizon which has been fold repeated and subsequently stretched and attenuated. The vertical to subvertical dipping cleavage observed within dykes cutting iron formation is also parallel to banding and developed under the same strain conditions. The consistent emplacement of quartz porphyry dykes parallel to subparallel to magnetite-chert banding and their strong internal cleavage suggests these bodies were emplaced either before, or during this strain event, as well. There is little field evidence recorded for the presence of late brittle-ductile and brittle deformation. Minor narrow brittle-ductile shears zones were encountered in recent drillholes. However, several late structures along east-northeast and northwest trends can be interpreted from the recent magnetic survey data. Brittle faulting encountered at the base of a historic drillhole on the B zone may be one of these late structures.

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MINERALIZATION Historical programs of geophysics and diamond drilling on the property has outlined linear zones of magnetite bearing iron formation within a large scale, EW trending fold structure with a closure to the southwest of Kesaka Lake. Within this structure, a total of 7 zones (A to G) of high magnetic susceptibility were detected from airborne and ground magnetic surveys. The most prominent zones, A and B, were detected over lengths of 13,200 feet (4023m) and 7200 feet (2195m), respectively. Outcrop along the magnetic trends is mostly along the A Zone, where banded magnetite-chert iron formation is exposed along the western shore of Kesaka Lake. Bowen (1989) reported that a channel sample taken by the Geo-Technical Development Company returned a result of 31.74% Fe over 26.5 feet (8.1 metres). In 1980, the same channel was re-cut and sampled by Bowen. A similar result of 31.8% Fe and 0.02% P was reported. The extent of the A and B Zones has been previously tested with 67 drillholes. Estimated true widths for the iron formation ranged between 30 and 90 metres. Drill logs describe the unit as alternating, fine bands of magnetite and chert +/- jasper with local sedimentary interbeds of chloritic argillite +/- garnet, hornblende +/-garnet schist and quartz biotite schist. Specular hematite was noted in some intervals, as well. A large composite sample comprised of 69 assay rejects from the drilling program returned results of 33.86% Fe (total) and 31.20% Fe(acid soluble), with 0.26% S, 0.084% P, and 0.21% TiO2. From available results in diamond drill logs, Bowen (1989) calculated that within the iron formation, sulphur values range from 0.15 to 0.26%, P2O5% values range from 0.22% to 0.35% and SiO2 ranges from 45% to 47%. These results indicated the iron mineralization contains low levels of deleterious contaminants and is therefore relatively clean.

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7.0 DEPOSIT TYPES Banded iron formations (BIF) contribute more than 95% of the world’s iron resources. They are thinly bedded to laminated sedimentary rocks, of possible chemical or biochemical origin, which are dominated by iron-rich layers alternating with chert or quartz-rich layers. The mineralogy of the iron-rich layers is used to classify the BIF into different facies: oxide (hematite and magnetite), carbonate (siderite), silicate (greenalite, chamosite and glauconite), and sulphide (pyrite). Iron formation deposits range from a few metres to greater than 150 m thick and may extend laterally from a few kilometers to hundreds of kilometres. Due to the great extent of these horizons, iron ore mines are typically large scale, open pit operations which can remain in production for decades. Most are early to middle Precambrian in age and formed at a time when the earth’s atmosphere was relatively anoxic. They are considered to be chemically or biochemically precipitated, and potential sources of iron are thought to be derived from either erosion of nearby landmasses, from volcanic exhalations, or by leaching from euxinic sediments. Many BIF deposits have also been enriched by secondary processes such as weathering or hydrothermal activity. Two main subtypes of iron formation are recognized: Lake Superior and Algoma, based different depositional settings. Lake Superior BIF are typically intercalated with other sediments formed in a continental shelf environment, including quartzite, black carbonaceous shale, red shale, conglomerate, dolomite, massive chert, chert breccia and argillite. Common varieties are banded hematite (Hamersley in Western Australia), itabirite (Minas Gerais area in Brazil, Liberia and Venezuela), taconite (Mesabi Range in Minnesota, the Kursk region in Russia and Norway), jaspillite (Marquette Range, Michigan) and siderite (Michipicoten District in Ontario, Canada). Algoma BIF are found mostly in Precambrian greenstone belts and are associated with volcanogenic sediments of ranging from greywacke to volcanics. Iron and silica in this setting is thought to have been derived from volcanic effusive and hydrothermal sources along volcanic belts and deep fault or rift systems. The formation and distribution of these deposits were controlled by tectonic rather than by biogenic or atmospheric factors. Examples include: Helen Mine at Wawa, Sherman Mine at Temagami, Griffith Mine at Ear Falls and Lake St Joseph, all in Ontario, Canada; Woodstock in New Brunswick, Canada; and Kudrem UK in India.

Processing of the ore requires coarse crushing and screening, followed by rough crushing and grinding to a fineness at which a maximum amount of magnetite can be liberated from silica gangue. The resultant pulp is then passed under a magnetic separator to form a concentrate. This determines the energy inputs required to run a milling operation. Early stage evaluations are therefore focused not only on iron grade and tonnage, but also on metallurgical considerations such as coarseness of the magnetite and content of contaminents within the concentrate. Most magnetite BIF deposits must be ground to between 32 and 45 micrometres in order to provide a low-silica magnetite concentrate. The typical grade of iron at which a magnetite-bearing banded iron formation becomes of interest is about 25% Fe, as this may yield a 33% to 40% recovery of magnetite by weight, to produce a concentrate grading in excess of 63% Fe by weight. A desirable concentrate will typically have less than 0.1% phosphorus, 3–7% silica, less than 3% aluminium and titanium, and minimal sulphide content.

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8.0 2008 EXPLORATION PROGRAM The 2008 exploration program on the El Sol Project was conducted from September to November, 2008, but analytical work continued until June 2009. The activities included ground geophysical surveying, diamond drilling and preliminary metallurgical testing. Recommendations about field procedures, metallurgical testing, and analytical methods was provided by senior personnel of Watts, Griffis, and McOuat (WGM): R. Risto, M. Kociumbas and B. Neal. Preliminary commentary on the results of various stages of the optimization testwork was also provided. Senior Associate Geologist, R. Risto, made a field visit to the property while this drilling program was in progress. WGM is a Tononto-based consulting firm with demonstrated expertise in the evaluation of iron deposits. An earlier program (May-Sept 2008) of property wide line cutting and ground geophysical surveying was supervised by G. Allen. The results of this work have been previously documented in an assessment report, and are not repeated here. The objectives of this program were:

1) Assess and/or confirm the extent of iron formation along the A Zone, using new data compared with historical data sources.

2) Conduct preliminary metallurgical tests on selected core samples, to assess the optimum grind for desirable levels of liberation of iron and silica from the iron formation.

3) Characterize the iron formation and its component units, for the contents of total iron (TFe%), magnetic iron (FeMt%) and any potential deleterious elements within the horizon.

4) Conduct bulk density and specific gravity determinations for use in future resource estimations

5) Compare the above parameters with available historical results. 6) Establish a protocol for future exploration activities focused on resource definition.

The program consisted of compilation of historical results, ground magnetic surveying, diamond drilling, and preliminary metallurgical testing. The historical compilation was largely completed after the field activities, as limited data was available in advance. A ground magnetic survey was completed in late September, however, consultant R.Tkailjo, expressed concerns regarding the positioning of data and the limitations of survey instrumentation for an area of such high magnetic gradient. It was advised that a GPS controlled survey using different instrumentation would give a more accurate position of an anomaly related to the iron formation horizons. The field program was conducted from September 28th 2008 to November 28th, 2008. Drilling was conducted from October 1st to October 28th, 2008. The program was based out of a permitted camp at the South Bay Mine site, which was owned and operated by Ackewance Exploration Services. Access to the property and support for all drilling activities was provided by Forest Helicopters, of Kenora, Ontario. For reasons of both safety and time effectiveness (considering erratic fall weather and limited daylight), an A-STAR 350B2 helicopter was used for the duration of the program. A BC Level 3 First aid attendant was also contracted from 1984 Enterprises Inc., of Vancouver, BC.

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Ground geophysical surveying was conducted by Clearview Geophysics, of Toronto, ON. The survey was concurrent with diamond drilling and the results were used to help select drill sites. Post-survey processing of geophysical results was conducted by Kit Campbell of North Vancouver, BC. Diamond drilling was conducted by Hy-tec Drilling Ltd., of Smithers, BC and was supported by their operations in Red Lake, Ontario. Drill pads were cleared and built by personnel of CJ Enterprises Ltd., of Smithers, BC. Raytec personnel cut grid lines and access trails, and helped to build drill pads. DGPS surveying of drillhole collar locations was completed by E. Rody, O.L.S, of Kenora, Ontario. After completion of the drill program, the core was mobilized to Red Lake, Ontario, by Barrens Transport. Drill core was logged and sampled at a full equipped, permanent core shack which was rented from Premier Gold Mines Ltd. Drill core logging and geotechnical data collection were completed by Janice Fingler, P.Geo, and James Thurston. Drill core sampling and packaging was completed by Willy Desmeules of Ackewance. Samples were shipped by truck, with Gardewine, to SGS Mineral Services in Lakefield, Ontario. The remaining core in boxes was cross piled, secured and is currently stored at Barrens Transport, in Red Lake. 8.1 GROUND GEOPHYSICS METHODS and RESULTS Survey methods and data processing for the ground magnetic survey were documented in a logistical report by J. Mihelcic (2009) of Clearview Geophysics Ltd. Details are presented in Appendix 2. “ The Walking-mode magnetometer surveys were carried out using Scintrex SM5 NavMag magnetometers. The internal GPS from the NavMag was used for navigation and positioning. Readings were acquired at 1x per second. The magnetometer sensor was located on a vertical staff over 0.5 metres above the operator’s head. The GPS sensor antenna was located on a backpack carried by the operator. GEM Systems Overhauser magnetometers were used for the base station corrections. The base station magnetics data were real-time UTC stamped. They were located less than 15 km from the survey grids. Two base stations were running at all times at different locations on the grid. This was done so that a backup was available in case the main base station failed. All data were downloaded and transferred to a central Dell laptop computer. In-house and Geosoft software were used to convert and present the readings. The Cesium and Overhauser magnetometer clocks were synchronized to UTC time using their internal GPS receivers. Magnetic diurnal corrections were done with Geosoft’s Table-lookups. This application linked the files according to GPS acquired UTC time. Base station readings were taken at 1-second intervals. Straight-line interpolation was applied to the base station readings to match the coinciding field magnetometer readings.” Post-processing of the data was completed by Kit Campbell, of Intrepid Geophysics. Filtering transformations (in Fourier domain) generated secondary products with enhanced information content. The enhancements made to the data included vertical and horizontal derivatives, to produce anomaly contrasts over the peaks and edges of the formation.. Contoured images of both total magnetic intensity and horizontal derivative are show together with the interpreted iron formation surface trace, are shown in Figures 5a and 5b.

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8.2 DIAMOND DRILLING METHODS Before the start of drilling, the position of historic drillholes was estimated as a best fit from available maps and local grid coordinates on drill logs and sections. Data was derived from drill logs and sections. Information about drill hole specifics were preserved by these sources; sample data was not. Field checks conducted during this program located casing for drillhole ES57-032 off the north shore of Jean Lake. The bulk sample trench which was excavated along iron formation intersected by drillhole ES57-055 was found, as was the original iron formation outcrop for which channel sample results have been reported. These locations were used to adjust positions for the historical drillholes. Of a total of 67 historic drillholes, all but four holes interested iron formation. Sample results are indicated for 22 of 42 holes on the A Zone and 10 of 15 holes on the B Zone. Samples with results all reported %Fe values, while only some samples reported %SiO2, %P2O5 or %P and %S. There are no indications of analytical methods and there is no drill core available for review. Nevertheless, the available results provide a baseline to which the 2008 results may be compared. The 2008 program was planned at spaced intervals, to test previously drilled sections and to test to depth, within accessible areas. Optimum drill spacing or specific sites based on historic data could not be drilled due to boggy ground conditions to the south of the A zone within a wide margin around the creek joining Jean and Kesaka Lakes. A total of 2301 metres of NQ sized core was drilled in 11 holes, over a 3.5 week period. The distribution of drillholes is presented in a compilation in Figure 6 and details are presented in Table 4, below. Details regarding data collection, sampling and analytical methods are documented in the following section. Advice on sample preparation, analysis and metallurgical testwork was provided by R. Risto and M. Kociumbas, of WGM. WGM is a consulting firm with demonstrated expertise in the evaluation of iron deposits worldwide.

TABLE 4: SUMMARY OF 2008 DIAMOND DRILLHOLES DDH Easting Northing Elev_m Azimith Inclination Depth_m Started Finished

ES08-001 543883.28 5644407.72 407.56 355 -43.0 234.00 3-Oct-08 6-Oct-08ES08-002 543883.28 5644407.72 407.56 355 -58.0 291.00 6-Oct-08 9-Oct-08ES08-003 543624.34 5644484.14 410.38 358 -46.5 177.00 9-Oct-08 11-Oct-08ES08-004 543317.76 5644501.70 417.24 360 -45.5 171.00 11-Oct-08 13-Oct-08ES08-005 543317.76 5644501.70 417.24 360 -65.5 222.00 13-Oct-08 15-Oct-08ES08-006 543008.72 5644430.66 412.06 358 -45.0 234.00 15-Oct-08 17-Oct-08ES08-007 542803.30 5644581.14 418.04 179 -46.0 168.00 18-Oct-08 19-Oct-08ES08-008 542803.30 5644581.14 418.04 179 -59.5 228.00 19-Oct-08 21-Oct-08ES08-009 541791.32 5644248.96 418.76 360 -45.0 201.00 21-Oct-08 23-Oct-08ES08-010 541982.95 5644263.98 417.80 360 -46.5 189.00 23-Oct-08 24-Oct-08ES08-011 540810.00 5644265.62 429.20 180 -46.0 186.00 25-Oct-08 26-Oct-08TOTAL: 11 drillholes 2301.00 metres

Coordinates are in UTM NAD83 zone 15.

Eight holes (ES08-001 to -008) were drilled along five sections of the A Zone in the Kesaka Far East area, towards Jean Lake. Two holes (ES08-009, 010) were drilled along two sections at the Kesaka East area, located northeast of Kesaka Lake. One hole (ES08-011) was drilled in the Kesaka West area, approximately 100 metres off the western shore of Kesaka Lake.

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During the 2008 program, locations for drilling were selected to test widely spaced intervals along the A Zone. Due to widespread, boggy ground to the south of the A Zone, specific drill sites were limited to areas with suitable conditions to support a drill rig. Drill locations were spotted along approximate north-south trending cut lines. Sites were cleared and drill pads were built in advance. Drilling was conducted using a heli-portable Tech 500 rig which was moved and supported with an ASTAR 350 B2 helicopter. Mobilization was from logging roads in a clear cut area located 4 kilometres to the north of the property. The drill rig was positioned on elevated drill pads and aligned with two sighting pickets. The initial inclination of the drillhole was set using a carpenter’s inclinometer and was later checked by the geologist, with a brunton. Downhole surveys were conducted approximately every 50 metres, with a Ranger single shot downhole survey tool. Since the instrument was affected by the magnetic field associated with the iron formation, only measurements of inclination were accepted as valid. Drillcore was transported daily, from each drill pad location, by helicopter. Wooden core boxes were stacked, covered, and strapped into a steel caged basket which was slung back to camp each day on a long line. After each drillhole was completed, the casing entry point was marked with a 1 to 1.5 metre long cut log of a tree. A metal tag indicating drillhole details was attached to and photographs were taken of the site. A metal anchor rod remains at each pad location. DGPS surveying of 10 of 11 of the drillholes, as well as a located metal casing of historic drillhole ES57-032, was completed by surveyor Eric Rody, O.L.S, of Kenora, Ontario. All points were provided as UTM NAD83 zone 15 coordinates. A metal survey reference pin was installed at the easternmost helicopter pad. The coordinates of this pin are: IB (iron bar) 543767.403 metres East 5644429.645 metres North

410.138 metres above sea level UTM NAD 83 Zone 15

A base station was positioned at this point and a second roving unit was positioned at the marked hole collar location and/or anchor for the drillholes ES08-001 to -010. GPS signals in the area were difficult to obtain, due to the tall tree cover surrounding the drill sites, as well as the low trajectory of satellites over the areas. Long data collection times at each survey point were required to ensure data was within acceptable error limits. The corrected results of the ground points were provided in as a list from E. Rody. The “zero” mark of all downhole measurements was from the surface of the drill pad. The height of the pad was measured in the field and the location of this point was used as the elevation of the drillhole. Using the height of the pad and the surveyed location of the entry point on the ground, the coordinates were estimated. In the drill logs, and in the database, the base of the casing, therefore, indicates the ground surface.

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8.2.1 LOGGING and SAMPLING METHODS Core boxes were delivered daily from to the property to camp by helicopter, within a secure core basket. Core was checked for continuity between correctly placed metreage blocks. Any concerns or errors were addressed with the drill crew, and corrections were made, when required. Boxes were labeled with aluminum tags designating drillhole, box number and from-to intervals. Geotechnical logging of the core was conducted, measuring core intervals between approximate drill run blocks for % recovery and % RQD (Rock Quality Designation). Overall core recovery and RQD were both very good, averaging 98.6 % and 76.2 %, respectively. Core was then secured in stacks on a flatbed trailer and at the end of the drilling, was transported to Red Lake for core logging and sampling. Before being logged, drill core was oriented with banding and bedding (the main reference fabrics) inclined towards the up hole direction. This is consistent with documented vertical or subvertical trends for outcrop exposures and historic drilling. Core was logged for general lithology (Litho_gen codes) and structure. Selected sample intervals were also logged for detailed lithology (Litho codes) within these intervals. Estimates of the relative components of the iron formation (I) were made and coded in order of relative proportions: as magnetite(M), chert(C), chloritic mudstone (L), jasper (J) and sediment interbeds (S). The presence of garnets (gt) and grunerite (R) were also included in the coding. The groupings of the codes used are previously shown in the stratigraphic column of Table 4. Structural measurements for planar fabrics were made with zero being the plane perpendicular to core axis, with positive values being angles measured from zero to uphole directions and negative values being angle measured from zero downhole directions. A measurement of magnetic susceptibility was taken within each drill run interval using a KT-9 handheld unit. Due the high proportion of magnetite within the iron formation, readings taken within the iron formation mostly exceeded the detection limits of the instrument. Samples were laid out at mostly 3 metre intervals, but were also broken at unit boundaries at both shorter and longer intervals. Sample selected for in-field bulk density measurements were laid out at approximate 1 metre intervals. Samples submitted from the field included the insertion of regular(“REG”) samples, as well as QA-QC samples of a field blank(“FB”) and a field duplicate (“FDC”) which were each included within every 20 samples to be submitted for analysis. In the first few drillholes, 20 intervals of greywacke were sampled, assigned temporary numbers of B1-B20 and were put aside for insertion into the sample stream as blanks with numbers assigned from the main sample stream.

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Sample intervals and numbers were marked on the core with a red china marker. Sequentially numbered two part sample tickets, together with an aluminum tag containing sample interval information, were stapled into the box near the end of each regular sample. Tags for designated field blanks and field duplicate samples were included. Blank tags were positioned at the start of the sample they proceed, and the duplicate tags were placed after the sample they are to follow. Details about all samples submitted were recorded on the original drill logs. After samples were marked and tagged, the core boxes were photographed with core both wet and dry. A total of 429 samples were submitted for analysis, including 20 blanks and 22 duplicates. This represented 407 downhole intervals over a length of 1064.45 metres. The average sample length was 2.62 metres. In-field bulk density measurements were made on 47 intervals which represented a variety of lithological units with variable iron content. A total of 38 of these measurements were made on sampled intervals. The weight of whole core in air and water was determined by comparing the weight in air versus water for each sample. The entire core for the interval was weighed whole core in air, on the scale and was also weighed in water, while suspended in a sling, from the scale. The in-water weights accounted for sling weights. All of the core samples were split in half using a diamond saw. One half was returned to the core box and the other half was placed, together with the sample tag, into a large 3mm poly bag labeled with the sample number. The bags were sealed with zap straps and also put into individual, labeled rice bags for additional strength. When the sampler encountered a tag for a blank sample, the designed blank sample and the new tag was transferred into a new bag with the new sample number. When the sampler encountered a tag for duplicate sample, the sampler placed the remaining half core for the preceding interval, and the sample tag into a bag with the indicated number. The resultant gap in the core box was replaced with a wooden block bearing a metal tag with information about the two samples: regular and duplicate, for the interval. Five samples (5751 to 5755) were selected for preliminary metallurgical tests. These were packed into 3 sealed sample pails, together with a shipping list. The remaining routine samples were loaded sequentially into 3 large wooden crates which contained shipping lists. All of these containers were to SGS Lakefield, to the attention of Nick Lee, metallurgist. 8.2.2 SAMPLE PREPARATION As indicated above, samples sent to SGS Lakefield were either designated as test, or routine. SGS is an accredited laboratory facility which meets the requirements of ISO 9001 and ISO 17205. The 5 preliminary samples (5751 to 5755) were submitted for initial Davis tube testing at different grinds to establish the optimum grind size for LIMS, as well as bulk density and SG determinations. The 424 routine samples were subjected to more conventional preparation methods for multi-element whole rock and FeO analyses, and Satmagan determinations. Selected samples were also designated for bulk density and specific gravity determinations. Details about the preparation and analytical methods, as well as results, are documented in a report from SGS Lakefield, Appendix 3. Bulk density determinations on entire samples were also made on a total of 54 samples (including 5 test samples).

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Each of the 5 test samples was crushed to nominal 1/4” and a 1-kg sub-sample was riffled out. The remainder was stored. Each nominal 1/4” sub-sample was stage-crushed to minus 10 mesh (1.7 mm), and seven 100-g test charges were prepared. Three charges were used for grind curve determination, three for Davis tube testing by size, and one for direct head analyses. The resultant products from the Davis tube tests were also subjected to the same analyses as their associated head samples. Each of the 424 routine samples was cone-crushed to nominal 1/4” and a 1-kg sub-sample was riffled out. The 1-kg sub-sample was stage-crushed to minus 10 mesh and one 100-g test charge was prepared prepared, while the remainder was stored. An additional 18 of the routine samples were selected by Raytec to be prepared as –A and –B suffixed prep duplicates (FR. For these samples, an additional 1 00-g test charge was prepared to minus 10 mesh for sample preparation QA/QC purpose. These samples were prepared to be run in lieu of lab duplicates for pending metallurgical tests on routine samples, since SGS did not run internal lab duplicates for their metallurgical procedures (Nick Lee, personal communication). The samples were labeled as A and B, since they were not intended to be submitted blindly, like the field duplicates. They were intended to be referred to by the lab as part of internal quality control which would otherwise not be present. All sample rejects were re-packaged using the original sample bags and are currently stored by SGS Lakefield. 8.2.3 ANALYTICAL METHODS The -10 mesh pulps from all samples, both test and routine, were forwarded to the analytical laboratory of SGS Lakefield, for multi-element whole rock analysis (WRA) of SiO2, Al2O3, Fe2O3, MgO, CaO, Na2O, K2O, TiO2, P2O5, MnO, Cr2O3, V2O5 and loss on ignition (LOI), and also for FeO analysis. Satmagan determinations of % magnetite contents were conducted on all samples, as well. WRA, FeO and S (sulphur) analyses were also completed on the magnetic concentrates obtained from the Davis Tube tests. Samples were further pulverized to a -200 mesh size, with various splits made for the WRA, FeO and Satmagan determinations. Details about analytical methods are presented Appendix 3. Sample preparation for WRA consists of the formation of a homogenous glass disk by the fusion of 0.2 to 0.5 g of rock pulp with 7g of lithium tetraborate/lithium metaborate (50/50). The LOI at 1000°C is determined separately gravimetrically. The LOI is included in the matrix-correction calculations, which are performed by the XRF instrument software. The disk is analyzed by X-ray diffraction (XRF) spectrometry. Sample preparation for FeO analysis consists digestion of a 0.25 g split from the rock pulp, with sulphuric and hydrofluoric acids, and the addition of boric acid. After cooling, the digested sample is titrated with a standardized solution of potassium dichromate to determine Fe2+.Sample preparation for sulphur (S) analysis consists of mixing a 0.1 to 0.5g split from the rock pulp, with an accelerator. The mixture is then combusted and measure by infrared dectios on LECO instrumentation. Specific gravity determinations were conducted on a total of 101 sample pulps from the routine samples, including 5 from the test samples selected by Raytec. These determinations were completed by the gas pycnometer method.

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8.2.4 METALLURGICAL METHODS The details of metallurgical methods are presented in the SGS Lakefield report, in Appendix 3, and are summarized below. GRIND CURVE ESTIMATION To derive the a grind curve for the 5 test samples, three 100g charges from each were pulverized for 90, 150 and 210 sections in a pulverizing pot containing a metal ring and a puck. The resultant ground products were then submitted for wet particle size analysis (PSA). The P99 grind size for each 100g sample was plotted against time, to generate the grind curves. From these curves, grind times for each of the five samples were estimated for each of the -200 mesh, -325 mesh and -400 mesh sizes. DAVIS TUBE DETERMINATION The grind curve work indicated the samples were hard and therefore, the estimated grinding times were very long, at an average of 932 seconds. Since long pulverizing sessions cause the pots to heat up, samples were stage pulverized, screened on the top mesh size and then the oversize was pulverized. This was repeated to 100% passing the designated screen sizes of -200 mesh, -325 mesh and -400 mesh sizes. A 20 g sub-sample from each of these products was subjected to Davis tube determination. The Davis tube was operated at conditions of 1.5 amperes, 1 L/min of wash water, and 100 strokes/minute. The 20g sample was introduced into the Davis tube, which was agitated for 4 minutes. The non-magnetic tailings were collected in a pail throughout the process. After 4 minutes, the magnets were interrupted and the concentrate was collected separately. Both products of concentrate and tailings were filtered and dried. The concentrates were subjected to WRA, FeO, S analyses, as noted above. Satmagan determinations were also conducted to assess the efficacy of the Davis Tube test. SATMAGAN DETERMINATION Satmagan (Saturation Magnetization Analyzer) refers to an electromagnetic method used to estimate either the amount of magnetite or magnetic iron of a sample.. The instrument is a magnetic balance in which the sample is weighed in gravitational and magnetic fields. If the field is strong enough to saturate the magnetic material within the sample, the ratio between the two measurements is linearly proportional to the amount of magnetic material in the sample. The amount of magnetic material in a sample may therefore be estimated by calculating the ratio between the measured magnetic force and gravitational force, and multiplying this by a coefficient and an instrument constant. For this program, the testing was completed on a 4 to 5g sub sample from each rock sample pulp (for routine and test samples) and from each Davis Tube concentrate (for test samples).

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9.0 DIAMOND DRILLING RESULTS 9.1 GENERAL RESULTS During the 2008 exploration program, a total of 11 drill holes tested the A Zone iron formation over a strike length of approximately 3 kilometres. The locations of the holes are shown in a compilation in Figure 6. Details of the drill holes are presented in drill sections Figures 7a-h, in the map pocket and within drill logs in Appendix 5. Eight holes (ES08-001 to -008) were drilled along five sections over a distance of 1100 metres of the Kesaka Far East area. Two holes (ES08-009, -010) were drilled along two sections spaced approximately 200 metres apart, in the Kesaka East area. One hole (ES08-011) was drilled at the far west end of the A zone, in the Kesaka West area. All holes were drilled to the north, with the exception of ES08-007,-008,-011. Ground conditions along these sections were not suitable for the construction of drill pads to the south of the A Zone The drillholes tested a panel of iron formation of the A Zone which, in agreement with historical drilling, was shown to be inclined steeply to the south. The original holes indicated the thickness of the iron formation ranged mostly between 30 and 70 metres. The recent drill holes confirmed these trends, and intersected a geological succession consistent with previous work. The general stratigraphic column for the intervals drilled is shown in Table 5, below. The progression of the sequence, from coarse to fine sediments (CONG, GWK, ARG) into iron formation ranging from silicate (IFL) to mixed silicate-oxide ((IFLM, IFML), to oxide (IFM, IFMJ) types, is consistent with general facies development of iron formation. The distribution of these units throughout the A and B Zones define a property scale synclinal fold. In several of the 2008 drillholes, the presence of cross bedding and scours within bedded greywacke, indicate that stratigraphic tops along the north limb of the fold, at the A Zone, are to the south. Conglomeratic horizons below the iron formation in the B Zone, and in the Kesaka West area of the A Zone, are good stratigraphic marker horizons which also define the fold structure. In the holes drilled during this program, conglomeratic textures are only locally developed within greywacke. However, the conglomerate is well exposed in outcrop along the western shore of Kesaka Lake. Argillite horizons have been documented within the sediments both above and below the iron formation. They are locally carbonaceous and may contain disseminated sulphides. These horizons may be the source of conductive, linear VLF-EM responses which were detected with ground geophysics.

Proceeding upsection within the iron formation, there is a decrease in iron silicate and an increase in iron oxide. Iron silicates as chlorite and amphiboles are mostly contained within laminated to bedded sections of chloritic mudstone (IFL). Decimetre to centimeter scale beds of chloritic mudstone are components of the lean and mixed facies, as well. Within the lowermost units, IFL and IFML, fine to medium grained garnets are disseminated throughout the mudstone. Upsection, the proportion and thickness of interbeds of chloritic mudstone decrease and become subordinate to alternating bands of magnetite and chert, within the oxide facies units, IFM and IFMJ. Within these units, the proportion of chert and jasper is variable. Local variants of the mixed and oxide facies were logged as IFMS and IFMR, which contain sediment interbeds or a strong grunerite overprint, respectively.

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TABLE 5: STRATIGRAPHIC COLUMN for 2008 DRILLHOLES (Stratigraphic tops are to the south)

Sediments GWK, ARG Greywacke, Argillite

QPM Quartz Porphyry with Iron Formation Felsic to Intermediate

dykes or tuffs QP Quartz Porphyry

IFMJ Magnetite-Jasper Iron Formation (IFMJ) Oxide Facies

Iron Formation IFM Magnetite Iron Formation (IFM)

IFML Magnetite-Chlorite Iron Formation (IFML) Mixed Silicate-Oxide

Iron Formation IFLM Chlorite-Magnetite (Lean) Iron Formation

+/-garnets (IFLM)

Local variants with sediment

interbeds (IFMS) or with strong

grunerite overprint (IFMR)

Silicate Facies Iron Formation IFL Silicate Iron Formation (IFL)

+/- garnets, sediment interbeds

ARG Argillite locally carbonaceous +/- sulphides

Sediments GWK, CONG,

PG, QBS Greywacke, Conglomerate

Metamorphosed to migmatitized

equivalents: Paragneiss and Quartz Biotite

Schist Within the iron formation, magnetite is commonly medium grained and granular textured. Chert bands are mostly variable from white to pale grey in color and may be interbanded with minor jasper. With decreased silicate content as chloritic bands, the iron formation grades into an oxide facies, unit IFM. Within IFM, chert varies from pale to dark grey-blue in color; magnetite is dark grey to black. With increasing magnetite content, the unit contains massive intervals of finely laminated, fine grained, argillaceous magnetite and chloritic partings. Local fine grained specular hematite was noted as mm scale seams and fine disseminations. With a progressive increase in jasper content, compared with chert, the iron formation grades into unit IFMJ. Quartz porphyry (QP) was not identified in historical drill logs; however, similar narrow horizons internal to the iron formation have been described as paragneiss. It has been documented in drillholes of the Kesaka Far East area. The porphyry occurs as narrow, metre scale sections with sharp upper and lower contacts which are parallel to banding within the flanking iron formation. Within drillholes, it alternates mostly with iron formation, and locally with greywacke. The unit is buff colored, and has a medium to fine grained groundmass with 1-3mm quartz eyes and local biotite or chlorite wisps. An internal, moderately strong cleavage is developed, and is consistent with that within flanking units. Some textures suggest that the quartz porphyry unit may be narrow tuffaceous horizons which are intercalated or infolded with iron formation. They may also be narrow, parallel dykes emplaced into the succession during early strain events. Regardless of the provence of this unit, its presence in the succession is a source of dilution within some sections of the A Zone iron formation.

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Decimetre scale, grey-brown lamprophyre dykes locally cut the iron formation and quartz porphyry. The dykes have straight to undulating contacts which are sharp and subparallel to banding. Due to their high biotite and calcite content, the dykes have been loci for increased strain, resulting in strong cleavage and mylonitic textures. Rare dm to cm scale granitic, aplitic and dioritic dykes also cut the sequence. In the Kesaka East area, drillholes ES08-009 and -010 encountered a sequence which most closely represents the above stratgraphic column. The horizontal width of the iron formation intersected in these holes is 47 and 53 metres, respectively. In both holes, the iron formation grades downhole from more magnetite-hematite bearing oxide facies (IFMJ, IFM) into leaner, mixed silicate-oxide facies (IFML) with lower garnetiferous members, and argillite below. No fold repetition of these internal units was apparent; however, internal ductile strain is recognized as local cm to dm scale asymmetrical folds, some of which appear refolded. In the Kesaka Far East area, however, the stratigraphy encountered is more diverse; alternating between oxide, mixed oxide-silicate and silicate facies iron formation. The horizontal width of the iron formation intersected in these holes ranges from 39.5 metres (ES08-003) to 66.9 metres (ES08-008). On the three sections where two holes were drilled (ES08-001 and-002; ES08-004 and -005; ES08-007 and -008), the horizontal width of iron formation is variable and the lithological sequences are complex. Intervals of quartz porphyry were predominantly encountered in only one of the holes on these sections, and textures suggested they may be syntectonic dykes or tuffaceous horizons near the top of the succession. This is consistent with both the distribution of sections of quartz porphyry within the drillholes, as well as their sharp, contacts which are parallel to the iron formation banding. Tight, asymmetrical folding of the succession may account for the observed distribution of downhole lithologies in the Kesaka area. The horizontal widths of iron formation encountered in this area are similar to those of the Kesaka East, but include internal dilution as intervals of lean facies IF, quartz porphyry and sediments. These observations suggest that to the east (Kesaka Far East area), the iron formation encountered is a folded thickened succession which includes overlying felsic to intermediate tuffs or syntectonic dykes. The Kesaka West area, the iron formation is comparatively thinner than in the east, and occurs as multiple horizons. Intervals of quartz porphyry or paragneiss are present but are not common. The property scale map patterns of iron formation, as interpreted from historical drilling and geophysics, show the horizon is broken into long segments and isolated fold structures. These patterns may be the product of ductile strain along EW and WSW-ENE trends, as well as late brittle faulting along NE and NNW trends. The structures observed in both diamond drillcore and outcrop exposures are complex. They also indicate that the rocks of the property have been subjected to high strain during successive deformational events. The dominant structural grain on the property is a strong east-west trending, steeply south dipping cleavage which is mostly parallel to the lithological trends. In drillcore, the observed banding of iron formation and cleavage is mostly consistent with this. Within bedding units of iron formation, greywacke and argillite, several cm to dm scale folds were also identified. These are interpreted as the products of a minimum of two, superimposed strain events.

36

An early event is recognized as tight, cm scale asymmetrical folds which have axial planes consistent with the vertical to steeply south dipping regional cleavage. Lineations indicate these folds plunge shallowly (to the west or east). These early fold structures and banding are also commonly deformed into later dm scale folds along steeply dipping axes which are also closely coincident with the regional cleavage. These folds plunge steeply to the west. Within drillcore, the observed repetition of these fold structures with straight banded sections may be the expression of asymmetrical folding along east-west trending axes. In addition to fold hinges, other linear elements such as migmatic segregations, clasts, and segments of boudinaged chert bands also plunge steeply to the west. This later ductile strain event has tightened earlier fold structures, has caused transposition and local boudinage of iron formation banding. Such elements could develop during an episode of ductile shearing. Later stage, metre scale shearing was also recognized in the upper sections of drillholes ES08-001 and -002, of the Kesaka Far East area. These structures were described as east dipping mylonitic shear zones which are silicified, carbonatized. Minor pyrite and sphalerite were noted. Late brittle deformation is noted in drillcore and outcrop exposures; however, it represents a minor component of the strain which have affected the rocks of the El Sol property. In drillcore, it is expressed as minor, steeply dipping hair fractures and microbreccias of calcite+/-pyrite+/-quartz, chlorite which cut all rock types. Fractures are both steeply and shallowly dipping. A NNW, steeply dipping set was common. 9.2 ANALYTICAL RESULTS The results of XRF whole rock analysis and Satmagan determinations on a total of 407 samples provided a characterization of the component units of the iron formation. The various proportions of iron from magnetite, hematite and other (silicate, carbonate) sources, and the hematite content were determined by R. Risto of WGM, using a proprietory method of calculation. Table 6 presents the averaged sample results and the hematite content for each of the general units (Litho_gen) documented in the 2008 drillholes. Six of the iron formation units (IFM, IFMJ, IFML, IFMR, IFMS) and a unit of quartz porphyry with sections of iron formation (QPM), were documented as magnetite bearing. These units comprised 313 (77%) of the total samples. Elevated total iron (TFe%) and magnetic iron (FeMt%) contents for these units range from 13.94%(QPM) to 35.67%(IFMJ) and 5.31%(IFLM) to 33.63%(IFMJ), respectively. The ratio of FeMt% to TFe% (Recoverable iron) indicates the proportion of magnetic iron which could be recovered from total iron, and therefore gives an indication of the amount of iron as magnetite (in the absence of other magnetic iron sources) for the iron bearing lithologies (Fig 8). For the seven magnetite bearing lithologies, this ratio ranged from 25.49% (IFLM) to 96.25%(IFM). The highest ratio results of 96.25% (IFM), 94.36% (IFMJ) and 80.96% (IFML) represented 264 (65%) of the total samples. The results therefore show that most of the iron within the iron formation occurs as magnetite.

37

TABLE 6: ANALYTICAL RESULTS AVERAGED BY LITHOLOGY

ARG GWK IFL IFLM IFM IFMJ IFML IFMR IFMS QP QPM# SAMPLES 17 33 11 15 83 117 64 13 13 33 8

T Fe% 8.96 4.53 14.07 16.47 34.25 35.67 29.80 28.74 22.69 3.23 13.94Hm_cal% 0.84 0.46 2.52 1.95 0.43 2.53 0.31 0.39 0.61 0.35 0.50Mt_SAT% 1.52 0.33 1.48 7.34 45.70 46.48 34.07 22.53 23.96 1.02 14.61Fe_Mt% 1.10 0.24 1.07 5.31 33.07 33.63 24.65 16.30 17.34 0.74 10.57

T Fe% - Fe_Mt% 7.87 4.29 12.99 11.15 1.19 2.04 5.15 12.43 5.36 2.50 3.37Recoverable Fe_Mt% 10.54 5.40 7.43 25.49 96.25 94.36 80.96 52.18 70.37 13.78 76.23

SiO2% 57.06 64.16 54.90 53.28 42.73 41.84 45.39 45.46 49.94 63.54 55.04Al2O3% 15.14 14.58 12.86 9.52 1.57 1.27 3.18 3.87 6.66 15.27 10.71Fe2O3% 12.81 6.48 20.11 23.54 48.96 50.98 42.52 41.08 32.44 4.62 19.93MgO% 2.80 1.83 2.29 2.70 1.67 1.64 1.92 2.00 2.01 1.82 2.38CaO% 2.76 3.59 2.47 3.08 2.81 2.38 3.22 3.68 2.47 3.59 3.81

Na2O% 0.86 2.45 0.64 0.18 0.14 0.13 0.11 0.18 0.48 3.97 2.43K2O% 3.53 2.91 3.27 3.00 0.70 0.65 1.12 0.91 3.94 3.12 2.07TiO2% 0.56 0.54 0.51 0.37 0.05 0.04 0.13 0.14 0.23 0.29 0.25P2O5% 0.17 0.15 0.18 0.17 0.16 0.16 0.18 0.17 0.17 0.12 0.16MnO% 0.10 0.07 0.16 0.13 0.06 0.05 0.09 0.14 0.09 0.04 0.06

Cr2O3% 0.02 0.02 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01V2O5% 0.02 0.02 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01LOI% 3.75 2.84 2.17 3.43 0.91 0.67 1.66 1.76 1.32 2.97 2.27Sum% 99.59 99.63 99.63 99.43 99.77 99.83 99.52 99.42 99.78 99.37 99.08

Fe2_as_FeO% 10.00 5.08 14.92 14.50 16.39 15.19 17.49 23.09 14.86 3.16 8.43 Recoverable Fe_Mt% is the proportion of Fe from magnetite (Fe_Mt%) which can be recovered from TFe%.

TFe% vs Fe_Mt% by Lithology

y = 0.6431x + 13.589R2 = 0.8516

0

10

20

30

40

50

0 10 20 30 40 50

Fe_Mt%

TFe

%

IFLM

IFM

IFMJ

IFML

IFMR

IFMS

QPM

All Mt Samples

1:1 Line TFe%

1:1 Line TFe%

FIGURE 8: ANALYTICAL RESULTS by LITHOLOGY

38

Unit IFMJ had a higher TFe% content (35.67%) compared with unit IFM (34.25%), yet a lower recovery. The elevated calculated hematite content in unit IFMJ (2.53%) compared with unit IFM (0.43) would account for this difference. The low hematite content for unit IFML (0.31%) suggests that the lower recovery for this unit is not due to elevated hematite, but instead, due to elevated iron in silicate or carbonate sources. In Figure 7, a greater variance between TFe% and FeMt% is shown for samples of units IFML, IFMR, and IFMS. These samples contain a wider range of overall magnetite content, due to higher proportions of non-magnetic iron sources (chloritic mudstone, grunerite) and dilutive components (sediment interbeds). Samples along the 1:1 Line contain iron mostly as magnetite, while those above the line contain iron from non-magnetic sources (ie. hematite, silicates and carbonates), as well. The graph also shows that 63 of 407 samples lie below the line and therefore had values for FeMt% greater than TFe%. This apparent contradiction may be due to the known poorer accuracy of Satmagan determinations at high magnetite content (G. Chiasson, pers.comm) or laboratory errors. This is further addressed in the QA-QC section below. 9.3 BULK DENSITY-SPECIFIC GRAVITY RESULTS A preliminary assessment of the bulk density-specific gravity compared with total iron and magnetic iron contents was completed during this program. A total of 192 determinations were completed on selected 2008 drill core samples. The selected samples represented the various facies of iron formation, quartz porphyry, argillite and greywacke. Samples of the various facies of iron formation had average bulk density and specific gravity results of 3.43 and 3.46, respectively. Samples of the dilutive lithologies (GWK, ARG, QP) had average bulk density and specific gravity results of 2.75 and 2.79, respectively. The highest average bulk density and specific gravity results of 3.50 and 3.54, are associated with samples of the IFMJ facies. Table 7, below, shows a summary of the results compared with total iron (TFe%) and magnetic iron (FeMt%). These relationships are shown for each type of determination, in Figures 9a and 9b. The bulk density (field and lab) and specific gravity results show a good correlation with TFe% results, ranging from 0.9413 to 0.9732. The results show a lower and wider range of correlations with FeMt%, from 0.7789 to 0.9342. This discrepancy may be, in part, due to QA-QC issues with the Satmagan procedure. Based on current results, a formula to determine specific gravity (SG) of a sample based its TFe% content would be: SG = 0.0248(TFe%) + 2.6397.

TABLE 7: SUMMARY OF BULK DENSITY-SPECIFIC GRAVITY RESULTS

CORRELATION

(R2) MEASUREMENT # SAMPLES

T Fe% Fe Mt% All 192 0.9413 0.8357

Bulk Density Field 37 0.9764 0.7789 Bulk Density Lab 54 0.9732 0.9342

Specific Gravity Lab 101 0.9453 0.8526

39

Bulk Density and Specific Gravity compared with TFe%

y = 0.0248x + 2.6397R2 = 0.9413

2

2.5

3

3.5

4

0 10 20 30 40 50

TFe%

Bul

k D

ensi

ty o

r S

peci

fic G

ravi

ty

Bulk Density_FieldBulk Density_LabSpecific Gravity_LabALLLinear (ALL)

FIGURE 9a: BULK DENSITY and SPECIFIC GRAVITY

COMPARED WITH TFe%

Bulk Density and Specific Gravity compared with Fe Mt%

y = 0.0188x + 2.8877R2 = 0.8357

2

2.5

3

3.5

4

0 10 20 30 40 50

Fe Mt%

Bul

k D

ensi

ty o

r Sp

ecifi

c G

ravi

ty

Bulk Density_FieldBulk Density_LabSpecific Gravity_LabALLLinear (ALL)

FIGURE 9b: BULK DENSITY and SPECIFIC GRAVITY

COMPARED WITH FeMt%

40

9.4 2008 DRILLHOLE SUMMARIES The 2008 exploration program, of 2301 metres drilled in 11 holes, was focused along the iron formation of the A Zone. Ten of the holes were drilled in the Kesaka Far East (ES08-001 to -008) and the Kesaka East (ES08-009,-010) areas, between Kesaka and Jean Lake. One of the holes (ES08-011) was drilled in the Kesaka West area, near the western shore of Kesaka Lake. The distribution of the drillholes is shown in Figure 6. The composite results for the 2008 drillholes are shown in Table 8. The horizontal width is along the drilled section (and therefore apparent) and is calculated based on a vertical panel of iron formation. Composites are calculated for all samples within the selected interval, and also for only samples with >10% FeMt. The latter method does not include lower grade, or areas of internal dilution. This is similar to some of the detailed composites shown on the historical sections. The amount of internal dilution is the difference between the drilled length and the sum of the intervals of samples with >10% FeMt. For both composite series, the TFe% and FeMt% grades are shown as both an average and weighted average. The composite results of the new drillholes are compared with the composite results which were used as a basis for the historical resource estimate by Hicks (1958). Although the source data for the composites is incomplete, these composites at least represent a consistent treatment of results for all historic drillholes. In his calculations using the sectional method, Hicks documented an Fe% grade and horizontal width for each intercept. It is uncertain if the horizontal width documented is apparent (ie. along the section) or true. It is, however, accepted for general comparison with the sectional horizontal widths for the 2008 drillholes, since many of the drillholes were drilled perpendicular to the strike of the iron formation. The Fe% grade is assumed to be an iron soluble result which would include iron from oxide, limonite and carbonate sources. In the absence of hematite, this approximates the FeMt% grade; however, in the presence of hematite, the Fe% grade may be higher than the FeMt% grade. The Fe% grade would not approximate the total iron TFe% grade, unless there is no iron from silicate sources in the sampled interval.

41

DD

HFr

om

(m)

To

(m

)

Dril

led

Leng

th

(m)

Hor

iz

Wid

th

(m)

Avg

T Fe

%A

vg

Fe

Mt%

WtA

vg

T Fe

%W

tAvg

Fe

Mt%

Dril

led

Leng

th

(m)

Avg

T Fe

%A

vg

Fe

Mt%

WtA

vg

T Fe

%W

tAvg

Fe

Mt%

Met

res

of

dilu

tion

%

dilu

tion

ES08

-001

125.

5519

1.05

65.5

049

.51

25.8

722

.55

25.9

622

.73

50.2

532

.17

29.1

832

.21

29.4

815

.25

23.2

8

ES08

-002

148.

5724

7.00

97.2

355

.77

30.7

827

.07

30.9

427

.27

87.7

932

.98

30.0

333

.18

30.3

69.

449.

71

ES08

-003

90.0

014

7.43

57.4

342

.34

28.3

123

.57

28.5

223

.58

43.8

832

.09

28.9

032

.42

29.2

813

.55

23.5

9

ES08

-004

63.6

214

1.47

77.8

555

.53

32.3

028

.59

32.1

728

.55

71.7

033

.63

30.2

833

.54

30.3

36.

157.

90

ES08

-005

95.3

819

7.90

102.

5248

.13

24.2

721

.40

22.8

519

.85

65.3

732

.70

30.3

532

.48

30.0

137

.15

36.2

4

ES08

-006

113.

4620

8.83

95.3

770

.76

30.0

626

.06

30.5

126

.36

78.2

933

.89

31.3

134

.02

31.2

317

.08

17.9

1

ES08

-007

52.5

514

0.00

87.4

561

.73

23.0

420

.59

20.5

017

.85

51.4

732

.33

30.0

631

.68

29.2

435

.98

41.1

4

ES08

-008

65.8

019

7.65

131.

8568

.30

32.0

730

.45

31.0

429

.39

118.

1534

.54

32.9

634

.34

32.7

613

.70

10.3

9

ES08

-009

101.

3516

8.00

66.6

549

.61

33.3

530

.47

33.2

030

.32

66.6

533

.35

30.4

733

.20

30.3

20.

000.

00

ES08

-010

87.9

216

5.00

77.0

857

.28

33.2

829

.44

32.9

829

.20

77.0

833

.28

29.4

432

.98

29.2

00.

000.

00

ES08

-011

130.

3514

7.00

16.6

511

.77

27.4

521

.04

27.6

921

.11

16.6

533

.70

29.2

433

.96

29.3

80.

000.

00

AL

L S

AM

PLE

SSA

MPL

ES

with

>10

%Fe

Mt

INT

ER

NA

L

DIL

UT

ION

INT

ER

VA

L

TA

BL

E8:

CO

MPO

SIT

ER

ESU

LT

Sfo

r20

08D

RIL

LH

OL

ES

42

KESAKA FAR EAST A total of eight holes (ES08-001 to ES08-008) in five sections were drilled to test the A Zone over an approximate 1100 metre strike length. Three of the sections were tested with two drillholes. For the holes drilled in the Kesaka Far East area, the horizontal width of the iron formation interval averaged 56.51 metres. It varied between 42.34m (ES08-003) to 70.76m (ES08-006) and proportions of internal dilution ranged from 7.90% (ES08-004) to 41.14% (ES08-007). Drillholes ES08-004, -006, and -008 all had thicker horizontal widths of iron formation intervals and low to moderate ranges of internal dilution. Their horizontal widths of iron formation only (ie. not including dilutive samples) are 51.14 m, 58.09 m, and 61.02 m, respectively. For both series, the difference between average and weighted average for TFe% and FeMt% is minimal, since the majority of the samples were 3 metres in length. Exceptions to this are drillholes ES08-005 and -007. These holes encountered higher proportions of internal dilution and had more irregular sample intervals, resulting in larger discrepancies between the two composites. The weighted TFe% and FeMt% grade of iron only samples for each hole averaged 32.98% and 30.34%, respectively. The weighted TFe% and FeMt% grade of full composites for each hole averaged 27.81% and 24.45%, respectively Drillholes with composites having higher values in both weighted TFe% and FeMt% include: ES08-002 (30.94%,27.27), ES08-004 (32.17%, 28.55%), ES08-006 (30.51%,26.36%) and ES08-008 (31.04%, 29.39%). These intervals both contain a high proportion of magnetite bearing iron formation and lower proportions of internal dilution. They therefore represent the better intercepts encountered during 2008 drilling in the Kesaka Far East area.

DRILLHOLES ES08-001 and ES08-002 SECTION DDH Length

m Horiz Width m

WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 3883 ES08-001 65.50 49.51 25.96 22.73 2008 E 54 3883 ES08-002 97.23 55.77 30.94 27.27 2008 E 54 3883 ES57-053 68.58 28.5 Hicks East ES57-049 67.06 27.8 Hicks West ES57-042 54.86 32.3 Hicks

Drillholes ES08-001 and -002 were planned to test the A Zone iron formation in the vicinity of historic drillhole ES57-053. The holes intersected a steeply south dipping iron formation with horizontal widths of 49.51 and 55.77 metres, at elevations of approximately 305 and 245 masl. The internal facies of the iron formation outline an upright, antiformal fold of IML and IMJ iron formation which is flanked by IFML. Towards the base of the drilled intervals, there are dilutive sections of quartz porphyry (in ES08-001) and sediment interbeds (in ES08-002). These may be equivalents of up section intervals of paragneiss in ES57-053. The general interpretation of the margins the iron formation suggests that the assumed position of drillhole ES57-053 is a close approximation. The increase in the width of the iron formation in this hole, compared to the underlying 2008 holes and iron formation surface trace, suggests that the horizon may have been fold thickened. It is also possible that the surface trace of the iron formation is actually broader than interpreted.

43

The above results indicate that within the iron formation intersected in both drillholes ES08-001 and -002, most of the iron occurs as magnetite. The lower TFe% and FeMt% grades in ES08-001 can be attributed to internal dilution from quartz porphyry, as well as greater thickness of IFML. The variable thicknesses and grades of historic holes, both along the same section and along strike, suggest that fold thickening in both dimensions may have affected thickness and overall grade of the iron formation.

DRILLHOLE ES08-003

SECTION DDH Length

m Horiz

Width m WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 3624 ES08-003 57.43 42.34 28.52 23.58 2008 E 54 3624 ES57-054 54.86 23.7 2008

Drillhole ES08-003 was planned to test the A Zone iron formation in the vicinity of historic drillhole ES57-054. The hole intersected a steeply dipping iron formation with a horizontal width 42.34 metres, at an elevation of approximately 330 masl. The drillhole intersected alternating sections of magnetite-chert, magnetite-chert-chlorite, and magnetite-chert-jasper iron formation, which are flanked by thin horizons of lean iron formation. Minor internal dilution occurs as lean iron formation, quartz porphyry, and biotite dykes. Historic drillhole ES57-054 intersected the centre of the iron formation approximately 50 metres above ES08-003. The increase is width in the iron formation may be due to localized fold thickening, as well. The Fe% grade (23.7%) in the historic drillhole is a close equivalent to the TFe% grade (23.58%) of drillhole ES08-003.

DRILLHOLES ES08-004, ES08-005

SECTION

DDH Length m

Horiz Width m

WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 3317 ES08-004 77.85 55.53 32.17 28.55 2008 E 54 3317 ES08-005 102.52 48.13 22.85 19.85 2008

East ES57-057 51.82 32.0 Hicks West ES57-061 64.01 28.6 Hicks

Drillholes ES08-004 and -005 were planned to test the A Zone iron formation between historic drillholes ES57-057, to the east, and ES57-061, to the west. The holes intersected a panel of steeply south dipping iron formation with horizontal widths of 55.53 and 48.13 metres, at elevations of approximately 350 masl and 285 masl, respectively. The iron formation appears to thicken to the west, towards drillhole ES08-006. Downhole lithologies encountered in these two holes are complex. The shallower drillhole, ES08-004, intersected an upper section of alternating magnetite-chert (IFM) and magnetite-chert-jasper (IFMJ) facies and a lower section of magnetite-chert-chlorite facies interbedded with chloritic mudstone (IFL). Within the deeper drillhole, ES08-005, the general upper and lower distribution of iron formation is similar; however the central and lower parts of the interval also contain numerous sections of quartz porphyry that do not appear at higher levels.

44

The distribution of lithologies between the drillholes, together with the high strain observed in drillcore, suggest that the iron formation on this section represents a series of highly transposed asymmetrical folds which climb uphole, to the south. Facing to the east, the structures would appear as Z-folds. Within these patterns, the general stratigraphy encountered is younging up hole, to the south, and dykes or tuffaceous beds of quartz porphyry are found lower in the stratigraphy. The above results indicate that, within the iron formation of drillholes ES08-004 and -005, most of the iron occurs as magnetite. The overall lower TFe% and FeMt% grades in ES08-005 can be attributed to internal dilution (36%). The FeMt% grade of 28.55% is similar to that reported for historic drillhole ES57-061, to the west. The geology observed on this section, together with the composite results, demonstrate that variable thicknesses and grades of iron formation at depth are also related to fold thickening.

DRILLHOLE ES08-006 SECTION DDH Length

m Horiz Width m

WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 3008 ES08-006 95.37 70.76 30.51 26.36 2008 E 54 3008 ES57-030 68.58 32.0 Hicks E 54 3008 ES57-035 71.63 27.5 Hicks E 54 3008 ES57-055 54.86 31.5 Hicks

Drillhole ES08-006 was planned to test the A Zone iron formation along a section of multiple historic drillholes (ES57-030,-035,-055) which tested the iron formation below a bulk sample trench described by Hicks (1958). During this field program, the trench was located along the projection of the iron formation, to the immediate west of the drilled section. Drillhole ES08-006 intersected a section of vertically dipping iron formation with a horizontal width of 70.76 metres, at an elevation of 300 masl. The location of the upper contact of the iron formation, compared with those of the historic holes appears to be closely coincident (within 10 metres) and therefore, drillhole ES08-006 should most closely approximate ES57-035. The top of the hole collared in a thick section of laminated to bedded greywacke. Local scours, flame structures and crossbedding within this unit consistently indicate a stratigraphic tops direction which is up hole, to the south. Downhole, the greywacke appears to be intercalated with 2-4 metre, bedding parallel intervals of quartz porphyry. Below this section, greywacke fines into a grey laminated argillite with chloritic mudstone and chert bands. Similar to drillhole ES08-004 to the east, the upper section of the iron formation is dominated by relatively high grade sections of magnetite chert+/-jasper (IFM) and magnetite-jasper iron formation (IFMJ). Moderately to strongly hematitic jasper bands are common and specular hematite occurs in some sections. Individual samples in these 10 to 20 metre long sections have hematite contents which vary between 1% and 8%. Moderate to strong grunerite is also developed in the upper iron formation, along a cleavage with is oblique to the main trend of banding.

45

Further downhole, the IFM and IFMJ horizons alternate with increasing proportions of magnetite-chert-chlorite iron formation (IFML) and chloritic mudstone +/- garnet (IFL). Narrow, metre scale quartz porphyry dykes cut the upper part of the iron formation and are parallel to the banding trends. The base of the sequence is marked by a section of interbedded black argililte and chloritic mudstone, with trace to 0.5% pyrrhotite. The horizontal thickness of the horizon (70.76m) is similar to that of the historic drillholes on this section. The above results for drillhole ES08-006 returned a TFe% grade of 30.51% and a lower FeMt% grade of 26.36%. The higher total iron grade may reflect the noted higher hematite content within this drillhole. Due to the elevated hematite, the weighted average grade for Fe% in the historic drillholes more closely approximates total iron TFe%, instead of FeMt%. The TFe% and FeMt% grades weighted by horizon width returned values of 2159 and 1865 respectively. These represent the second best (after ES08-008) results of the 2008 drilling campaign.

DRILLHOLES ES08-007, ES08-008 SECTION

DDH Length m

Horiz Width m

WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 2799 ES08-007 87.45 61.73 20.50 17.85 2008 E 54 2799 ES08-008 131.85 68.30 31.04 29.39 2008 ES57-026 54.86 32.9 Hicks

Drillholes ES08-007 and -008 were planned to test the A Zone iron formation along the section drilled by historic drillhole ES57-027. The holes were drilled to the south, instead of to the north, since suitable stable ground for a drill pad could not be found in the south. The drillholes intersected a vertically dipping panel of iron formation along horizontal widths of 61.73 and 68.30 metres, and centered at elevations of approximately 350 masl and 305 masl, respectively. The position of the iron formation within the historic and new drillholes suggests that the interpreted position of the old hole is within 10 metres of its actual position. Similar to the section of ES08-006 to the east, thick sections of iron formation were encountered in these drillholes. A narrower width of 54.86 metres for drillhole ES57-026 may be due to the exclusion of a narrow section of iron formation which is above a broad dilutive section of sediments or quartz porphyry. Similar to drillholes ES08-004 and ES08-005, downhole lithologies encountered in these two holes are complex. In the lower drillhole, ES08-008, the upper limit of the iron formation is marked by an interval of grey argillite interbedded with chlorite-garnet mudstone (IFL). The upper section of the iron formation consists of magnetite-chert-chlorite (IFML) and magnetite-chert-jasper (IFMJ) intervals with sections of quartz porphyry. The high grade core of the iron formation consists of interbedded magnetite-jasper-specularite (IFMJ) and magnetite-chert (IFM) intervals. The lower part of the iron formation is comprised of high grade magnetite-chert intervals +/- grunerite (IFMR). A subvertical, 1.5 metre wide breccia zone cuts near the base of the iron formation. A 5 metre section of grey to black carbonaceous argillite marks the limit of the iron formation.

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The upper drillhole, ES08-007, intersected a similar stratigraphic sequence, with intervals of magnetite-jasper-specularite (IFMJ) and magnetite-chert-jasper (IFM) in the core of the iron formation, flanked both uphole and downhole by intervals of magnetite-chert +/- grunerite (IFM, IMFR) iron formation. A total of 41% of the section is comprised of quartz porphyry, which occurs through the iron formation interval. This is in apparent contradiction with the sequence cut below, by drillholes ES57-026 and ES08-008. The distribution of lithologies between the drillholes, and the high strain observed in drillcore suggests that the iron formation on this section represents a series of highly transposed asymmetrical folds which climb uphole, to the north. Facing to the east, the structures would appear as S-folds. Within these patterns, the general stratigraphy encountered is younging downhole, to the south, and dykes or tuffaceous beds of quartz porphyry are found higher in the stratigraphy. The above results indicate that, within the iron formation of drillholes ES08-007 and -008, most of the iron occurs as magnetite. The overall lower TFe% and FeMt% grades in ES08-007 can be attributed to internal dilution (41%). The FeMt% grade of 29.39%, for drillhole ES08-008 is lower than that reported for historic drillhole ES57-026; however this hole did not incorporate an iron formation interval (and flanking internal dilution) into the composite. The geology observed on this section, together with the composite results, demonstrate that variable thicknesses and grades of iron formation at depth are also related to fold thickening. For drillhole ES08-008, the TFe% and FeMt% grades weighted by horizon width returned values of 2120 and 2007 respectively. These represent the best results of the 2008 drilling campaign. KESAKA EAST A total of two holes (ES08-009,-010) were drilled to test the A Zone in the northeast area of Kesaka Lake. The holes tested separate sections spaced 191 metres apart, with ES08-010 collared east of ES08-009. The horizontal width of the iron formation encountered in the two holes was 47.14 and 53.06 metres, with no internal dilution. Both drillholes returned similar composite grades for both TFe% and FeMt%: ES08-009 (33.20%, 30.32%) and ES08-010 (32.98%, 29.20%). These intervals both contain a high proportion of magnetite within the iron formation.

DRILLHOLE ES08-009 SECTION

DDH Length m

Horiz Width m

WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 1791 ES08-009 66.65 49.61 33.20 30.32 2008 ES56-023 62.79 31.5 Hicks ES57-036 57.91 32.8 Hicks

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Drillhole ES08-009 was planned to test the A Zone iron formation along a section of multiple historic holes (ES65-025,-023,-022, ES57-036) which tested the iron formation to the elevation of 50 masl, or to depths of 350 metres below surface. The hole intersected a section of steeply dipping iron formation with a horizontal width of 49.61 metres, at an elevation of 325 masl. The location of the upper contact of the iron formation, compared with those of the historic holes appears to correspond well, and therefore, drillhole ES08-009 should most closely approximate ES56-023. The top of the drillhole collared in a thick section of greywacke. Downhole, the units of iron formation represent a progressive facies change from magnetite-jasper-chert with specularite (IFMJ) to magnetite-chert (IFM), to magnetite-chert-chlorite (IFML) to magnetite-chert-chlorite-garnet (IFML, IFL). The latter unit also has a strong grunerite overprint. The base of the section is marked by a 2.2 metre horizon of grey argillite which is weakly carbonaceous. The underlying unit is a banded argillite and quartz-sericite-chlorite schist within a mylonitic shear zone. Horizontal thicknesses of iron formation in ES56-023 and ES57-036 are greater both above (62.79m) and below (57.91m) the new drillhole. The FeMt% grade of 30.32% for ES08-009 is lower than the Fe% grades of 31.5% and 32.8% for the historic drillholes. The higher historical results may be due to the inclusion of soluble iron from hematite. The TFe% and FeMt% grades weighted by horizon width returned values of 1647 and 1504, respectively. These represent the mid range results similar to those obtained from drillhole ES08-002 and ES08-010.

DRILLHOLE ES08-010 SECTION

DDH Length m

Horiz Width m

WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 1982 ES08-010 77.08 57.28 32.98 29.20 2008 East ES57-064 60.96 30.2 Hicks

Drillhole ES08-010 was planned to test the A Zone iron formation along a section to the east of ES08-009. The nearest historic hole, ES57-064, was drilled on a section approximately 150 metres to the east. The hole intersected a section of steeply dipping iron formation with a horizontal width of 57.28 metres, at an elevation of approximately 335 masl. The hole intersected iron formation which grades downhole into different facies which do not display major repetitions due to folding. The top of the hole collared in a thick section of greywacke. Downhole, the units of iron formation represent a progressive facies change from magnetite-chert-jasper with specularite (IFMJ) to magnetite-chert +/- specularite (IFM), to magnetite-chert-chlorite (IFML) with a grunerite overprint. The underlying unit is grey argillite to knotted phyllite. This section appears to lack the horizon of garnetiferous chloritic mudstone which is normally at the base of the drilled section of iron formation. It may be obscured by the strong grunerite overprint.

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The horizontal thickness of iron formation in ES09-010 (57.28m) is relatively consistent with that encountered in drillhole ES57-064 (60.96m) to the east and is thicker than that in drillhole ES57-009 (49.61m) to the west. The FeMt% grade of 29.20% is lower than the Fe% grade of 30.2%, for drillhole ES57-064. The higher historical result may be due to the inclusion of soluble iron from hematite. The TFe% and FeMt% grades weighted by horizon width returned values of 1889 and 1672, respectively. These represent the mid range results similar to those obtained from drillhole ES08-002 and ES08-009. KESAKA WEST Potential drill sites were limited in this area north of the iron formation, due to uneven and boggy ground conditions. A single hole (ES08-011) was planned to test the A Zone in the west of Kesaka Lake. This hole was drilled south to test the western limit of the A Zone. A section of historical drillholes (ES56-007, -006) to the east tested the iron formation to an elevation of 365 masl, or 60 metres below the surface.

DRILLHOLE ES08-011 SECTION

DDH Length m

Horiz Width m

WtAve TFe%

WtAve FeMt%

WtAve Fe%

Source

E 54 0810 ES08-011 16.65 11.57 27.69 21.11 2008 East ES56-007 25.30 29.8 Hicks East ES56-006 24.69 29.2 Hicks

The horizontal width of the iron formation encountered in this hole was 11.57 metres, with no internal dilution. This represents an apparent width, since the iron formation cuts the section obliquely, in this area. The hole an upper section of conglomerate and greywacke which, near the iron formation, grades into grey argillite with lean iron formation and quartz-sericite-chlorite-pyrrhotite schist. The interval is intensely fractured and cut by fine qtz-tourmaline breccias. The units internal to the iron formation are diverse, and may be fold or fault repeated. The core is dominated by intervals of magnetite-chert-jasper with specularite (IFMJ) which is flanked, both up and downhole, by intervals of chert-magnetite-chlorite-garnet. Internal sections of strongly foliated biotite wacke and quartz porphyry are sources of internal dilution. The horizontal thickness (11.57m) of iron formation in ES09-011 is notably thinner than those on the section to the east. In the Kesaka West area, historic drillhole show that the iron formation generally thins to the west. The FeMt% grade of 21.11% is lower than the Fe% grades of 29.8% and 29.2%, for drillholes ES56-007 and -006. This may be due to greater internal dilution in drillhole ES08-011, as well as the inclusion of soluble iron from hematite in the historic analyses.

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10.0 METALLURGICAL RESULTS The results of the original metallurgical studies by SGS Lakefield and Lurgi have been summarized in historical reports. The Lurgi report documents the results of LIMS (Low Intensity Magnetic Separation) testing on various grind sizes, on composite samples of 40 of the original drillholes. Polished thin sections of mineralization from each sample were also reviewed, to explain the analytical results. These results are summarized below. The 2008 metallurgical program was proposed by the consultants of WGM, who also advised on procedures and made informal comments on the results. The objective of the test program was to determine an optimum grind to reach desirable targets. To achieve this, characterization of the iron mineralization of 5 test samples was conducted through grind curve determination, low intensity magnetic separation (LIMS) and Blaine testing. The methods and results of the program are presented as Appendix 3, in a report by SGS Lakefield. The results of this program are summarized below; however, a review of the results by WGM is pending. Lurgi (1957) The Lurgi study included mineralogical examination and Davis Tube magnetic separation on various grind products, for composites from 40 drillholes. A roll crusher ground each sample to 20 mesh material and three, 1 kg splits were made. These coarse fractions were each ground 100% to three different sizes: -65 mesh (0.2mm), -200 mesh (0.074mm) and -325 mesh (0.044mm). Two, 30g splits were made from each of the pulps, and were subjected to Davis Tube separation. The tube parameters were constant for each test: a current intensity of 1.8 amperes and a tension of 115 volts, with a constant up/down motion and constant rate of flow. Analyses of Fe% and Fe++% were recorded for the head, magnetic concentrate and the non-magnetic tailings. Weight recovery values were calculated from these analyses. The 40 composite samples represented iron mineralization from 28 and 10 drillholes on the A and B Zones, respectively. The majority of the samples (20) were from drillholes on the far eastern part of the A Zone, closer to Jean Lake. An additional 5 samples were from drillholes on the east side of Kesaka Lake. Only three samples were from some of the early drillholes on the west side of Kesaka Lake. Material from these holes may have been used in earlier tests and may not have been available. The Fe% values of Lurgi head samples can be compared to three sources of historic data, including (1) Fe% sample results on drill logs and on sections (section samples), (2) composites indicated on the sections, and (3) the drillhole composites used by Hicks (1958), for his resource estimate.Only the report by Hicks has a complete composite listing for all drillholes which intersected iron formation. It was assumed that the numbering of both the Lurgi composites and Hicks’ downhole composites, represent the same drillhole source. With this assumption, a total of 32 composites common to each both the Lurgi and Hicks datasets were selected for comparison. These included only the composites which had both legible Lurgi results and only a single intercept for each hole. Drillholes with multiple intercepts, such as those cutting the A Zone South and A Zone or the two limbs of the B Zone West fold structure, were not included since it is unclear if the Lurgi samples included both intercepts.

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Figure 10, below, shows a comparison of the Fe% values for each composite set. The overall poor correlation shows that the analytical methods used for iron determinations were not equivalent. The common distribution of samples below the 1:1 line indicates that, for these samples, Fe% Lurgi values exceed the Fe% Hicks values. This implies that the analyses used by Hicks for his estimate, were only partial determinations of iron, while the analyses by Lurgi were of total iron. The analyses for soluble iron, as were common at this time, included iron from magnetite and hematite sources. Total iron analyses included iron from all sources, both oxides and silicates. In Figure 10, points closely associated with the 1:1 line represent samples containing mostly oxide (magnetite) sources. Those below the line represent samples containing variable amounts of silicates. In the absence of hematite, the samples with similar Fe% values for both Hicks and Lurgi analyses will therefore approximate the magnetic iron content (FeMt%) of the 2008 drillhole composites. For these samples, higher Fe% values compared with FeMt% values will indicate the presence of hematite.

FIGURE 10: COMPARISON of FE% GRADE for

DRILLHOLE COMPOSITES from HICKS and LURGI

Fe% (Hicks) vs Fe% (Lurgi) 32 Composite Pairs

20.00

25.00

30.00

35.00

40.00

20.00 25.00 30.00 35.00 40.00

Fe% Lurgi Composites

Fe%

Hic

ks C

ompo

sites

ALL Kesaka EastKesaka Far EastKesaka South

1:1 Line

The thin section reviews and Davis tube test results indicated that the iron mineralization is predominantly magnetite, with variable, but minor, amounts of hematite and iron bearing silicates (mostly as hornblende). A concentrate in the range of 68% to 71.5% could be obtained from feed material ground to 100% passing -325mesh. The results showed that, in general, grinding to the finer 325 mesh size could yield a higher iron grade and higher recovery than the coarser grinds. An exception to this was when the mineralization contained silicate-bound iron.

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In this case, with finer grinds, the grade increased but the recovery was less since a higher proportion of Fe reports to the tailings. A broader range of 60-94% iron recovery is a reflection of the variable proportions of iron bearing minerals. Hematite was reported in several samples, to greater than 10% for samples 59, 60, and 66, from the B Zone. Grind Curve Determination (2008) The objective of the grind curve determination was to estimate the required grind time to achieve the grind targets for Davis tube testing. From a plot of P99 against grind time, the estimated grinding times for each grind size (-200, -325, -400 mesh), from each sample, were tabulated. The results indicated that the samples were harder than anticipated and that the estimated grinding times were very long, averaging 932 seconds. To avoid causing the pot to heat up by long grind times, the samples were instead stage-pulverized until 100% passed the desired screen size. The hardness of the mineralization and possible intergrowth of gangue with magnetite was noted in previously in historical testwork by Lakefield (1957). Additional testing reported that improved results were possible with adjustments to procedures and instrumentation (Lakefield, 1957). Low Intensity Magnetic Separation (2008) For each of the five test samples, the resultant pulps from stage grinding to three sizes (-200, -325 and -400 mesh) were submitted for Low Intensity Magnetic Separation (LIMS) using a Davis tube. The objective of this preliminary testwork was to find the final grind required to achieve a magnetite concentrate containing less than 4% SiO2. The Davis tube feed for each sample and the magnetic concentrates from each grind size were submitted for whole-rock analysis, Satmagan determination, FeO, sulphur (S), and specific gravity (S.G.) using a gas pycnometer. Test sample details and the analytical results for the Davis tube feed (head samples) for each, as summarized in Table 9, below.

TABLE 9: SUMMARY of RESULTS for DAVIS TUBE FEED

SAMPLE DDH From_m To_mLitho Code Mt% TFe% FeMt% Hm%

Recovery FeMt%

5751 ES08-004 87.00 90.00 IFMJ 49.50 35.61 35.82 0.00 100.605752 ES08-004 126.00 129.00 IFML 39.10 31.97 28.29 0.00 88.495753 ES08-005 123.00 126.00 IFM 38.85 31.48 28.11 0.00 89.305754 ES08-006 126.00 129.40 IFMJ 46.05 35.82 33.32 3.19 93.035755 ES08-008 132.00 135.00 IFMJ 44.80 37.57 32.42 7.36 86.30

The above results show that the average head grade for TFe% is 34.5%. Higher TFe% results were obtained from the three samples (5751, 5754, 5755) of magnetite-jasper+/-chert facies (IFMJ) iron formation. Sample 5751 also had a closely equivalent FeMt% value of 35.82%, indicating that all of the iron contained in the sample occurs as magnetite. Samples 5754 and 5755 both had comparatively lower FeMt% results, suggesting that some of the iron is contained in other sources. The presence of iron as hematite is shown by elevated values for calculated hematite, of 3.19% and 7.36%. The higher hematite result for sample 5755 corresponds with the lowest recovery of 86.30%. Samples 5752 and 5753, also have lower FeMt% results compared with TFe%, but no hematite content is indicated. The results suggest that this difference, as well as the lower recoveries, may be due to the presence of iron as silicates. Samples 5752 and 5753 also had elevated sulphur S% results of 0.23% and 0.32%, while the other three samples have very low results ranging from 0.03% to 0.07%.

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Table 10, below, summarizes the results for analyses of the Davis Tube products from the various grinds for each sample. Sample 5751 had the highest weight recovery which ranged from 57.2% at -200 mesh, to 54.5% at -400 mesh. Sample 5754 had similar, but slightly lower weight recoveries which ranged from 55.4% at -200 mesh, to 53.1% at -400 mesh. Weight recoveries for the other samples were lower and ranged from 44.2% to 46.3%. Samples 5751, 5753 and 5755 produced concentrates with close to 70% iron (TFe%) and less than 5% SiO2. Fine grinding to -400 mesh was required to achieve these levels of silica liberation. The concentrates were all clean; with the alumina grade less than 0.3% and sulphur grades ranging from 0.01% to 0.08%. Overall, these test results corroborate those of historical metallurgical studies. Iron occurs mostly as magnetite and good iron recoveries are possible to yield a concentrate of approximately 70% iron and 5% SiO2. Grind tests indicated that the samples were hard and therefore required long grinding times, to fine grinds of -400 mesh, to approach the target SiO2 content of 4%. This was also encountered in historic tests conducted by Lakefield. Additional flotation testing was recommended. The Lurgi study also noted the general relationship that the iron grade of the concentrates increases with increasing fineness of the grind, while recoveries decrease. It was interpreted that only the finest levels of grinding can dissolve intergrowths between magnetite and hematite or silicate. Particles of hematite and silicate reported to the concentrate at coarser grinds, but reported to the tails at the finer grinds. The Davis tube products were not analyzed for SiO2 during this study. Hicks (1958) indicated that a Lurgi test reported that the “ …final concentrate assay was 70.8% iron and 2% silica and pellet assay 68.39% iron and 2.2% silica. Grind was 100 -325 mesh.” This is the first historic reference to concentrating test results which achieved target levels for a premium product.

TABLE 10: SUMMARY of RESULTS for DAVIS TUBE PRODUCTS

Sample Test Grind mesh Wt % Mt% T Fe% SiO2% S%5751 DT-1 Conc. -200 mesh 57.2 96.9 66.6 8.52 0.055751 DT-2 Conc. -325 mesh 57.1 98.6 66.9 7.05 0.035751 DT-3 Conc. -400 mesh 54.5 100.0 69.7 4.08 0.035751 Head 100.0 49.5 35.6 42.2 0.075752 DT-4 Conc. -200 mesh 46.3 92.7 63.9 11.0 0.085752 DT-5 Conc. -325 mesh 44.2 97.8 67.6 6.44 0.075752 DT-6 Conc. -400 mesh 44.2 98.2 68.1 5.63 0.085752 Head 100.0 39.1 32.0 45.3 0.235753 DT-7 Conc. -200 mesh 45.2 93.0 65.0 9.37 0.065753 DT-8 Conc. -325 mesh 44.3 98.3 67.8 6.14 0.065753 DT-9 Conc. -400 mesh 43.5 99.7 69.0 4.93 0.075753 Head 100.0 38.9 31.5 43.8 0.325754 DT-10 Conc. -200 mesh 55.4 92.2 63.7 11.3 0.025754 DT-11 Conc. -325 mesh 54.7 93.5 65.2 9.66 0.025754 DT-12 Conc. -400 mesh 53.1 99.9 68.5 5.58 0.025754 Head 100.0 46.1 35.8 41.2 0.055755 DT-13 Conc. -200 mesh 45.7 94.2 66.7 8.45 0.015755 DT-14 Conc. -325 mesh 43.9 97.7 69.7 4.00 0.015755 DT-15 Conc. -400 mesh 43.5 99.9 70.6 3.14 0.015755 Head 100.0 44.8 37.6 40.2 0.03

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Blaine Testing (2008) Upon consultation with WGM, additional testwork was requested by Raytec to analyze the fineness of the Davis tube feed and the magnetic concentrate. The objective was to determine if the minus 325 and 400 Davis tube concentrates would be appropriate for pelletizing. The minus 325 and 400 mesh Davis tube feeds were submitted for PSA and the magnetic concentrates of the corresponding sizes were submitted for Blaine air permeability test. This measures the specific surface area of a sample. The significance of the results are uncertain and remain to be reviewed by consultants of WGM. The Blaine results varied from 890 to 1170 cm3/g for the -325 mesh samples and from 1120 to 1250 cm3/g for the -400 mesh samples. For each of the samples, except 5752, the proportion of DT feed passing P80 decreased significantly with the finer grind. This sample has the highest proportion of silicates, with 30% bands of chloritic mudstone. Samples 5751, 5754 and 5755 had Blaine results which increased with the increased proportion of P80. These samples are all of magnetite facies iron formation with jasper bands. 11.0 QA-QC PROGRAM 11.1 DATA TREATMENT

For the 2008 exploration program, the drillhole collar information related downhole data for geology, structure, sample intervals, bulk density, geotechnical, and downhole surveys were first entered on hard copy log sheets in the field. This information was then entered into digital MS Excel spreadsheets, and later imported into an MS Access digital database. Handling of data was kept to a minimum through the use of calculations and queries based on the original input data. Analytical results for WRA, FeO and S, were received from SGS in hardcopy and electronic (by email) formats. The electronic results were received as CSV (comma delineated) files which were individually loaded in its original format, directly into the database. The Satmagan data was received in hardcopy and electronic (by email) formats, from Nick Lee. The electronic results were received as excel files which required some formatting before loading into the database. The results of each certificate were successively loaded into a “compiled” table for each analytical certificate source (WRA or SAT). Within these two tables, each entry was assigned a unique reference ID incorporating certificate number and order on the certificate. QA-QC codes were assigned to each entry. Each analytical value below detection limits was replaced with ½ of the lower detection limit, less 0.00001. Cells will no entries were populated with -99999. On the certficates for WRA and FeO analyses, lab standard 676-1 XRF is recorded; however, no results were indicated. The WRA, FeO, S, and Satmagan results in the compiled tables were subjected to QA-QC reviews of blanks, duplicates and standards from both field and laboratory sources. Details of the QA-QC sampling program are presented below. If the analytical results from each certificate were accepted, all non QA-QC samples coded as REG were loaded directly into the MASTER WRA_SAT table of the database. Duplicate sample results were successively averaged in the order of priority from lab duplicates, prep duplicates, to field duplicates and the results were loaded into the master table, with a unique sample number.

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The compiled results in the “MASTER_NEW_WRA_SAT” table were then forwarded to WGM for calculations of % hematite, as well as the % proportions of the total iron species as magnetite, hematite and other sources (silicate, carbonate), in each sample. This calculated data is preserved in the database as the “MASTER_NEW_CALC from WGM” table. These two master tables of results were imported into Mapinfo and Discover, together with other data tables of interest, and were used to general drill logs and drillhole sections. The data presented in the tables of this report were generated using queries within Mapinfo. 11.2 QA-QC SAMPLING PROGRAM SGS Mineral Services, of Lakefield, Ontario, was the primary laboratory used for analytical services and metallurgical testing. It is an accredited facility which meets the standards of ISO 9001 and ISO 17025:2005. To monitor the accuracy and precision of both the analyses and determinations completed by SGS, the 2008 QA-QC program included both field and laboratory components. These involved the insertion of random and blind material into the sample stream as blanks, standards and duplicates. A summary of the sampling program, by QA-QC sample type and analysis, is shown in Table 12. A total of 429 samples, including field blanks and duplicates, were submitted to the SGS for WRA, FeO analyses and Satmagan determinations. These samples represented 353 intervals of core. QA-QC samples from the field included the insertion of field blanks and the designation of duplicates. One sample of each was inserted into the sample stream as sequential numbers. Metal tags with sample details are stapled into the core boxes, at their location in the sample stream. Details were recorded on the drilllogs. A total of 20 intervals of unmineralized greywacke in the early drillholes were sampled and temporarily stored, for insertion into the sample stream as blanks. A total of 22 samples were designated as field duplicates. The remaining half core of the interval to be re-sampled was used as the duplicate sample. A wooden block labeled with duplicate details was placed in the core box to mark the gap. Since SGS indicated that, for their metallurgical testing, no internal QA-QC samples were inserted into the sample stream, Raytec decided to add 22 prep duplicates. These were not blind, so the lab could monitor them, and were suffixed –A an –B, to be different from the lab duplicates from analytical procedures. Lab duplicates were; however, done by both the analytical laboratory and the test facility. A total of 18 lab duplicates were done on the WRA and FeO samples, as well as 21 on the Satmagan determinations. A total of 13 lithium blanks were added to the sample stream, as well. Several different certified standards for whole rock(9), FeO(3) and S (2) analyses were also inserted into the sample stream. No standards were used for the Satmagan determinations, however, Nick Lee (pers comm.) reported that daily instrument calibrations were conducted. .

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TABLE 11: SUMMARY of QA-QC SAMPLING

SAMPLE TYPE ITEM CODE WRA FeO S SATTotal # of Sampled Intervals 353 353 5 353Total Samples Submitted* 429 429 5 429

Total Analyses* 558 558 22 463Blanks_Field* No. of Analyses FB 20 20 0 20

% of Total Analyses 3.58% 3.58% 0.00% 4.32%Blanks_Lab No. of Analyses LB 13 13 0 13

% of Total Analyses 2.33% 2.33% 0.00% 2.81%Duplicate_Field* No. of Analyses FD 22 22 0 22

% of Total Analyses 3.94% 3.94% 0.00% 4.75%Duplicate_Prep No. of Analyses FR 18 18 0 18

% of Total Analyses 3.23% 3.23% 0.00% 3.89%Duplicate_Lab No. of Analyses LD 18 18 0 21

% of Total Analyses 3.23% 3.23% 0.00% 4.54%Standards_Lab No. of Analyses LS 24 37 2 0

% of Total Analyses 4.30% 6.63% 9.09% 0.00%Standards_Lab #Used 9 3 2 0

Total Samples Submitted*: From field to laboratory, includes test and routine samples, field blanks, field duplicatesTotal Analyses*: Includes total samples submitted, prep duplicates, 15 metallurgical samples, lab QAQC samplesBlanks_Field*: These are from sampled intervals of greywacke from select holes which were reinserted as blanksDuplicate_Field*: One of these samples was also run as a prep duplicate (16265).Duplicate_Field*: Three of these samples were also run as lab duplicates for WRA and FeO (16355, 16388, 16582).Duplicate_Prep*: One of these samples was also run as a lab duplicate for WRA and FeO (5805B)

11.3 QA-QC RESULTS WRA, FeO and S The total number of analyses for WRA and FeO was 558. These were completed on the submitted samples, both field and laboratory QA-QC samples, as well as the Davis Tube concentrates derived from the 5 test samples. The field QA-QC program included the insertion of blanks (from sampled intervals of greywacke) and the collection of field duplicates. The laboratory QA-QC program included the insertion of certified blanks and standards, as well as the sampling of selected prep duplicates (as indicated by Raytec) and laboratory duplicates. A review of the field and laboratory blanks indicated that gross errors related to sampling handling or data transfer were not detected. The results showed no signs of contamination. In Figures 11,12 and 13, the various duplicate results for Fe2O3 and SiO2 all show good correlations between sample pairs, indicating high levels of precision. Similar levels of precision were shown for duplicates of FeO. Table 12 shows that the averaged results for inserted laboratory standards for WRA, FeO and S were all within acceptable levels. Figures 14a,b show the standard results by batch. Based on these results, the QA-QC samples for WRA, FeO and S demonstrated good precision and accuracy.

56

% Fe2O3 Lab Duplicates 18 Sample Pairs

y = 1.0011x - 0.0283R2 = 0.9999

0.00

10.00

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40.00

50.00

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70.00

0.00 10.00 20.00 30.00 40.00 50.00 60.00 70.00

% Fe2O3 Original (Dup 1)

% F

e2O

3 D

uplic

ate

(Dup

2)

Series1 1:1 Line Linear Best Fit Line

FIGURE 11a: COMPARISON OF LAB DUPLICATES (Fe2O3)

% SiO2 Lab Duplicates 18 Sample Pairs

y = 0.9811x + 0.8767R2 = 0.999

0.00

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80.00

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% SiO2 Original (Dup 1)

% S

iO2

Dup

licat

e (D

up 2

)

Series1 1:1 Line Linear Best Fit Line

FIGURE 11b: COMPARISON OF LAB DUPLICATES (SiO2%)

57

% Fe2O3 Prep Duplicates 18 Sample Pairs

y = 1.0074x - 0.2348R2 = 0.9677

0

10

20

30

40

50

60

70

0 10 20 30 40 50 60 70

% Fe2O3 Original (Dup 1)

% F

e2O

3 D

uplic

ate

(Dup

2)

Series1 1:1 Line Linear Best Fit Line

FIGURE 12a: COMPARISON OF PREP DUPLICATES (Fe2O3)

% SiO2 Prep Duplicates 18 Sample Pairs

y = 0.9812x + 0.7123R2 = 0.9253

0

10

20

30

40

50

60

70

0 10 20 30 40 50 60 70

% SiO2 Original (Dup 1)

% S

iO2

Dup

licat

e (D

up 2

)

Series1 1:1 Line Linear Best Fit Line

FIGURE 12b: COMPARISON OF PREP DUPLICATES (SiO2)

58

% Fe2O3 Field Duplicates

22 Sample Pairs

y = 0.9899x + 0.7626R2 = 0.9784

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70.00

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% Fe 2O3 Original (Dup 1)

% F

e2O

3 D

uplic

ate

(Dup

2)

Series1 1:1 Line Linear Best Fit Line

FIGURE 13a: COMPARISON OF FIELD DUPLICATES (Fe2O3)

% SiO2 Field Duplicates 22 Sample Pairs

y = 0.9644x + 1.7265R2 = 0.9016

0.00

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30.00

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50.00

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70.00

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% SiO2 Original (Dup 1)

% S

iO2

Dup

licat

e (D

up 2

)

Series1 1:1 Line Linear Best Fit Line

FIGURE 13b: COMPARISON OF FIELD DUPLICATES (SiO2)

59

TABLE 12: SUMMARY of LABORATORY STANDARDS for IRON

Sample_ID CountStd

Fe2O3% Average

Fe2O3 %Std

FeO% Average FeO%

681-1, Iron Ore, SETT 12 8.70 8.54FER-1, SETT 13 23.34 23.30FER-2, SETT 12 15.24 15.43SARM4 XRF 6 8.97 9.06 680-1 XRF 8 85.75 85.65 SY4 XRF 1 6.21 6.27 681-1 XRF 3 47.48 47.60 SARM42 XRF 1 4.68 4.71 NIST-690 XRF 1 95.56 95.80 SARM-1 XRF 1 2.00 1.92 SO3 XRF 1 2.25 2.14 SARM-12 XRF 2 95.21 95.55

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Fe2O3 Results for SGS Lab Standards by Certificate Order (23 Samples)

0.00

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80.00

90.00

100.00

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14

Certificate Order

% F

e2O

3

680-1 XRF681-1 XRFNIST-690 XRFSARM-1 XRFSARM-12 XRFSARM4XRFSO3XRFSY4 XRF

FIGURE 14a: RESULTS for LABORATORY STANDARDS (Fe2O3)

Fe2++ as FeO Results for SGS Lab Standards by Certificate Order (37 Samples)

0.00

5.00

10.00

15.00

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25.00

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14

Certificate Order

% F

e2++

as

FeO

681-1, Iron Ore, SETT

FER-1, SETT

FER-2, SETT

FIGURE 14b: RESULTS for LABORATORY STANDARDS (FeO)

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SATMAGAN

The total number of Satmagan determinations was 463. These were completed on the submitted samples, both field and laboratory QA-QC samples, as well as the Davis Tube concentrates derived from the 5 test samples. The field QA-QC program included the insertion of blanks (from sampled intervals of greywacke) and the collection of field duplicates. The laboratory QA-QC program was limited to daily calibration of the instrument, sampling of selected prep duplicates (as indicated by Raytec) and laboratory duplicates. No internal standard or blanks were inserted into the sample stream. Numerous gross errors due to human handling, data transfer and data entry were detected in the Satmagan results. These errors were detected in field blank results and in wide discrepancies for duplicate pair results. Raytec requested additional and specific samples to be re-run; SGS also checked additional samples and revised the results. Reviews of the final lab, prep, and field duplicate results are shown in Figures 15a, 15b, and 15c. The results for each show good, acceptable levels of correlation. No internal standards were run by the laboratory, so there is no reliable estimate of the accuracy of the Satmagan determination. It was noted that 63 of the 407 sample intervals returned FeMt% results which were higher than TFe%. As well, the comparisons of bulk density-specific gravity with TFe% and FeMt%, correlations were notable better for TFe% than for FeMt%. These observations raise concerns in the accuracy of the determinations. It is possible that errors may have developed in the exist in the calibration or in inhomogeneous sample preparation and handling.

% Magnetite (Satmagan) Lab Duplicates 21 Sample Pairs

y = 1.0029x - 0.0749R2 = 0.9999

0.00

10

20.0

30.0

40.0

50.0

60.0

0.00 10 20.0 30.0 40.0 50.0 60.0 70.0

% Magnetite Original

% M

agne

tite

Dup

licat

e

Series1 Linear Best Fit Line

FIGURE 15a: COMPARISON OF LAB DUPLICATES (Satmagan)

62

% Magnetite (Satmagan) Prep Duplicates 18 Sample Pairs

y = 0.9998x - 0.1158R2 = 0.9974

0.00

10

20.0

30.0

40.0

50.0

60.0

0.00 10 20.0 30.0 40.0 50.0 60.0 70.0

% Magnetite Original

% M

agne

tite

Dup

licat

e

Series1 Linear Best Fit Line

FIGURE 15b: COMPARISON OF PREP DUPLICATES (Satmagan)

% Magnetite (Satmagan) Field Duplicates 22 Sample Pairs

y = 0.9975x + 0.3932R2 = 0.9842

0.00

10

20.0

30.0

40.0

50.0

60.0

0.00 10 20.0 30.0 40.0 50.0 60.0 70.0

% Magnetite Original

% M

agne

tite

Dup

licat

e

Series1 Linear Best Fit Line

FIGURE 15c: COMPARISON OF FIELD DUPLICATES (Satmagan)

63

12.0 INTERPRETATION AND CONCLUSIONS The stratigraphy encountered in both historic and recent drillholes is consistent with a basinal shelf succession with possible contributions from volcanism. The gradation of the succession from coarse sediments fining upwards into iron formation and tuffs, is typical of Algoma iron formation deposits. Along the A Zone, the iron formation is thickest in the Kesaka East area, and thins to both the east and west, where it has been thickened by ductile deformation in successive folding and shearing events. The lithological and structural trends, as interpreted from geophysics and observed in drill core, indicate that the rocks of the El Sol property lie within a corridor of intense ductile strain. The observed patterns and fabrics are consistent with a deformational history which has been described in English River Subprovince, to the west (Hrabi and Cruden, 2006). The stratigraphy underlying the El Sol property has been deformed by successive D2 and D4 folding events and subsequent D5 ductile shearing within the Sydney Lake fault zone. Regionally, the stratigraphy within D2 folds has been repeated by EW trending D4 folds. The trend of the A and B Zone horizons of iron formation outline the limbs of an upright synclinal D4 fold structure. The southern limb of the fold, along the B Zone, has been overturned and is inclined to the south. The isolated zones of interpreted iron formation in the core of this structure may be D2 fold repetitions of the A-B horizon, which have been subjected to D4 folding and later disrupted by D5 dextral oblique shearing associated with the Sydney Lake fault. The dominant fabrics observed in drillcore and reported in outcrop (Bowen, 1984) are a strong, vertical to steeply south dipping cleavage and lineations which plunge steeply to the west. These structures are interpreted as products of widespread east-west trending D5 ductile shearing. The shearing has caused localized tightening of earlier folds, high levels of transposition of parallel (EW trending) stratigraphy and earlier fabrics, as well as disruption of oblique stratrigraphy. In the Kesaka Far East area, D4 folds have been recognized by the repetition of the different facies of iron formation and quartz porphyry within drillholes. Possible limbs of tightened D4 fold(s) were recognized within asymmetrically folded stratigraphy of drillholes ES08-005 and ES08-007. Several orders of smaller asymmetrical D4 fold and related fabrics were recognized in drillcore, but they have mostly been transposed by later shearing. Asymmetrical folding related to dextral shearing is commonly observed in drillcore and are noted as interference patterns of “refolded folds” which have moderately to steeply south dipping axial planes. Local boudinaged and disrupted banding are also products of this event. Some repetition of stratigraphy within drillholes (albeit on a smaller scale than the D4 folding) may be along the D5, subvertical fold axes. Hicks’ data indicates that horizontal widths of iron formation drilled along the A and B Zones averaged 44 metres. Thicker widths of 60 to 70 metres were intersected in some holes in the Kesaka East and Kesaka Far East areas. Progressively thinner widths to the west were intersected by drillholes in the Kesaka West area. The greatest widths of up to 90 metres were intersections through a fold nose at the western end of the B Zone. The horizontal widths vary due to fold thickening.

64

In the 2008 drillholes, thick horizontal widths of up to 68 metres were encountered, however internal dilution due mostly to infolded quartz porphyry, varied from 0 to 41%. The dilution accounts for overall lower composite grades for some drillholes in the Kesaka Far East area. On the historical drill sections and drill logs, few sections of internal dilution were noted. This suggests that the dilution due to folding may be a local effect due to polyphase folding. It may, therefore, have an overall low dilutive effect to the overall grade of the iron formation. The 2008 samples of drillcore consisted mostly by magnetite dominant facies of IFM and IFMJ. A lower proportion of the samples were of facies IFML, which has a variable silicate content as bands of chloritic mudstone. A comparison of the total iron (TFe%) and magnetic iron (FeMt%) content of these samples indicates that most of the iron sampled occurs as magnetite. Hematite contents of 1-10% were associated with some samples. This was also noted in the Lurgi Davis Tube results, as well as within thin sections. The FeMt% grades for the 2008 composites ranged between 20.50% to 33.20%, due to infolding of dilutive lithologies. In comparison, the FeMt% composited grade of the samples with >10% FeMt had ranges of 29.20% to 32.76%. This shows that the iron formation on the A Zone has a relatively consistent grade range, related to relative magnetite proportions. In the resource calculations completed by Hicks (1958), the grade of sectional panels varies between 28-30% Fe and 30-33% Fe. The higher grade panels represented drilling in the area of the A Zone Kesaka East and B Zone Kesaka South areas. Since the Fe% analysis included hematite, but not silicate, the higher grade panels may be areas with a greater proportion of magnetite and/or hematite facies (IFM, IFMJ). This could be due to facies changes within the iron formation and/or fold thickening. The greatest variability was within A Zone panels of the Kesaka Far East area, where grades ranged from 23.7% Fe to 34.5%. The grade variability in this area may be due to infolding of greater proportions of lean iron formation and/or quartz porphyry. The historical drilling on the El Sol property defined the strike extent of the iron formation on the A and B Zones. The depth extent, however, has only been well tested in the Kesaka West area, which is the thinnest part of the A Zone. Multiple holes were drilled on only four sections in the Kesaka FarEast area, and one section in the Kesaka West area. The only area tested by multiple drillholes on the B Zone was at the western fold nose. Hicks’ calculations of tons per vertical foot were extrapolated to a depth of 1000 feet (305 metres). This is supported by little drilling evidence to depth, however. A tonnage factor of 10 was also used, which is equivalent to a specific gravity of 3.22. During this program, the SG and bulk densities of the iron bearing samples and quartz porphyry averaged 3.45 and 2.77, respectively. Hicks’ calculations of tonnages per vertical foot, compared to grade, provide a general indication of the relative potential of the different areas of the iron formation. The Fe% analysis used for grade included hematite and therefore the historical results may have been higher than those which would be obtained from current Davis Tube tests. If, within the higher grade panels, increased grade reflects increased hematite content, the overall grade of FeMt% in these areas may be lower than the historic Fe% grade. The variable Fe% grades in the Kesaka Far East area suggest that additional drilling to depth is required in this area.

65

Historical metallurgical results consistently show that magnetic separation of samples from the iron formation can yield good iron concentrate grades with good recoveries. Head samples and concentrates returned low levels of deleterious elements and are considered to be “clean”. Lurgi reported that a premium concentrate product of 70% iron and 2% silica was possible at a grind of 100% passing 325 mesh. Specifics associated with this determination are not available. The Davis Tube results from this program also yielded similar iron grades and recoveries. Finer grinds to –400 mesh were required to reach SiO2 levels approaching the target of 4%. Metallurgists from SGS have recommended additional testing of other beneficiation methods, with a goal of lowering the silica content of the concentrate, while minimizing grinding. The combined results from historical and recent programs, have demonstrated the potential of the property to host an iron resource which could generate a metallurgically desirable product. The Davis tube results from this program corroborated those reported by Lurgi and Hicks, indicating that a suitable, clean concentrate product could be obtained. Iron mines are usually large scale operations, with an economy of scale that can overcome expensive transportation and processing. Marketing of a product, therefore, also depends on several resource factors which include the size and grade of the resource, as well as the characteristics of the ore. The definition of iron resources in the vicinity of the El Sol project, therefore, may also contribute to future viability through infrastructure, transportation and marketing synergy.

66

13.0 RECOMMENDATIONS An acquisition strategy is an important part of the overall potential of the El Sol property. It is therefore a priority of the project to identify other iron formation prospects in the vicinity, with which future synergy may possible. Regional deformation patterns suggest that these occurrences may be at the same stratigraphic level within the basin, and may be chemically similar. Further exploration of the El Sol property is recommended in two Phases, as outlined below. The objective of these activities are firstly, to identify a suitable beneficiation process which can generate a concentrate with high iron and low silica contents, with minimal grinding, and secondly, to define a NI43-101 compliant resource through diamond drilling. Exploration activities should be conducted during the winter. The frozen ground conditions allow easier access for drill rigs and heavy equipment, while minimizing environmental impact. The proposed drilling represents a program which tests areas which are in accessible during the summer. Positive results from the metallurgical testing and diamond drilling of this program will warrant additional drilling to generate a NI43-101 estimate. PHASE 1 (pre drilling)

• Engage the consultants of WGM to provide monitoring and interpretation of the Phase 1 testwork, as well as to provide recommendations for resource level drilling targets and QA-QC procedures for the drill program.

• Send a proportion of samples to Midland Research Centre for check assaying and testwork.

This will provide a comparison of different methods and also checks on the Satmagan results. • Conduct additional metallurgical testing to investigate different beneficiation methods, such as

reverse flotation. Larger scale, drillhole composites should be used.

• Conduct ground magnetic surveying over Kesaka Lake, to confirm the position of the iron formation under the lake. This data will be merge with the 2008 survey and used for targeting.

• Conduct thin section reviews of iron formation samples, as well as selected concentrates, to

assess possible magnetite intergrowths which may be affecting liberation. Review samples of quartz porphyry to determine if it is intrusive (dyke) or tuffaceous. This affects the validity of this unit as a marker horizon within the succession.

• Establish a strict data entry and QA-QC protocol, suitable for resource level work.

• Acquire commercial iron standards for use as field standards, or alternatively, generate a

property specific standard from the rejects of 2008 samples.

• Initiate communications with stakeholders in the area, including the Lac Seul First Nation.

67

PHASE 1 (drilling)

• Construct a winter road from the Maskooch Lake clear cut area to the north of the property. 2008 field reconnaissance suggest that a level road on a good bed of coarse glacial debris could access the property from the northeast.

• Conduct a minimum of 4000 metres of winter drilling to confirm strike and depth extent on

the A and B Zones. A few holes should also test the central magnetic anomalies.

• Based on the Phase 1 tests, conduct Davis Tube tests on all samples with total iron and FeO analyses completed on the head samples and concentrates. A proportion of these samples (5%) should also be analyzed for sulphur and trace elements. A proportion of the tailings (5%) should also be analyses for total iron, FeO, sulphur and trace elements. All products are to be retained.

• Ensure that QA-QC procedures for the metallurgical determinations are documented and

executed. The internal results should be obtained.

68

TABLE 13: BUDGET PROPOSAL FOR 2010 ACTIVITIES CONTRACTS NO. # Unit # Units RATE Aircraft Charters 1 flights 6 500$ 3,000$ Camp Mob/Demob 1 1 15,000$ 15,000$ Camp Rental 1 month 2 15,000$ 30,000$ 48,000$ Ground Geophysics Mob/Demob 1 1 3,000$ 3,000$ Ground Geophysics Survey, incl. linecutting 1 1 25,000$ 25,000$ 28,000$ Winter Road and Maintenance (incl fuel) 1 1 30,000$ 30,000$ 30,000$ Drill and Crew Mob/Demob to camp 1 1 15,000$ 15,000$ Diamond Dril ling-Operating Costs 1 metres 4000 100$ 400,000$ Diamond Dril ling-NonOperating Costs 1 hours 400 150$ 60,000$ Diamond Dril ling-Rentals (downhole survey) 1 months 2 1,500$ 3,000$ Diamond Dril ling-Consumables-steel 1 1 5,000$ 5,000$ Diamond Dril ling-Consumables-coreboxes 1 NQ corebox 800 15$ 12,000$ 495,000$ CONSULTING NO. # Unit # Units RATE Geophysicist 1 $/day 5 800$ 4,000$ Watts, Griffis, McOuat 1 1 25,000$ 25,000$ 29,000$ ANALYTICAL NO. # Unit # Units RATE Metallurgical Testing-SGS 1 1 65,000$ 65,000$ Standard Purchase 2 standards 1 1,500$ 3,000$ Petrography 1 1 3,000$ 3,000$ Rock samples-Check Analyses 1 samples 80 50$ 4,000$ 75,000$ Rock samples-Davis Tube tests, assays 1 samples 750 250$ 187,500$ 187,500$ PROJECT SUPPORT and SUPPLIES NO. # Unit # Units RATE Travel Airfare, Hotels, Meals 6 flights 1 750$ 4,500$ Hotel and Meals 40 mandays 1 125$ 5,000$ Room and Board (Camp) 14 mandays 65 40$ 36,400$ Field durables 3,000$ Field expendibles (include rock saw blades) 3,000$ Camp expendibles 1 6,000$ Fuel Diesel (Drill) 2 days 60 200$ 24,000$ Fuel Diesel (Camp) 1 days 60 200$ 12,000$ Fuel-Gas 1 days 10 325$ 3,250$ Fuel Propane (Drill) 2 days 45 160$ 14,400$ Fuel Propane (Camp) 1 week 7 160$ 1,120$ Rentals-First Aid Equipment, Spill Kits 1 days 50 75$ 3,750$ Rentals-Vehicles 2 month 2 1,500$ 6,000$ Rentals-Rock Saw 1 month 2 1,500$ 3,000$ Snowmobile 2 days 60 85$ 10,200$ Freight-Land 4,000$ Expediting Services 5,000$ Communications, Radio Rentals 5,000$ 149,620$ MISCELLANEOUSDrill Core and Sample Storage 4,000$ Land Use Permits, Consultations 4,000$ 8,000$ WAGES NO. # Unit # Units RATE SUBTOTAL TOTALGeologist 1 $/day 100 600$ 60,000$ Geotechnician 1 $/day 125 350$ 43,750$ Camp Manager 1 $/day 60 450$ 27,000$ Labourers, Cooks Helper, Camp Helper 3 $/day 60 250$ 45,000$ Cook/First Aid Attendant 1 $/day 60 500$ 30,000$ 205,750$ COMPILATION and REPORTING NO. # Unit # Units RATE Data Compilation and Reporting 15,000$ Drafting and GIS 4,500$ Printing, Copying, Reference Material 2,500$ Courier Charges 600$ 22,600$

Subtotal 1,278,470$ Management 93,722$ Contingency 10% 127,847$

TOTAL : 1,500,039$

69

14.0 REFERENCES Allen, Gordon, P., 2008. Assessment Report on Line Cutting and Magnetic and VLF-EM Surveys on the Avis Lake (EL Sol) Property, Red Lake Mining Division. For Raytec Metals Corp.

Batelle Institute,1957. Letter covering proposed investigation., July 18th 1957. On file with the Ministry of Northern Development and Mines in Red Lake.

Bowen, R.P., 1981. Precambrian Geology of the Slate Lake Area, East Sheet, Kenora District (Patricia Portion); Ontario Geological Sruvey Preliminary Map P.2408, Geological Series, Scale 1:15840 or 1 inch to ¼ mile. Geology 1980.

Bowen, R.P., 1984. Geology of the Slate Lake Area, District of Kenora, Patricia Portion, Ontario Geological Survey Open File Report 5471.

Bowen, R.P., 1989. Geology of the Slate Lake Area, District of Kenora, Patricia Portion, Ontario Geological Survey Report 256 Bowen, R.P. 1989; Slate Lake Area, District of Kenora (Patricia Portion); Ontario Geological Survey, Map 2517, Precambrian Geology Series, scale 1:31 680. Geology 1980. Gross, G.A., 1973, The depositional environment and principal types of Precambrian iron-formation, in Genesis of Precambrian iron and manganese deposits, Proceedings of the Kiev Symposium, 1970: UNESCO Earth Sciences 9, p. 15-21. Gross, G.A., 1980, A classification of iron-formations based on depositional environments: Canadian Mineralogist, v. 18, p. 215-222. Hicks, H. Brodie, 1957. Transportation Report, February 1957. Hicks, H. Brodie, 1958. Report on El Sol Mines Limited Iron Ore Properties, Red Lake Mining Division, Ontario. An internal report prepared for El Sol Gold Mines Ltd, February 26, 1958. On file with the Ministry of Northern Development and Mines in Red Lake. Hrabi, B., and Cruden, A.R., 2006. Structure of the Archean English River subprovince: implications for the tectonic evolution of the western Superior Province, Canada. Canadian Journal of Earth Sciences, Volume 43. Huston, Carl, D., 2006. Compilation Report, Avis Lake Area, Red Lake Mining Division, Ontario, Canada. Lakefield Research Ltd., 1956. Preliminary Investigation, December 17th, 1956 Lakefield Research Ltd., 1957a. Progress Report #2, February 15th, 1957. Investigation by D.M. Wyslousi for El Sol Gold Mines Ltd.. On file with the Ministry of Northern Development and Mines in Red Lake. Lakefield Research Ltd., 1957b. Progress Report #3, April 18th , 1957. Investigation by D.M. Wyslousi for El Sol Gold Mines Ltd. On file with the Ministry of Northern Development and Mines in Red Lake.

70

Lakefield Research Ltd., 1957c. Progress Report #4, June 12th , 1957 On file with the Ministry of Northern Development and Mines in Red Lake. LURGI Gesellschaft fur Chemie und Huttenwesen, 1957. Report on Magnetic Separation and Pelletizing Tests carried out on Drill Core Samples from El Sol Gold Mines Ltd, Toronto, Ontario, executed in the pilot plant of LURGI. Autumn, 1957. On file with the Ministry of Northern Development and Mines in Red Lake.

Montgomery, W.R., 1957, Report on the Property of El Sol Gold Mines Limited, Kesaka Lake, Red Lake Mining Division, Northwestern Ontario. An internal report prepared for El Sol Gold Mines Ltd. On file with the Ministry of Northern Development and Mines in Red Lake.

Ontario Department of Mines, 1940, Geology and Gold Deposits of the Uchi- Slate Lakes area Ontario Department of Mines Annual Report for 1939, Volume 48, Part 8, p. 1-43. Ontario Department of Mines-Geological Survey of Canada, 1960, Aeromagnetic series Maps 871G, 872G, 882G, 831G. Flown 1959 Ontario Geological Survey, 1991. Airborne electromagnetic and total intensity magnetic survey, Birch-Uchi-Confederation Lakes area, Ontario Geological Survey, Maps 81656, 81657, Scale 1:20,000.

Ontario Ministry of Northern Development and Mines, 1991, Birch- Uchi-Confederation Lakes area, Airborne Electromagnetic Survey, Total Intensity Magnetic Survey maps 81656, 81657.

Panagapko, D.A. and Gibson, J.C., 1980. Avis Lake Area, District of Kenora (Patricia Portion); Ontario Geological Survey Preliminary Map P.2018, Red Lake Data Series, Scale 1:15,840 or 1 inch to ¼ mile. Data compiled 1979. Risto, R., Kociumbas, M.W., and El-Rassi, D., 2008. Technical Report on the Peppler Lake Iron Project, Quebec, for Quinto Mining Corporation. Filed on Sedar. Ross, H.U., 1957a. Report on Iron Ore Concentration Tests, January 12th , 1957. Internal Report for Newkirk Mining Corp. On file with the Ministry of Northern Development and Mines in Red Lake. Ross, H.U., 1957b. Letter Report on Iron Ore Concentration Tests, February 28th , 1957. Internal Report for El Sol Gold Mines Ltd. On file with the Ministry of Northern Development and Mines in Red Lake. Ross, H.U., 1957c. A Comparative Study of the Pelletizing Process and the Krupp-Renn Process, June 4th, 1957. On file with the Ministry of Northern Development and Mines in Red Lake. Segsworth, R.B., 1957. Preliminary Estimate of Cost of Mining El Sol, with indicated Profits, May 6th, 1957. Internal Report for El Sol Gold Mines Ltd. On file with the Ministry of Northern Development and Mines in Red Lake. Shklanka, Roman, 1968, Iron Deposits of Ontario, Ontario Department of Mines, Mineral Resources Circular No. 11.

SIGNATURE PAGE

This report titled "2008 Exploration Report on the El Sol Iron Project, Northwestern Ontario", for Raytec Metals Corp. (now Lion Energy Corp.), and dated November 20th, 2009, was prepared and signed by the following author:

Dated at Vancouver, BC November 20, 2009

71

CERTIFICATE OF QUALIFICATIONS

I, Janice L. Fingler, of business address of 1409-675 West Hastings Street in the city of Vancouver, in the province of British Columbia, certify that:

1. I am an independent consulting geologist providing exploration services to the mineral exploration community.

2. I am a member in good standing with the Association of Professional Engineers and Geoscientists of British Columbia (2 1 566).

3. I am a graduate of the University of Manitoba with a Bachelor of Science (Honors) in Geology in 1985 and a Master of Science in Geology in 1991.

4. I have practiced my profession continuously since 1985 and have been involved in projects and evaluations exploring for precious metals, base metals, and industrial minerals in Canada, Mexico, South and Central America and Russia

5. I am independent of Lion Energy Corporation. I do not, indirectly or directly, hold any shares in the company.

6. I have prepared this reported, titled. "2008 Exploration Report on the El Sol Iron Project, Northwestern Ontario", dated November 201

h, 2009. I supervised the activities described in this report, on behalf ofRaytec Metals Corp. (now Lion Energy Corp.).

Dated at Vancouver, BC, this 20th day of November, 2009

72

2008 EXPLORATION REPORT

on the

EL SOL IRON PROJECT

For

RAYTEC MINING CORPORATION

(now LION ENERGY CORPORATION)

APPENDIX 1 Listing of Contractors and Services

November 20th, 2009 J. Fingler, M.Sc., P.Geo

J. Fingler Geological

EL SOL IRON PROJECT LISTING of CONTRACTORS and SERVICES USED Contractor/Business Address Services Provided Dates

Hy‐tech Drilling Red Lake, ON Diamond Drilling Oct 2‐Oct 27, 2008Forest Helicopters Kenora, ON Helicopter Sept 30‐Nov 3, 2008CJL Enterprises Smithers, BC Drill/Heli Pad Construction Sept 28‐Oct 27, 2008Clearview Geophysics Brampton, ON Ground Magnetics Survey Oct 6‐Oct 18, 2008Eric Rody, O.L.S. Kenora, ON Surveying Nov 2, 2008Intrepid Geophysics N. Vancouver, BC Geophysical Imaging Jan 2009Ackewance Madsen, ON Camp services, support, supplies Sept 25‐ Nov 2,2008Ackewance Madsen, ON Core shack, personnel Nov 2‐Nov 20, 20081984 Inc.  Vancouver, BC First Aid attendant, gear Sept 30‐Oct 27, 2008Trillium Motel Ear Falls, ON Accomodation, meals Sept‐Nov, 2008Howey Bay Motel Red Lake, ON Accomodation, meals Oct‐Nov, 2008Nature's Inn Balmertown, ON Accomodation, meals Oct‐Nov, 2008Woman River Camp Ear Falls, ON Cabin Rental  Oct 2008Gardewine Red Lake, ON Truck Freight  Nov 2008Barrens Northern Red Lake, ON Truck Freight Oct, Nov 2008Deakin Equipment Vancouver, BC Field Supplies Sept, Oct 2008Chaltrek Suppllies Thunder Bay, ON Field Supplies Oct, Nov 2008SGS Mineral Services Lakefield, ON Analyses, Metallurgy testing Nov 2008‐Aug 2009Kay Air Ear Falls, ON Float Plane Sept, Oct 2008Bearskin Airlines Red Lake, On SKED flights and cargo Sept‐Nov, 2008G. Allen Duncan, BC Truck Rentals Sept‐Nov, 2008Terracad GIS Vancouver, BC GIS and Database Post programMcElhanney Vancouver, BC GIS and Drill Sections Post programJ. Fingler Vancouver, BC Geologist Sept 2008‐Nov 2009J. Thurston Vancouver, BC Geotechnician Sept 25‐Nov 20, 2008B. Mankelow Duncan, BC Field Assistant: Pad and trail cutting Sept 25‐Oct 29, 2008Cam Schellenberg Duncan, BC Field Assistant: Pad and trail cutting Sept 25‐Oct 29, 2008

2008 EXPLORATION REPORT

on the

EL SOL IRON PROJECT

For

RAYTEC MINING CORPORATION

(now LION ENERGY CORPORATION)

APPENDIX 2 Statement of Costs

November 20th, 2009 J. Fingler, M.Sc., P.Geo

J. Fingler Geological

EL SOL IRON PROJECT 2008 DRILLING/GEOPHYSICS PROGRAM ASSESSMENT COST ALLOCATIONS

Cost  Cost Assessment Pro Rata Items drilling metres/claimAssessment Summary Summary Summary 8% 17% 75%Category Detail Unit Unit Rate Pre Post Totals KRL3019665 KRL3019666 KRL3019667Accomodation Room, board in Red Lake 898$             5,618$         6,516$             521$                 1,108$              4,887$             Analytical Prep, Metallurgy, Density 41,198$       41,198$          3,296$              7,004$              30,898$           Analytical Routine Analyses 424 samples $99.50/ea 42,188$       42,188$          3,375$              7,172$              31,641$           Camp Services Rental, supplies, food, phones 36,735$       22,362$       59,097$          4,728$              10,046$            44,323$           Camp Support Cook, First Aid, personnel 19,300$       13,575$       32,875$          2,630$              5,589$              24,656$           Data and Report J. Fingler_Office 30 days $600/day 18,000$      18,000$         1,440$             3,060$             13,500$          Data and Report J. Thurston_Office 3 days $350/day 500$             500$               40$                  85$                  375$               Data and Report Report Formatting, Print 1,050$         1,050$            84$                  179$                788$               Data Support GIS, Database, Imaging 3,650$         3,650$             292$                 621$                 2,738$             Drill/Heli Pads Drill Pad Building 30 days $800/day 16,000$       8,000$         24,000$          1,920$              4,080$              18,000$           Drilling Drilling 2301 metres $125.15/m 168,833$     119,140$     287,972$        23,038$            48,955$            215,979$        Field Supervision J. Fingler_Field 57 days $600/day 13,800$       20,400$       34,200$          2,736$              5,814$              25,650$           Field Supplies Various 525$             3,880$         4,405$             352$                 749$                 3,304$             Field Support W. Desmueles 14 days $325/day ‐$                  4,550$         4,550$             364$                 774$                 3,413$             Field Support B. Mankelow, C. Schellenberg 70 days $150/day 6,900$         3,600$         10,500$          840$                 1,785$              7,875$             Field Support J. Thurston 57 days $350/day 8,050$         11,900$       19,950$          1,596$              3,392$              14,963$           Freight Camp and Drillcore Mob/Demob 7,962$         7,962$            637$                1,354$             5,972$            Geophysics Geophysics Survey, transport 13 days $2093.57/day 27,216$      27,216$         2,177$             4,627$             20,412$          Geophysics Geophysics Report 1,500$         1,500$            120$                255$                1,125$            Surveying Surveying of Collars 1,615$         1,615$             129$                 275$                 1,211$             Transportation Helicopter 132.5 hours $1728/hr 124,762$     104,198$     228,960$        18,317$            38,923$            171,720$        Transportation Truck, fixed wing 4,900$         5,250$         10,150$          812$                 1,726$              7,613$             TOTALS 427,919$    440,135$    868,054$       69,444$           147,569$        651,041$       

05/02/2010 08:10 204-483-3541 P ENGLISH PAGE 01101

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f')h

t -:> r Ontario Ministry of

Northern Development and Mines

Assessment Work Performed on Mining Lands Transaction Number (office use)

W-

Mining Act, Subsections 65(2) and 66(3), R.S.O. 1990 Submission 2.

Personal information collected on this form is obtained under the authority of subsections 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, this information is used to maintain a public record. This information will be also used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to the Senior Manager, Mining Lands Section, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury ON P3E 685. Telephone 1 888 415-9845.

Instructions: - For work performed on Crown Lands before recording a claim, use form Assessment Work Performed Before Recording Claim(s)

- Please type or print in ink. - Submit to Geoscience Assessment Office, 933 Ramsey Lake Road,

Sudbury ON P3E 685. Telephone 1 888 415-9845.

Note: All correspondence will be sent to the address on record in the Provincial Recording Office, as required under the Mining Act, subsections 19(6) and (8).

1. Submitter I am [8] an authorized agent or D the recorded holder (if a company, enter name of person submitting) Name (last) I (first) (initial) I Client number (optional)

Fingler Janice L Address -Unit number, Street number, Street name 1409-675 West Hastings Street City, Town or Village I Province or State Country I Postal Code Vancouver BC Canada V6B 1N2 Telephone number I Fax number E-mail address (optional)

( 604 ) 605 8814 ( )

2. Provide

D where there is a surface rights holder, before starting ground exploration work for the first time on a staked claim you must provide notice to the surface rights holder(s) as required by the Mining Act and provide proof of notification to the Ministry

12] your technical report and maps in paper or on a compact disc [8] a current legible map showing how the contiguous mining lands are linked for assigning work D proof of beneficial interest (if assigning amongst different recorded holders)

3. Work Performed This includes the date you traveled to the field or mobilized equipment to the date the technical report was completed.

From: DD/MMMMIYYYY (enter the month in full in this box e.g. 12/July/2008) To: DD/MMMMIYYYY (enter the month in full in this box e.g. 28/July/2008) 21/November/2009

Regulations: Calculate the time-adjusted credit column, in the tables below, as follows:

1. Work filed within 2 years of performance is claimed at 100%. (Enter 100% of actual costs in both of the last 2 columns). 2. Work filed after 2 years and up to 5 years after performance is credited at 50%. (Enter 100% of actual costs in the 2nd last

column and 50% in the last column.) 3. Work older than 5 years is not eligible for credit.

3(A) Dates and Costs of Work Performed

From date To date Work Type Unit of Work DD/MMIYYYY DD/MMIYYYY (example: hours/day,

metres of drilling, km of grid lines)

10/02/2008 27/10/2008 2301 metres

28/09/2008 27110/2008 30

10/06/2008 18/10/2008 13 days

25/09/2008 20/11/2008 57 days

25/09/2008 20/ ll/2008 57 days

25/09/2008 29/ 10/2008 70

11103/2008 18/ 11 /2008 14 days

3(6) Associated Costs

To date Associated Costs From date DD/MMIYYYY DD/MMIYYYY (example: supplies, mobilization, demobilization)

25/09/2008 20/ l l/2008

I 1/03/2008 11103/2008

21/I 112008 20/ll/2009

21/11 /2008 20/1 I/2009 Database

12/01/2008 15/08/2009

0241 E (04/2006) ©Queen's Printer for Ontario, 2006

Cost per Unit of Work

125

800

Actual Costs ($)

24,000

16

10,500

4,550

Actual Costs ($)

4,405

1,615

20,000

Time-Adjusted Credit($)

(See notes 1 and 2 above)

287,972

Time-Adjusted Credit($)

(See notes 1 and 2 above)

3(C) Transportation Costs

From date To date Transportation Costs Actual Costs Time-Adjusted 00/MMIYYYY 00/MMIYYYY ($) Credit($)

(See notes 1 and 2 above)

30/09/2008 11/03/2008 HehwtJLCOt 228,960 228,960

25/09/2008 21/ll/2008 Truck Rentals 10,150 10,150

25/10/2008 20/11/2008 Freight (camp/core to RL, samples to lab) ·, .,

3(0) Food and Lodging Costs From date To date Food and Lodging Costs Actual Costs Time-Adjusted

00/MMIYYYY 00/MMIYYYY ($) Credit($) (See notes 1 and 2

above)

25/09/2008 21111/2008 Room and Board in Red Lake (logging, sampl 1g) 6,. 16 6,516

25/09/2008 11/02/2008 Camp Services (rental, supplies, food, ~) 59,097 ,,. 25/09/2008 11102/2008 1p Support (incl. cook, t1rst aid, camp lp) ~,875 12,:

Total of Time Adjusted Credit Columns (3A through 30) = Total Value of Assessment Work

4. Type of Work Performed - please check off the type of survey performed (optional)

Work Type Survey Type Work Type Survey Type

Airborne DAEM Geophysical OEM geophysical DAMAG 0GRAV

DAVLF DIP D other airborne [ZJ MAG

geophysical DVLF D other geophysical

Assays Dassay Physical D manual work D re-cutting claim lines D beneficiation D mechanical work D trenching D geochemical D overburden stripping D other physical

Drilling [ZJ diamond drilling Prospecting D Prospecting D drill core submission to Rehabilitation D Rehabilitation

MNDM Other - Please print D overburden drilling examples: microscopic studies, bulk sampling, downhole geophysics D boring other than core

Line cutting D line cutting Geochemical D geochemical Geological D geological

5. Commodities Explored for- please list (optional)

IRON

6. Work Performed, Assigned, Banked

6(A) If you performed work on mining lands other than a staked mining claim, fill in the table below. Lease or Patented Land or Licence of Occupation (LO) or Other Mining Lands: Work performed, assigned or banked

Lease # or Parcel GAO-Approved Hectares Amount of Work Amount of Credits Bank (Amount of #orG #or LO# Identifier Performed on this Assigned to Mining credits to be

(office use only) Land($) Claim(s) ($) assigned at a future date)

Column Totals for 6(A)

D Schedule attached (if you have more entries attach a schedule) rf· 0241 E (04/2006) © Queen's Printer for Ontario, 2006

6(8) Mining Claims: Work performed, applied, assigned, banked .Q! assigned from table 6(A) above

Mining Claim Number Number of Amount of Work Amount of Credits Amount of Credits Bank Claim Performed on this Applied to this Assigned to Other (Amount of credits Units Claim($) Claim($) Mining Claims ($) to be applied or

assigned at a future date)

KRL 3019665 16 69,444 32,000 37,444

KRL 3019666 16 147,569 32,000 115,569

KRL 3019667 16 651,041 32,000 38,400 580,641

KRL 4241201 16 0 38,400 0 0

Column Total for 6(8) 868,054 134,400 38,400 733,654

Column Totals of 6(A) + 6(8) 868,054 38,400 73_3,6?_4

Note: Work performed on mining claims = credits applied + credits banked

0 Schedule attached (if you have more entries attach a schedule)

7. Some of the credits claimed in this Assessment Work form may be reduced. Please indicate below how you want your credits reduced if they are not approved. Check (IZ!) in the boxes below. If you have not indicated how your remaining credits are to be allocated, credits will be reduced from the Bank first, followed by option number 2 if necessary. Credits are to be cutback:

~ 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated; or 0 2. Credits are to be cut back starting with the claims listed last, working backwards; or 0 3. Credits are to be cut back equally over all claims listed in this Assessment Work form; or

0 4. Credits are to be cut back as shown below:

List the claim numbers in the order you want the credits to be cut back (setting your priority list).

Priority Claim Number Priority

1. 6.

2. 7.

3. 8.

4. 9.

5. 10.

0 Schedule attached (if you have more entries attach a schedule)

8. Certification by Recorded Holder or Authorized Agent

I,

Claim Number

_o_5_/0-=5=-=/-=-20::-:1-::-0::-::-:-::----- that 1 have personal (00/MMIYYYY)

knowledge o he facts set forth in this Assessment Work form having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.

"Mining Lands Website: http://Www.ontario.ca/mininglands"

0241 E (04/2006) © Queen's Printer for Ontario, 2006

2008 EXPLORATION REPORT

on the

EL SOL IRON PROJECT

For

RAYTEC MINING CORPORATION

(now LION ENERGY CORPORATION)

APPENDIX 3 Geophysics Logistics Report

Clearview Geophysics Inc.

November 20th, 2009 J. Fingler, M.Sc., P.Geo

J. Fingler Geological

APPENDIX A – Instrument Specifications

APPENDIX B – Plan Maps

f Zf1J~~~ce>,( ;

Legend:

ZONE A

ZONE H

Histo!ie M.ag.nc:k, Anomaly Llbcls (from 'Map ~. Chart A' Ra:f'I'C web!i.i:e)

Added MagnetiC'S. Arlc~N iy Label (Prt~a•n:Sur.·•y)

< ······ '!-

' , , , , , ~L

Total Field Magnetics lll:aytee MetalsCorp.

EI Sol lron Or .. Prol""rty RIM! lake Mining DistrK:t , NWOntario

Plate 1

!';drw~• ~><'"'~"'~ ~).1~- · ., .. ~iCo<l ('..,.._ _...,. V.o~J'""'"''""""'"'

( ;/'V ~'-""''"" t.w:ri'.-.>M>r i'IM..:: .~t.ot~M s.. .... ,,,. ('"""""'" x.~.1

- In h~ O::;o~ <Iiiii ~"'"""'"''~- .,., '"'~"" - +

Survl'y by Cl...,rVN!ow G.aphys ics lm;.. jrfl.Mt1930)

1 '

f ZQ~.:I!•''~t ;

Legend:

ZONE A

ZONE H

Histo!ie M.ag.nc:k, AnomalyLlbcls (from 'Map ~. Chart A' Ra:f'I'C web!i.i:e)

Added MagnetiC'S. Arlc~N iy Label (Prt~a•n: Sur.·•y)

< ·· l;:

< ······ '!-

Total Field Magnetics lll:aytee MetalsCorp.

EI Sol lronOr .. Prol""rty RIM! lake Mining DistrK:t , NWOntario

Plate 2

!';drw~• ~><'"'~"'~ ~).1~- · ., .. ~iCo<l ('..,..__...,. V.o~J'""'"''""""'"'

( ;/'V ~'-""''"" t.w:ri'.-. >M>r i'IM..:: .~t.ot~M s.. .... ,,,. ('"""""'" x.~.1

- In h~ O::;o~ <Iiiii ~"'"""'"''~- .,., '"'~"" - +

Survl'y by Cl...,rVN!ow G.aphys ics lm;.. jrfl.M t1930)

2008 EXPLORATION REPORT

on the

EL SOL IRON PROJECT

For

RAYTEC MINING CORPORATION

(now LION ENERGY CORPORATION)

APPENDIX 4 Metallurgical and Analytical Report

SGS Mineral Services

November 20th, 2009 J. Fingler, M.Sc., P.Geo

J. Fingler Geological

2008 EXPLORATION REPORT

on the

EL SOL IRON PROJECT

for

RAYTEC MINING CORPORATION

(now LION ENERGY CORPORATION)

APPENDIX 5 DIAMOND DRILL LOGS

November 20th, 2009

J. Fingler, M.Sc., P.Geo

J. Fingler Geological

Hole: ES08-001

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644407.72

Elevation (m):

543883.28

Depth (m): 407.56Logged By:

10/3/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 1 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 355

Dip : -43.0

Start Date:

10/6/2008

Core Size : NQLogged Date: 11/1/2008

Diamond Drill Log

HOLE ID

ES08-001ES08-001ES08-001

ES08-001

ES08-001

ES08-001

From_m

0.001.9610.78

69.07

122.70

125.55

To_m

1.9610.7869.07

122.70

125.55

146.89

Code

CASOVERGWK

GWK

ARG

IFML

Description

CASING: Casing pulled, anchor remains.OVERBURDENGREYWACKE: (Paragneiss) Pale-med grey, mgr-cgr, granular textured; wkly silicified,variably biotitic. Some sections appear porphyritic. Weak gneissosity at +40. Patchy Ksparaltered seams and granitic infilitrations along gneissosity, microfractures +/- patchybleaching, epidote alteration. Minor calcite +/- qtz micro veinlets, both parallel to gn andoblique at -55. Local 2-15cm qtz veins. From 35.18m, Increased calcite-epidote microfracturenet. From 39.53m, Coarse granular interbeds increase downhole, of 1-3mm subround qtzgrains in a med grey fgr matrix; patchy epidote, bleaching and Kspar alteration. Contacts areboth sharp and gradational, at +40 and +35. From 60m, unit appears strained/sheared andsilicified, at +45.GREYWACKE: Pale to med grey, fgr granular; grades from massive siltstone to wacke with10-50cm interbeds of wkly chloritic mudstone and biotitic wacke. Scattered, deformedqtz-calcitc vnlts in mudstone sections. Local parasitic folds discernable. Unit is banded at +45to +50. Local late calcite +/- qtz fractures parallel to banding and at -50. From 103.25m, unitis more massive, fgr greywacke.

CHLORTIIC MUDSTONE with local CHERT-MT BANDS: vfgr chloritic mudstone with 1-25cmsections of 0.5-5cm chert +/- pyrite bands. Banding is straight to boudlinaged, trending +40 to+30. Up to 0.5% py as mgr to cgr cubes (to 0.5cm), within chert and chlorite bands.MAGNETITE-CHERT IRON FORMATION with INTERBEDS OF CHLORITIC MUDSTONE:Mgr-fgr magnetite-chert IF with 10-30% interbeds of chloritic mudstone and local 10-20%jasper bands. Mt-chert bands are 0.5-2cm thick, straight to boudinaged, transposed at +30,with some parasitic folds discernable. Wk local grunerite development along band margins,increasing downhole. Chloritic mudstone bands are up to 45cm thick, but mostly 2-5cm.Jasper bands are 2-10mm thick. Entire section is cut by a wk network of calcite-qtz vnlts,tension gashes +/-microbreccia at -30 to -70, cutting and offsetting bands on a cm scale.From 130.63-131.34m: Section of subcm banded mt-jasper-chert IF. From 129.00-132.35m:Unit cut by low TCA fractures at +80, NNW direction. From 138.30-143.31m: Chloriticsiltstone interbed with dm mt-chert IF sections downhole. From 144.40-145.70m:Mt-chert+/-jasper IF , microbrecciated and cut by +30 qtz-calcite microfractures. From145.70-146.89m: Brecciated mt-chert-chlorite IF with carbonate matrix infill.

Sample

16512165371655116573165901650116502

1650316504165051650616507165081650916510

From_m

105.00108.00111.00114.00117.00120.00122.70

125.55127.00129.00132.00135.00138.00141.00144.00

To_m

108.00111.00114.00117.00120.00122.70125.55

127.00129.00132.00135.00138.00141.00144.00146.89

Interval_m

3.003.003.003.003.002.702.85

1.452.003.003.003.003.003.002.89

Litho

GWKGWKGWKGWKGWKARGcARGc

IMCLIMCLIMCLIMCLIMCLIMCLIMCLIMCL

%SiO2

65.1066.3069.1068.4067.8067.1054.80

44.7044.8037.9541.2041.1047.2040.0038.30

%Fe2O3

6.335.125.455.186.059.83

19.60

33.5045.8049.5047.4050.9036.4038.9042.30

%TFe

4.433.583.813.624.236.8813.71

23.4332.0434.6333.1635.6125.4627.2129.59

%Mt

SAT

0.800.000.400.400.400.003.70

23.9043.3046.1546.1049.7032.3031.8036.10

%Hm

CALC

0.330.000.400.670.870.000.99

0.040.000.000.000.000.000.000.00

%FeMt

13.070.007.597.996.840.0019.53

73.8094.5395.4097.0798.1089.3983.5687.30

%FeHm

5.270.007.2712.9514.440.005.06

0.120.000.000.000.000.000.000.00

%Fe

Other

81.66100.0085.1479.0778.72100.0075.41

26.085.474.602.931.9010.6116.4412.70

CLAIM: KRL 3019667

Hole: ES08-001

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644407.72

Elevation (m):

543883.28

Depth (m): 407.56Logged By:

10/3/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 2 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 355

Dip : -43.0

Start Date:

10/6/2008

Core Size : NQLogged Date: 11/1/2008

Diamond Drill Log

HOLE ID

ES08-001

ES08-001

ES08-001

ES08-001

From_m

146.89

166.73

176.00

179.15

To_m

166.73

176.00

179.15

181.98

Code

IFMJ

QP

IFL

QP

Description

MAGNETITE-CHERT-JASPER IRON FORMATION: Mgr, sility bands of magnetite, chertwith wkly hematitic jasper bands. Chert and jasper bands are 0.3-2cm thick. Bands arestraight at +25 to +35, with local parasitic folds indicating shallow plunges (5?) to thewest. Some rootless isoclines indicate strong transposition. Minor subcm qtz-calcitefractures at low angles TCA, NNW trending. At 165.80m: jasper bands appear to be refoldedalong banding parallels axes, folds plung steeply to the west.

QUARTZ PORPHYRY: pale grey to white, massive, with 40%, 1-3mm quartz eyes in a finerequivalent matrix of qtz-biotite-chorite composition. Contacts are both straight and ragged,parallel to banding at +38. Moderate cleavage thoughout has also affected IF. Local pressureshadows around qtz eyes and elongate chorite wisps in matrix. Unit is cut by net of spacedcalcitic microfractures at -64 and local low angle TCA, NNW trending fractures withbleached, epidote and Kspar altered margins. From 167.00-171.00m, core is broken andblocky.CHLORITIC MUDSTONE with interbeds of MAGNETITE-CHERT IRON FORMATION:Sharp, bleached upper contact with QP, parallel to banding at +34. Local contact is obscuredby bleaching, silicification and granitization. Unit is dominated by vgr, dk grey-greenchloritic mudstone with 30%, dm thick sections of 0.5-2cm bands of mt-chert IF. Banding isstraight, at +35, to isoclinally folded on a cm scale. Cut by minor calcitic hair fracturesparallel to banding and at -75. Core is broken and blocky throughout interval. Trace py onfractures. From 178.45m: Core is bleached, silicified and cut by increased fractutres.QUARTZ PORPHYRY: As described previously, with strongly pervasive K feldspar overprintand local microbrecciation with carbonate infill from 179.70-180.34m. Upper contact isobscured by alteration, local contact is sharp but undulating at +25, parallel to banding.Internal foliation at +45.

Sample

165111651316514165151651616517165191652016521165221652316524

16525

16526

From_m

146.89150.00153.00156.00157.00159.00162.00165.00166.73169.00171.00174.00

176.00

179.15

To_m

150.00153.00156.00157.00159.00162.00165.00166.73169.00171.00174.00176.00

179.15

181.98

Interval_m

3.113.003.001.002.003.003.001.732.272.003.002.00

3.15

2.83

Litho

IMCJIMCJIMCJIMCJIMCJIMCJIMCJIMCJQPQPQPQP

ILCM

QP

%SiO2

39.0038.2042.7043.1041.5042.0542.6042.2062.0062.7064.0063.90

54.00

54.20

%Fe2O3

51.3055.6051.5052.2049.7050.6048.6550.404.962.892.713.21

20.70

7.09

%TFe

35.8938.8936.0336.5234.7735.4034.0335.263.472.021.902.25

14.48

4.96

%Mt

SAT

47.2048.4047.1040.4047.3045.3043.1047.602.000.200.000.00

1.60

0.00

%Hm

CALC

0.475.121.9310.360.363.263.480.700.490.600.000.00

3.41

0.00

%FeMt

95.1790.0494.6080.0698.4492.6091.6497.6941.717.160.000.00

8.00

0.00

%FeHm

0.929.213.7519.850.726.447.161.389.9120.640.000.00

16.46

0.00

%Fe

Other

3.910.741.650.090.830.951.200.9348.3872.21100.00100.00

75.55

100.00

Hole: ES08-001

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644407.72

Elevation (m):

543883.28

Depth (m): 407.56Logged By:

10/3/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 3 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 355

Dip : -43.0

Start Date:

10/6/2008

Core Size : NQLogged Date: 11/1/2008

Diamond Drill Log

HOLE ID

ES08-001

ES08-001

From_m

181.98

191.05

To_m

191.05

234.00

Code

IFML

GWK

Description

MAGNETITE-CHERT-CHLORITE IRON FORMATION: (locally garnetiferous) Gradationaldownhole from grey-green mudstone with mt-chert IF sections, into well banded mt-chert IFwith chlorite mudstone bands, into 1-5cm chlorite-garnet mudstone bands with minormt-chert. Banding is 0.3-2cm thick, and is mostly straight, at +35, with minor subcmparasitic folds. Garnets (1-3mm) overgrow mudstone-chert margins. From 189.00-191.05m: IFis asymmetrically folded over >dm scale and disrupted, offset by cm spaced fractures at+17. From 190.92-191.05m: Up to 10% pyrite as 1-3mm seams parallel to mt-chert banding.BIOTITE WACKE with Cherty Sections: Mottled, patchy interval of mixed sediments whichalternate between and grade into each other. Upper 2m is a silty biotitic wacke with cmlenses of pale grey chert and siliceous siltstone with chlorite wisps. Downhole, the latterbecomes more dominant and varies in grain size between fgr and mgr. Bedding and contactsare poorly developed and are mostly gradational, but parallel to foliation at +35 to +40. Unitlocally appears conglomeratic, with cherty fragments. At 228.00-228.67m: dm scale interbedsof quartz eye tuff.

Sample

16527165281652916530

1653116532

From_m

181.98185.00186.00189.00

191.05193.00

To_m

185.00186.00189.00191.05

193.00195.00

Interval_m

3.021.003.002.05

1.952.00

Litho

IMCLIMCLIMCLIMCL

BWKBWK

%SiO2

51.8045.9047.5041.35

56.5057.70

%Fe2O3

34.5042.4038.7049.60

7.596.71

%TFe

24.1329.6627.0734.70

5.314.69

%Mt

SAT23.0032.3032.9042.65

0.170.30

%Hm

CALC0.220.020.000.00

0.830.79

%FeMt

68.9678.8077.2986.63

2.324.62

%FeHm

0.630.060.000.00

10.9111.80

%Fe

Other30.4121.1422.7113.37

86.7883.58

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-001 10.38 12.00 1.62 1.62 100.00% 0.92 56.79% NQ JT OCT 5 / 08 54cm Redrilled , possible OBES08-001 12.00 15.00 3.00 2.95 98.33% 0.84 28.47% NQ JT OCT 5 / 08ES08-001 15.00 18.00 3.00 2.94 98.00% 0.85 28.91% NQ JT OCT 5 / 08ES08-001 18.00 21.00 3.00 2.96 98.67% 1.97 66.55% NQ JT OCT 5 / 08ES08-001 21.00 24.00 3.00 3.04 101.33% 1.60 52.63% NQ JT OCT 5 / 08ES08-001 24.00 27.00 3.00 2.89 96.33% 2.22 76.82% NQ JT OCT 5 / 08ES08-001 27.00 30.00 3.00 2.95 98.33% 2.55 86.44% NQ JT OCT 5 / 08ES08-001 30.00 33.00 3.00 3.00 100.00% 2.78 92.67% NQ JT OCT 5 / 08ES08-001 33.00 36.00 3.00 3.07 102.33% 2.31 75.24% NQ JT OCT 5 / 08ES08-001 36.00 39.00 3.00 2.96 98.67% 2.50 84.46% NQ JT OCT 5 / 08ES08-001 39.00 42.00 3.00 3.00 100.00% 2.71 90.33% NQ JT OCT 5 / 08ES08-001 42.00 45.00 3.00 3.00 100.00% 2.51 83.67% NQ JT OCT 5 / 08ES08-001 45.00 48.00 3.00 3.00 100.00% 2.47 82.33% NQ JT OCT 5 / 08ES08-001 48.00 51.00 3.00 3.00 100.00% 2.70 90.00% NQ JT OCT 5 / 08ES08-001 51.00 54.00 3.00 3.00 100.00% 2.89 96.33% NQ JT OCT 5 / 08ES08-001 54.00 57.00 3.00 2.98 99.33% 2.19 73.49% NQ JT OCT 5 / 08ES08-001 57.00 60.00 3.00 3.10 103.33% 2.45 79.03% NQ JT OCT 5 / 08ES08-001 60.00 63.00 3.00 2.85 95.00% 2.47 86.67% NQ JT OCT 5 / 08ES08-001 63.00 66.00 3.00 2.93 97.67% 2.18 74.40% NQ JT OCT 5 / 08ES08-001 66.00 69.00 3.00 3.00 100.00% 1.98 66.00% NQ JT OCT 5 / 08ES08-001 69.00 72.00 3.00 3.00 100.00% 2.41 80.33% NQ JT OCT 5 / 08 TestES08-001 72.00 75.00 3.00 3.00 100.00% 1.13 37.67% NQ JT OCT 5 / 08ES08-001 75.00 78.00 3.00 3.00 100.00% 1.76 58.67% NQ JT OCT 5 / 08ES08-001 78.00 81.00 3.00 3.00 100.00% 1.67 55.67% NQ JT OCT 5 / 08ES08-001 81.00 84.00 3.00 3.00 100.00% 2.22 74.00% NQ JT OCT 5 / 08 Bit change at 81.00mES08-001 84.00 87.00 3.00 3.00 100.00% 1.74 58.00% NQ JT OCT 5 / 08ES08-001 87.00 90.00 3.00 2.95 98.33% 1.96 66.44% NQ JT OCT 5 / 08ES08-001 90.00 93.00 3.00 3.05 101.67% 1.29 42.30% NQ JT OCT 5 / 08ES08-001 93.00 96.00 3.00 2.95 98.33% 2.08 70.51% NQ JT OCT 5 / 08ES08-001 96.00 99.00 3.00 2.90 96.67% 1.98 68.28% NQ JT OCT 5 / 08ES08-001 99.00 102.00 3.00 3.10 103.33% 2.12 68.39% NQ JT OCT 5 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-001 102.00 105.00 3.00 2.97 99.00% 0.98 33.00% NQ JT OCT 5 / 08 91cm broken and fractured coreES08-001 105.00 108.00 3.00 3.00 100.00% 1.98 66.00% NQ JT OCT 5 / 08ES08-001 108.00 111.00 3.00 3.00 100.00% 2.19 73.00% NQ JT OCT 5 / 08ES08-001 111.00 114.00 3.00 3.00 100.00% 2.36 78.67% NQ JT OCT 5 / 08ES08-001 114.00 117.00 3.00 3.00 100.00% 2.40 80.00% NQ JT OCT 5 / 08ES08-001 117.00 120.00 3.00 2.96 98.67% 1.62 54.73% NQ JT OCT 5 / 08ES08-001 120.00 123.00 3.00 3.00 100.00% 1.87 62.33% NQ JT OCT 5 / 08ES08-001 123.00 126.00 3.00 2.97 99.00% 0.81 27.27% NQ JT OCT 5 / 08 1.08m broken and fractured coreES08-001 126.00 129.00 3.00 2.98 99.33% 2.77 92.95% NQ JT OCT 5 / 08ES08-001 129.00 132.00 3.00 3.00 100.00% 2.49 83.00% NQ JT OCT 5 / 08ES08-001 132.00 135.00 3.00 2.94 98.00% 2.63 89.46% NQ JT OCT 5 / 08ES08-001 135.00 138.00 3.00 3.00 100.00% 2.69 89.67% NQ JT OCT 5 / 08ES08-001 138.00 141.00 3.00 3.00 100.00% 2.08 69.33% NQ JT OCT 5 / 08ES08-001 141.00 144.00 3.00 2.94 98.00% 1.88 63.95% NQ JT OCT 5 / 08ES08-001 144.00 147.00 3.00 2.95 98.33% 2.75 93.22% NQ JT OCT 5 / 08ES08-001 147.00 150.00 3.00 2.94 98.00% 2.06 70.07% NQ JT OCT 5 / 08ES08-001 150.00 153.00 3.00 3.04 101.33% 2.72 89.47% NQ JT OCT 5 / 08ES08-001 153.00 156.00 3.00 2.90 96.67% 2.14 73.79% NQ JT OCT 5 / 08ES08-001 156.00 159.00 3.00 3.05 101.67% 2.74 89.84% NQ JT OCT 6 / 08ES08-001 159.00 162.00 3.00 2.89 96.33% 2.50 86.51% NQ JT OCT 6 / 08ES08-001 162.00 165.00 3.00 3.03 101.00% 2.67 88.12% NQ JT OCT 6 / 08ES08-001 165.00 168.00 3.00 3.00 100.00% 2.19 73.00% NQ JT OCT 6 / 08ES08-001 168.00 171.00 3.00 2.75 91.67% 1.62 58.91% NQ JT OCT 6 / 08 80cm broken and fractured coreES08-001 171.00 174.00 3.00 2.88 96.00% 0.37 12.85% NQ JT OCT 6 / 08 Test, All broken and fractured coreES08-001 174.00 177.00 3.00 2.91 97.00% 0.62 21.31% NQ JT OCT 6 / 08 All broken and fractured coreES08-001 177.00 180.00 3.00 2.79 93.00% 0.38 13.62% NQ JT OCT 6 / 08 All broken and fractured coreES08-001 180.00 183.00 3.00 3.00 100.00% 2.16 72.00% NQ JT OCT 6 / 08ES08-001 183.00 186.00 3.00 3.00 100.00% 2.72 90.67% NQ JT OCT 6 / 08 Bit change at 183.90mES08-001 186.00 189.00 3.00 3.00 100.00% 2.11 70.33% NQ JT OCT 6 / 08ES08-001 189.00 192.00 3.00 2.95 98.33% 1.86 63.05% NQ JT OCT 6 / 08ES08-001 192.00 195.00 3.00 3.00 100.00% 2.74 91.33% NQ JT OCT 6 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-001 195.00 198.00 3.00 3.00 100.00% 2.48 82.67% NQ JT OCT 6 / 08ES08-001 198.00 201.00 3.00 3.00 100.00% 2.56 85.33% NQ JT OCT 6 / 08ES08-001 201.00 204.00 3.00 2.97 99.00% 2.97 100.00% NQ JT OCT 6 / 08ES08-001 204.00 207.00 3.00 3.00 100.00% 2.91 97.00% NQ JT OCT 6 / 08ES08-001 207.00 210.00 3.00 3.00 100.00% 2.95 98.33% NQ JT OCT 6 / 08ES08-001 210.00 213.00 3.00 2.95 98.33% 2.90 98.31% NQ JT OCT 6 / 08ES08-001 213.00 216.00 3.00 3.00 100.00% 2.70 90.00% NQ JT OCT 6 / 08ES08-001 216.00 219.00 3.00 3.00 100.00% 2.91 97.00% NQ JT OCT 6 / 08ES08-001 219.00 222.00 3.00 3.10 103.33% 2.74 88.39% NQ JT OCT 6 / 08ES08-001 222.00 225.00 3.00 3.85 128.33% 2.85 74.03% NQ JT OCT 6 / 08 TestES08-001 225.00 228.00 3.00 3.00 100.00% 2.59 86.33% NQ JT OCT 6 / 08ES08-001 228.00 231.00 3.00 3.05 101.67% 2.82 92.46% NQ JT OCT 6 / 08ES08-001 231.00 234.00 3.00 2.93 97.67% 2.04 69.62% NQ JT OCT 6 / 08 E.O.H.

Hole: ES08-002

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644407.72

Elevation (m):

543883.28

Depth (m): 407.56Logged By:

10/6/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

291.0

Page: 1 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 355

Dip : -58.0

Start Date:

10/9/2008

Core Size : NQLogged Date: 11/2/2008

Diamond Drill Log

HOLE ID

ES08-002ES08-002ES08-002

ES08-002

ES08-002

ES08-002

ES08-002

From_m

0.001.589.60

57.75

80.62

144.10

148.57

To_m

1.589.6057.75

80.62

144.10

148.57

156.78

Code

CASOVERGWK

QP

GWK

IFML

IFL

Description

CASING: Casing pulled, anchor remains.OVERBURDENPARAGNEISS: med grey, mgr-cg sandstone to local conglomerate primary textures, possiblysome tuffaceous component. 30-45% 1-3mm grey-wt qtz grains, plagioclase with siliceous +/-biotitic matrix. Some local coarser 0.2-0.5cm plagioclase crystals. Common metamorphicsegregations of k feldspar, epidote +/- calcite as cm scale gneissic bands at +60 to +75, alsoalong microfractures +/- bleaching. Scalttered 1-2% subcm qtz vnlts parallel to gneissicbanding. Trace local pyrite-both along fractures and marginal to vnlts. From 57.12-57.75m,QFP dyke with sharp contact at +75, parallel to gneissosity, cloudy contact zone.QUARTZ PORPHYRY: Highly mixed interval with gneissic segregations of cg wacke and cgrquartz feldspar porphyry. Overprinted by mottled lenses and fractures of calcite – epidote +/-k feldspar, parallel to gneissosity at +65. Cut by network of cloudy grey quartz vnlts/wispsalong NNW trend, (dipping steeply east) and also parallel to gn. Interval becomes moreporphyritic downhole. From 78.50 – 80.62m: Strongly foliated to mylonitic zone at +75.Silicified, carbonatized and cut by 2-20cm qtz +/- pyrite veins at +45. From 80.35 – 80.60m:Quartz vein at contact with underlying unit; shearing extends an estimated 20cm beyond thevein. Trace pyrite, sphalerite noted.GREYWACKE: wkly bedded, silty greywacke with 10-15% sections of laminated, variablychloritic mudstone +/- folded to brecciated quartz vnlts. Up to 1% sulphide as py+/-po asseams, cgr euhedral cubes and minor sp, cpy in fractures, gashes and at qtz vnlt margins.

CHLORITIC MUDSTONE with 20% interbeds of MAGNETITE-CHERT IF: Wkly magneticoverall. Fgr, chloritic mudstone as 1-10cm laminate and up to 20% chert bands (1-15cm) +/-finer magnetite bands (1mm-2cm). Banding is highly transposed, folded at +50. 1% pyrite.From 144.60-145.10m: Up to 10% cgr pyrite as 1-3mm banding parallel seams at chertmargins, with minor mt +/-grunerite.CHLORITE-GARNET MUDSTONE with 50% interbeds of MAGNETITE-CHERT IF:1cm-50cm sections of garnetiferous, chloritic mudstone with up to 50% mt-chert laminae0.5-15cm thick. Banding at +57, is more finely laminated in upper sections and displaysmoderate grunerite development. 0.5% local cgr pyrite seams.

Sample

162201623716254162711653316534

165351653616538

From_m

132.00135.00138.00141.00144.11147.00

148.57151.00153.00

To_m

135.00138.00141.00144.11147.00148.57

151.00153.00156.78

Interval_m

3.003.003.003.112.891.57

2.432.003.78

Litho

GWKGWKGWKGWKILCMILCM

ILMCILMCILCM

%SiO2

65.8066.7069.1066.7055.5059.40

48.5045.6039.90

%Fe2O3

6.166.584.995.48

19.3014.30

36.0042.1013.85

%TFe

4.314.603.493.8313.5010.00

25.1829.459.69

%Mt

SAT

0.801.100.100.100.000.10

22.2027.201.40

%Hm

CALC

0.770.520.730.580.001.71

0.820.720.80

%FeMt

13.4317.292.071.890.000.72

63.7966.8310.46

%FeHm

12.587.9214.6710.540.0011.94

2.291.715.74

%Fe

Other

73.9974.7983.2687.58100.0087.33

33.9331.4683.80

CLAIM: KRL 3019667

Hole: ES08-002

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644407.72

Elevation (m):

543883.28

Depth (m): 407.56Logged By:

10/6/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

291.0

Page: 2 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 355

Dip : -58.0

Start Date:

10/9/2008

Core Size : NQLogged Date: 11/2/2008

Diamond Drill Log

HOLE ID

ES08-002

ES08-002

ES08-002

From_m

156.78

161.55

175.25

To_m

161.55

175.25

207.00

Code

IFML

IFMJ

IFM

Description

MAGNETITE-CHERT IF with interbeds of CHLORITIC WACKE: Well banded, fgrargillaceous, chert-mt bands (2-10cm) at +65. Up to 30% interbeds of chloritic wacke withmoderate banding parallel to foliation. Unit is cut by late microfractures of qtz-calcite,which are oblique to banding. From 157.92-158.18m: Interbed of chloritic wacke in the coreof a fold with an EW trending, south dipping axial plane. From 160.35-161.55m Massive bedof wacke. Upper contact at +55, lower contact at +75.MAGNETITE-CHERT-JASPER IRON FORMATION: Well banded, fgr argillacous to silitymagnetite with chert and minor jasper bands. Bands are 0.2-2cm thick and are straight, tolocally asymmetrically folded at +60 to +50. Possible refolded folds present. Interval iscut by <2% microfractures of qtz-calcite at -40 and -70, with local subcm offsets of bandsand microbreccia development. Core is blocky due to the low angle TCA fracturing. From168.52-169.38m: interbed of chloritic wacke with mod-strong foliation at +66. From169.38m.: Bands of mt and chert become thicker (1-15cm), disrupted, and asymmetricallyfolded bands are more common than in upper sections. Appears to be higher grade interval(for iron content). From 174.00-176.00m: Magnetite sections appear finer and moreargillaceous, with fine subcm laminae.MAGNETITE-CHERT IRON FORMATION: Gradational from above, with less jasper. Alsogrades from finely laminated magnetite, to a fine to medium granular variety. Estimated equalproportions of mt-chert as 0.5-5cm bands which are asymmeticallly folded at low angles TCA(+80, -80) over 6 metre interval (to 181m). Cut by 1-3mm qtz-calcite vnlts at -40. From 182m:banding is mostly straight, at +65. From 186-189m, chert bands appear whiter. From187.40-189.00m: Section of chert>>mt-chlorite IF which is higly milled and brecciated over1.2m. Internal foliation of breccia is parallel to banding at +70 to +65. Trace local py. From189-207m: More finely laminated, granular mt-chert bands (1-3mm), at +50; some 20-30cmsections of mt-chert (white) and sporadic jasper bands. 0.5-1% fgr-mgr pyrite alongbandking, margins of qtz boudins, qtz sweats. From 202.75-203.50m: Interval ofchert-mt-chloritic IF with 2-3% granular pyrite seams and clots along banding and boudinagedqtz vnlts. Some minor grunerite. 25cm section of foliated quartz feldspar porphyry, at +60(parallel to banding).

Sample

1653916540

165411654216543165441654616548

1654916550165521655316554165551655616557165581655916560

From_m

156.78159.00

161.55165.00168.52169.38172.00175.20

177.00180.00183.00186.00189.00192.00195.00198.00201.00202.00204.00

To_m

159.00161.55

165.00168.52169.38172.00174.00177.00

180.00183.00186.00189.00192.00195.00198.00201.00202.00204.00207.00

Interval_m

2.222.55

3.453.520.862.622.001.80

3.003.003.003.003.003.003.003.001.002.003.00

Litho

ILMCILMC

IMCJIMCJARGcIMCJIMCJIMC

IMCIMCIMCIMCIMCIMCIMCIMCIMCIMCIMC

%SiO2

38.1037.70

39.7041.5036.1040.6041.0041.90

37.1043.1045.0045.3042.2041.3043.2042.9042.7047.0041.80

%Fe2O3

46.3035.00

49.2051.1013.1053.3052.3551.10

55.0048.7045.1037.1050.5054.1051.0050.7051.3043.0051.80

%TFe

32.3924.48

34.4235.759.1637.2936.6235.75

38.4834.0731.5525.9535.3337.8535.6835.4735.8930.0836.24

%Mt

SAT

41.9029.65

45.6049.202.7048.1048.6047.30

52.7046.6540.6026.4045.2050.1042.7046.6045.2038.1044.80

%Hm

CALC

0.000.00

0.100.000.742.900.460.00

0.000.000.000.831.511.166.831.024.010.184.27

%FeMt

91.5585.32

95.8798.0221.3293.3596.0394.02

97.2997.0088.1173.6192.5895.7986.6095.0791.1491.6589.46

%FeHm

0.000.00

0.200.005.635.430.870.00

0.000.000.002.232.982.1513.402.017.810.428.25

%Fe

Other

8.4514.68

3.931.9873.051.223.105.98

2.713.0011.8924.164.432.060.002.921.057.932.29

Hole: ES08-002

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644407.72

Elevation (m):

543883.28

Depth (m): 407.56Logged By:

10/6/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

291.0

Page: 3 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 355

Dip : -58.0

Start Date:

10/9/2008

Core Size : NQLogged Date: 11/2/2008

Diamond Drill Log

HOLE ID

ES08-002

ES08-002

ES08-002

ES08-002

From_m

207.00

218.00

234.00

247.00

To_m

218.00

234.00

247.00

291.00

Code

IFMJ

IFMS

IFM

GWK

Description

MAGNETITE-CHERT-JASPER IRON FORMATION: Alternating 0.3-3cm bands of fgr-mgrgranular, sility magnetite-chert with weak jasper development. Straight bands throughout at+50 to +60. Decreased jasper content downhole.

MAGNETITE-CHERT-CHLORITE IF with SEDIMENT INTERBEDS: Transitional from above.0.5-2cm mt-chert bands with 10-30% 1-3cm interbeds of chloritic mudstone and 0-40%5-20cm interbeds of grey siltstone. Magnetite bands are vfgr, argillaceous. Chert is mostlywhite. Bands are straight to asymmetrically folded, with deavage at +52 to +58. Local cmscale qtz- vnlts with pyrite, arsenopyrite. From 219-220m: Cut by brown carbonate as beddingparallel replacements of chert and along -45% microfractures.MAGNETITE-CHERT IRON FORMATION: Well banded; 0.5-2cm thick, alternating mt-chertbands at +56. Bands of mt range from fgr, silty, to vfgr, argillaceous. Local subcm bands ofchloritic mudstone+/-garnet present. Bands are straight to ragged, where dominant foliationoverprints (and transposes) folded bands. This is most notable from 244m. Interval gradesinto sediments downhole.BIOTITE/CHORITE WACKE with CHERTY MEMBERS: Mostly silty, poorly banded biotiticwacke to 252m, which then grades into a mottled unit of mixed biotitic/chloritic wacke withchert lenses +/- chlorite wisps. May be a relict conglomeratic texture (?). Moderate cleavageat +60. Cut by minor calcite hair fractures at -55. Trace local magnetite.

Sample

16561165621656316564165651656616567165691657016571165721657416575165761657716578

From_m

207.00210.00213.00216.00218.00219.00222.00225.00228.00231.00234.00237.00240.00241.00243.00247.00

To_m

210.00213.00216.00218.00219.00222.00225.00228.00231.00234.00237.00240.00241.00243.00247.00249.00

Interval_m

3.003.003.002.001.003.003.003.003.003.003.003.002.001.004.002.00

Litho

IMCJIMCJIMCJIMCJIMCLIMCLIMCLSIMCLSIMCLSIMCLIMCIMCIMCIMCIMCBWK

%SiO2

43.9041.7042.9544.3041.1044.7053.2555.0047.1045.2044.0039.6046.1049.0044.3060.80

%Fe2O3

50.7051.3051.6048.6047.4041.4023.8021.2039.8544.8046.7050.1043.5039.8045.406.46

%TFe

35.4735.8936.1034.0033.1628.9616.6514.8327.8831.3432.6735.0530.4327.8431.764.52

%Mt

SAT

43.7047.7047.9047.3044.3036.107.183.3028.9540.3042.8045.2035.6030.4040.500.10

%Hm

CALC

5.091.961.770.000.000.001.482.120.210.000.000.000.000.000.000.74

%FeMt

89.1696.1896.0298.9294.0088.2931.2116.1075.1591.6392.7291.8583.5178.6290.441.60

%FeHm

10.033.823.430.000.000.006.2210.020.520.000.000.000.000.000.0011.38

%Fe

Other

0.810.000.551.086.0011.7162.5773.8824.338.377.288.1516.4921.389.5687.02

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-002 9.35 9.60 0.25 0.25 100.00% 0.00 0.00% NQ JT OCT 8 / 08 25cm OBES08-002 9.60 12.00 2.40 2.82 117.50% 2.14 75.89% NQ JT OCT 8 / 08ES08-002 12.00 15.00 3.00 2.92 97.33% 2.26 77.40% NQ JT OCT 8 / 08ES08-002 15.00 18.00 3.00 2.95 98.33% 2.25 76.27% NQ JT OCT 8 / 08ES08-002 18.00 21.00 3.00 2.95 98.33% 1.92 65.08% NQ JT OCT 8 / 08ES08-002 21.00 24.00 3.00 2.92 97.33% 2.07 70.89% NQ JT OCT 8 / 08ES08-002 24.00 27.00 3.00 3.07 102.33% 2.06 67.10% NQ JT OCT 8 / 08ES08-002 27.00 30.00 3.00 3.00 100.00% 2.48 82.67% NQ JT OCT 8 / 08ES08-002 30.00 33.00 3.00 3.00 100.00% 2.61 87.00% NQ JT OCT 8 / 08ES08-002 33.00 36.00 3.00 2.94 98.00% 2.16 73.47% NQ JT OCT 8 / 08ES08-002 36.00 39.00 3.00 3.09 103.00% 2.42 78.32% NQ JT OCT 8 / 08ES08-002 39.00 42.00 3.00 3.00 100.00% 2.66 88.67% NQ JT OCT 8 / 08ES08-002 42.00 45.00 3.00 3.00 100.00% 2.74 91.33% NQ JT OCT 8 / 08ES08-002 45.00 48.00 3.00 3.00 100.00% 2.68 89.33% NQ JT OCT 8 / 08ES08-002 48.00 51.00 3.00 3.00 100.00% 2.50 83.33% NQ JT OCT 8 / 08ES08-002 51.00 54.00 3.00 3.00 100.00% 2.71 90.33% NQ JT OCT 8 / 08ES08-002 54.00 57.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 8 / 08ES08-002 57.00 60.00 3.00 2.93 97.67% 2.13 72.70% NQ JT OCT 8 / 08ES08-002 60.00 63.00 3.00 3.07 102.33% 2.92 95.11% NQ JT OCT 8 / 08ES08-002 63.00 66.00 3.00 2.92 97.33% 2.35 80.48% NQ JT OCT 8 / 08ES08-002 66.00 69.00 3.00 3.05 101.67% 2.80 91.80% NQ JT OCT 8 / 08 TestES08-002 69.00 72.00 3.00 2.94 98.00% 2.37 80.61% NQ JT OCT 8 / 08ES08-002 72.00 75.00 3.00 3.00 100.00% 2.76 92.00% NQ JT OCT 8 / 08ES08-002 75.00 78.00 3.00 3.00 100.00% 2.77 92.33% NQ JT OCT 8 / 08 All broken and fractured coreES08-002 78.00 81.00 3.00 3.00 100.00% 2.23 74.33% NQ JT OCT 8 / 08ES08-002 81.00 84.00 3.00 2.97 99.00% 2.36 79.46% NQ JT OCT 8 / 08ES08-002 84.00 87.00 3.00 3.00 100.00% 1.59 53.00% NQ JT OCT 8 / 08ES08-002 87.00 90.00 3.00 3.00 100.00% 2.68 89.33% NQ JT OCT 8 / 08ES08-002 90.00 93.00 3.00 3.00 100.00% 2.70 90.00% NQ JT OCT 8 / 08ES08-002 93.00 96.00 3.00 3.00 100.00% 2.53 84.33% NQ JT OCT 8 / 08ES08-002 96.00 99.00 3.00 3.00 100.00% 2.50 83.33% NQ JT OCT 8 / 08ES08-002 99.00 102.00 3.00 2.95 98.33% 2.32 78.64% NQ JT OCT 8 / 08ES08-002 102.00 105.00 3.00 3.05 101.67% 2.38 78.03% NQ JT OCT 8 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-002 105.00 108.00 3.00 2.82 94.00% 1.99 70.57% NQ JT OCT 8 / 08 18cm Crushed core (faulted ?)ES08-002 108.00 111.00 3.00 3.00 100.00% 1.83 61.00% NQ JT OCT 8 / 08 18cm Crushed coreES08-002 111.00 114.00 3.00 2.95 98.33% 0.87 29.49% NQ JT OCT 8 / 08 1.35m Crushed and very fractured coreES08-002 114.00 117.00 3.00 3.00 100.00% 1.09 36.33% NQ JT OCT 8 / 08 Very fractured coreES08-002 117.00 120.00 3.00 3.05 101.67% 1.65 54.10% NQ JT OCT 8 / 08ES08-002 120.00 123.00 3.00 2.95 98.33% 2.28 77.29% NQ JT OCT 8 / 08ES08-002 123.00 126.00 3.00 3.00 100.00% 2.35 78.33% NQ JT OCT 8 / 08ES08-002 126.00 129.00 3.00 3.00 100.00% 2.41 80.33% NQ JT OCT 8 / 08ES08-002 129.00 132.00 3.00 2.77 92.33% 1.83 66.06% NQ JT OCT 8 / 08 32cm crushed core (evidence of gouge / fault)ES08-002 132.00 135.00 3.00 3.00 100.00% 2.63 87.67% NQ JT OCT 8 / 08ES08-002 135.00 138.00 3.00 3.04 101.33% 2.87 94.41% NQ JT OCT 8 / 08ES08-002 138.00 141.00 3.00 2.96 98.67% 2.55 86.15% NQ JT OCT 8 / 08ES08-002 141.00 144.00 3.00 3.00 100.00% 2.06 68.67% NQ JT OCT 8 / 08ES08-002 144.00 147.00 3.00 2.95 98.33% 2.08 70.51% NQ JT OCT 8 / 08ES08-002 147.00 150.00 3.00 3.00 100.00% 2.03 67.67% NQ JT OCT 8 / 08ES08-002 150.00 153.00 3.00 3.07 102.33% 2.65 86.32% NQ JT OCT 8 / 08ES08-002 153.00 156.00 3.00 2.96 98.67% 2.23 75.34% NQ JT OCT 8 / 08ES08-002 156.00 159.00 3.00 3.05 101.67% 2.18 71.48% NQ JT OCT 8 / 08ES08-002 159.00 162.00 3.00 2.80 93.33% 1.55 55.36% NQ JT OCT 8 / 08ES08-002 162.00 165.00 3.00 3.05 101.67% 1.34 43.93% NQ JT OCT 8 / 08ES08-002 165.00 168.00 3.00 2.60 86.67% 0.97 37.31% NQ JT OCT 8 / 08ES08-002 168.00 171.00 3.00 3.00 100.00% 2.12 70.67% NQ JT OCT 8 / 08ES08-002 171.00 174.00 3.00 2.96 98.67% 2.19 73.99% NQ JT OCT 8 / 08ES08-002 174.00 177.00 3.00 3.00 100.00% 1.81 60.33% NQ JT OCT 8 / 08ES08-002 177.00 180.00 3.00 3.05 101.67% 2.78 91.15% NQ JT OCT 8 / 08ES08-002 180.00 183.00 3.00 2.95 98.33% 2.80 94.92% NQ JT OCT 8 / 08ES08-002 183.00 186.00 3.00 2.95 98.33% 1.99 67.46% NQ JT OCT 8 / 08ES08-002 186.00 189.00 3.00 3.00 100.00% 2.14 71.33% NQ JT OCT 8 / 08ES08-002 189.00 192.00 3.00 2.95 98.33% 1.62 54.92% NQ JT OCT 8 / 08ES08-002 192.00 195.00 3.00 2.87 95.67% 2.00 69.69% NQ JT OCT 8 / 08ES08-002 195.00 198.00 3.00 3.00 100.00% 2.72 90.67% NQ JT OCT 8 / 08ES08-002 198.00 201.00 3.00 3.00 100.00% 2.45 81.67% NQ JT OCT 8 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-002 201.00 204.00 3.00 3.00 100.00% 1.81 60.33% NQ JT OCT 8 / 08ES08-002 204.00 207.00 3.00 3.00 100.00% 1.06 35.33% NQ JT OCT 8 / 08ES08-002 207.00 210.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 8 / 08ES08-002 210.00 213.00 3.00 2.97 99.00% 2.03 68.35% NQ JT OCT 8 / 08ES08-002 213.00 216.00 3.00 3.02 100.67% 2.49 82.45% NQ JT OCT 8 / 08ES08-002 216.00 219.00 3.00 2.96 98.67% 2.61 88.18% NQ JT OCT 8 / 08ES08-002 219.00 222.00 3.00 3.00 100.00% 2.46 82.00% NQ JT OCT 8 / 08 TestES08-002 222.00 225.00 3.00 3.00 100.00% 2.09 69.67% NQ JT OCT 8 / 08ES08-002 225.00 228.00 3.00 2.95 98.33% 2.62 88.81% NQ JT OCT 8 / 08ES08-002 228.00 231.00 3.00 3.00 100.00% 2.66 88.67% NQ JT OCT 9 / 08 ES08-002 231.00 234.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 9 / 08ES08-002 234.00 237.00 3.00 2.90 96.67% 2.20 75.86% NQ JT OCT 9 / 08ES08-002 237.00 240.00 3.00 3.06 102.00% 2.55 83.33% NQ JT OCT 9 / 08ES08-002 240.00 243.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 9 / 08ES08-002 243.00 246.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 9 / 08ES08-002 246.00 249.00 3.00 2.98 99.33% 2.58 86.58% NQ JT OCT 9 / 08ES08-002 249.00 252.00 3.00 3.02 100.67% 2.61 86.42% NQ JT OCT 9 / 08ES08-002 252.00 255.00 3.00 2.96 98.67% 2.96 100.00% NQ JT OCT 9 / 08ES08-002 255.00 258.00 3.00 3.00 100.00% 2.64 88.00% NQ JT OCT 9 / 08ES08-002 258.00 261.00 3.00 3.00 100.00% 2.73 91.00% NQ JT OCT 9 / 08ES08-002 261.00 264.00 3.00 2.95 98.33% 2.87 97.29% NQ JT OCT 9 / 08ES08-002 264.00 267.00 3.00 3.06 102.00% 2.77 90.52% NQ JT OCT 9 / 08ES08-002 267.00 270.00 3.00 2.94 98.00% 2.59 88.10% NQ JT OCT 9 / 08ES08-002 270.00 273.00 3.00 3.00 100.00% 2.90 96.67% NQ JT OCT 9 / 08ES08-002 273.00 276.00 3.00 3.00 100.00% 2.63 87.67% NQ JT OCT 9 / 08ES08-002 276.00 279.00 3.00 3.00 100.00% 2.71 90.33% NQ JT OCT 9 / 08ES08-002 279.00 282.00 3.00 2.92 97.33% 2.43 83.22% NQ JT OCT 9 / 08ES08-002 282.00 285.00 3.00 3.06 102.00% 2.92 95.42% NQ JT OCT 9 / 08ES08-002 285.00 288.00 3.00 3.00 100.00% 2.87 95.67% NQ JT OCT 9 / 08ES08-002 288.00 291.00 3.00 3.00 100.00% 2.58 86.00% NQ JT OCT 9 / 08 E.O.H. Test

Hole: ES08-003

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644484.14

Elevation (m):

543624.34

Depth (m): 410.38Logged By:

10/9/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

177.0

Page: 1 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -46.5

Start Date:

10/11/2008

Core Size : NQLogged Date: 11/5/2008

Diamond Drill Log

HOLE ID

ES08-003ES08-003ES08-003

ES08-003

ES08-003

ES08-003

ES08-003

From_m

0.001.138.02

83.60

86.35

90.00

93.00

To_m

1.138.0283.60

86.35

90.00

93.00

95.00

Code

CASOVERGWK

ARG

IFL

IFL

IFML

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:GREYWACKE: mgr, silty; wkly biotitic; wkly banded on a cm-dm scale. Grades into 20% finer0.1-1cm laminated intervals of silty mudstone. These sections are 15cm to 3m thick, are non-to wkly chloritic and locally host 2-10cm disrupted,folded qtz-calcite vnlts with chloritic,biotitic margins. Entire unit is banded at +40 to +50 and is cut by 1-2% scattered 1-3mmqtz-calcite-py and py fractures which are parallel banding and at -60 to -78. Core ismoderately blocky to 32m. From 54m, greywacke is more massive.

ARGLLITE: med-dk grey, 2-10mm laminae at +40, wkly chloritic; <2% subcm, beddingparallel qtz+/-calcite-py vnlts, lenses which are straight to deformed. 0.5% fgr py overall. Inthe lower 50cm, core is broken, blocky, with shearing and laminae at +62.CHLORITE-CHERT IRON FORMATION: Alternating 0,5-5cm bands of pale green chloriticmudstone and pale grey chert. Fine submm garnet grains and possible grunerite in mucstonebands. Interval has up to 10% sections containing disseminated magnetite. Banding is mostlystraight at +38, but also transposed into isoclinal folds. Central 1m section is of laminatedargillite, as above. Up to 3% mgr pyrite overall, in bedding parallel seams (1-2mm) and alsoas 1-2cm thick semi-massive bands at 89.28-89.55m. Entire interval is cut by 1-5mmqtz-calcite vnlts at -70.CHLORITE-CHERT-MAGNETITE IRON FORMATION: med grey-green chloritic mudstonewith finely granular magnetite, possible grunerite and 30-40% white chert bands (0,5-2cm) at+56. From 91.30m: Mudstone bands grade into massive, fgr argillaceous magnetite with 3%pyrite. Pyrite as 0.3-1cm banding parallel seams and along late micro fractures at low anglesTCA. Unit is cut by a net of 1-2% qtz-calcite+/-py fractures/vnlets (1-2mm), at +70 and -70.MAGNETITE-CHERT-CHLORITE IRON FORMATION and BRECCIA: Transitional intervalfrom above into magnetite-grey chert interval below, with increased mt-chert component. Unitis disrupted by low angle TCA chloritic fractures grading into subcm highly milled, butcompetent sections. Relict banding at +30 to +42. Fine hair fractures of qtz-calcite throughoutat parallel to banding and also at low angles TCA.

Sample

16289163081632716344164021642016579

16580

16581

16582

From_m

45.0048.0051.0054.0057.0060.0080.60

86.35

90.00

93.00

To_m

48.0051.0054.0057.0060.0063.0086.35

90.00

93.00

95.00

Interval_m

3.003.003.003.003.003.005.75

3.65

3.00

2.00

Litho

GWKGWKGWKGWKGWKGWKARG

ILC

ILCM

IMCL

%SiO2

66.8063.5061.4067.5066.5065.7059.30

47.70

46.40

41.10

%Fe2O3

5.686.477.065.335.995.806.67

22.90

36.70

42.73

%TFe

3.974.534.943.734.194.064.67

16.02

25.67

33.37

%Mt

SAT

0.100.300.100.200.500.400.10

5.50

25.00

32.47

%Hm

CALC

0.400.410.700.450.200.341.47

1.97

0.51

5.40

%FeMt

1.824.801.473.888.637.131.55

24.84

70.46

70.41

%FeHm

7.046.299.948.393.355.7822.00

8.62

1.40

11.31

%Fe

Other

91.1488.9188.5987.7388.0287.0976.45

66.54

28.14

18.27

CLAIM: KRL 3019667

Hole: ES08-003

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644484.14

Elevation (m):

543624.34

Depth (m): 410.38Logged By:

10/9/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

177.0

Page: 2 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -46.5

Start Date:

10/11/2008

Core Size : NQLogged Date: 11/5/2008

Diamond Drill Log

HOLE ID

ES08-003

ES08-003

ES08-003

ES08-003

ES08-003

From_m

95.00

106.10

113.15

118.05

129.00

To_m

106.10

113.15

118.05

129.00

131.00

Code

IFMJ

IFM

IFL

IFMJ

QP

Description

MAGNETITE-CHERT-JASPER IRON FORMATION: Finely laminated (0.2-2cm) bands offinely granular magnetite with finer 1-5mm bands of white chert and wk-moderate jasper.Chert-jasper comprises 40-50% of the unit, with a decreased proportion of jasper downhole.Bands are mostly straight, and transposed at +45 to +25, downhole. Interval is cut by submmto 2cm vnlts of qtz-calcite-+/-chlorite, pyrite, mostly at -68, -80, -55. Core is blocky along thesetrends.MAGNETITE-CHERT IRON FORMATION: Alternating 0.5-2cm thick bands of fgr magnetiteand pale grey/white chert. To 110.50m, bands are highly disrupted, folded along an axis whichis perpendicular to the drilling trend. Downhole, bands are straight, at +35. From 111.00m,jasper bands are more common. Core is blocky along a network of calcite-qtz fractures at -50to -75. From 106.10-107.00m: Interbed of pale grey-green chloritic wacke which is stronglyfoliated at +26. Both uoper and lower contacts are sharp and undulating at +25 to +30. Coreis broken and blocky.CHLORITE-CHERT-MAGNETITE IRON FORMATION: Highly broken, blocky core withchloritic fractures; unit is banded, disrupted chlorite>>chert>mt, with local asymmetricalfolds, and refolded folds. Overall 1% pyrite as 0.5-2cm disseminations and seams inchloritic bands (to 10%) and along fractures. From 115.77- 117.80m: Chorite-chert bandingtrends +45. From 117.80-118.05m: Section is finely milled, brecciated into 1-3mm fragmentsin a chloritic matrix. Local 1-5mm kspar lozenges present.MAGNETITE-CHERT +/- JASPER IRON FORMATION: Interval of 50-60% fgr magnetite with0.5-10cm bnads of 30-40% chert and jasper bands, with local 5-30cm interbeds of chloriticmudstone. Bands are highly transposed into asymmetrical folds, some disrupted by acleavage at +36. Bands are mostly transposed to +50. Core is mostly competent, but brokenalong -40 and -50 calcitic hair fractures. Pyrite as 1-3mm disseminations, bedding parallelseams, to 1% overall. At 11960m: minor +70 fractures over 15cm section.QUARTZ PORPHYRY: Pale grey-green, massive, fgr qtz eye-felspar bearing dyke. <1mmqtz grains/eyes and chlorite/biotite wisps are flattened in foliation plane of +50, similar toflanking banding. Both upper and lower contacts are obscured by fracturing/quartz veining.Interval is cut by qtz-calcite+/-pyrite at -60 to -70.

Sample

16584165851658616587

165881658916591

1659216593

1659416595165961659716598

16600

From_m

95.0096.0099.00102.00

106.10108.00111.00

113.15115.77

118.05120.00123.00125.00126.00

129.00

To_m

96.0099.00102.00106.10

108.00111.00113.15

115.77118.05

120.00123.00125.00126.00129.00

131.00

Interval_m

1.003.003.004.10

1.903.002.15

2.622.28

1.953.002.001.003.00

2.00

Litho

IMCJIMCJIMCJIMCJ

IMCIMCIMC

ILCMILCM

IMCJIMCJIMCJIMCJIMCJ

QP

%SiO2

39.8042.6043.2040.30

54.0044.3040.80

56.7054.10

38.3038.8037.8044.8043.25

65.30

%Fe2O3

49.7050.2047.1051.80

29.6046.3052.00

25.0021.90

49.9051.4556.5046.0048.15

4.26

%TFe

34.7735.1232.9536.24

20.7132.3936.38

17.4915.32

34.9135.9939.5232.1833.68

2.98

%Mt

SAT46.4048.2041.3049.20

24.7043.9048.20

8.754.25

45.5047.3549.4042.2044.40

0.30

%Hm

CALC0.000.001.400.00

0.870.000.06

1.741.97

0.000.565.050.150.00

0.74

%FeMt

95.6198.1190.7097.63

86.3296.4695.88

36.2020.07

93.0595.2090.4494.8994.51

7.28

%FeHm

0.000.002.970.00

2.930.000.12

6.978.99

0.001.108.930.330.00

17.41

%Fe

Other4.391.896.332.37

10.763.544.00

56.8370.94

6.953.710.634.775.49

75.30

Hole: ES08-003

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644484.14

Elevation (m):

543624.34

Depth (m): 410.38Logged By:

10/9/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

177.0

Page: 3 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -46.5

Start Date:

10/11/2008

Core Size : NQLogged Date: 11/5/2008

Diamond Drill Log

HOLE ID

ES08-003

ES08-003

ES08-003

ES08-003

ES08-003

From_m

131.00

137.65

142.60

144.00

147.43

To_m

137.65

142.60

144.00

147.43

149.80

Code

IFL

IFM

MD

IFML

IFL

Description

CHLORITE-CHERT-MAGNETITE IRON FORMATION: Interval is dominated by chloriticmudstone with 20-30% overall 5-20cm sections of subcm banded chert-magnetite. Mostlybanded at +50 and cut by late fractures at -45 and -70. From 131-131.15m: 5% pyrite as cmsemi-massive bands, seams. From 133.50-134.60m: 60% magnetite with chert-chloritebands, highly folded, 3-5% diss’d pyrite in bands, at +45 to +75. From 134.60-137.65m:Laminated (cm) chlorite-chert +/- fgr garnets and 1% disseminated and fracture pyrite. Brokencore interval.MAGNETITE-CHERT IRON FORMATION: Regular, 0.5-1cm thick, magnetite-white chertbands. Magnetite is vfgr, argillaceous. Minor 1-2cm bands of chloritic mudstone. Banding ismostly straight, at +45 to +40, with some sections with ragged, transposed margins,downhole. Minor asymmetrical folds. Cut by <1% scattered 1-3mm gashes, fractures ofcalcite+/-qtz+/-pyrite at -70, +75. At 138.50m: NS trending, steeply E dipping, 1cm widechloritic fault zone, gouge. From 140.50-141.50m 10-15% pyrite as 0.5-2cm semi-massivereplacements of mt bands in late calcitic fractures. Pyrite as fgr euhedral grains.MAFIC DYKE or SEDIMENT INTERBEDS(?): pale grey-brown, vgr massive series of dykesor sedment interbeds, 85 and 20cm thick. Contacts are sharp and subparallel to banding at+35, +40; attenuating some subcm bands of chert-magnetite. Contact is locally deformed andoffset by late low angle TCA fracture. Unit has a wk internal foliation parallel to banding at+40 to +50. Cut by calcite +/- qtz gashes, fractures at -60, +75. Some 0.5cm pyrite seams inlower 5cm of interval.MAGNETITE-CHERT-CHLORITE IRON FORMATION: Ragged, alternating 0.5-2cm bandsof mt-chert-chlorite, at +50. Moderate y-brown grunerite development. Minor 2-3mm garnetgrains in lower bands of chloritic mudstone. Interval is cut by minor -35, -50 1-3mmcalcite-quartz fractures.VARIABLY CHLORITIC, GARNETIFEROUS MUDSTONE with minor CHERT-MAGNETITEBANDS: Mediume to pale grey-green, laminated chloritic mudstone with 1-5mm overprintinggarnet grains. Upper section has cm scale chert-mt (and grunerite) bands in 2-20cmsections. Downhole, unit becomes less chloritic and has less chert and magnetite. Bandingand foliation is at +45. Interval is cut by rare -50, +75 caclite fractures. Lower contact isgradational into greywacke.

Sample

1620116202

1620316204

16205

16206

16207

From_m

131.00135.00

137.65140.50

142.60

144.00

147.43

To_m

135.00137.65

140.50142.60

144.00

147.43

149.80

Interval_m

4.002.65

2.852.10

1.40

3.43

2.37

Litho

ILCMILCM

IMCIMC

QPM

IMCL

ILC

%SiO2

52.2056.30

47.1041.90

41.30

45.45

55.70

%Fe2O3

30.6023.10

45.5045.30

29.30

42.60

21.30

%TFe

21.4116.16

31.8331.69

20.50

29.80

14.90

%Mt

SAT13.503.35

40.0539.50

20.10

31.10

1.10

%Hm

CALC2.393.30

0.182.06

1.34

0.84

3.36

%FeMt

45.6315.00

91.0590.19

70.96

75.52

5.34

%FeHm

7.8114.29

0.404.55

4.57

1.98

15.79

%Fe

Other46.5670.71

8.555.26

24.47

22.51

78.87

Hole: ES08-003

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644484.14

Elevation (m):

543624.34

Depth (m): 410.38Logged By:

10/9/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

177.0

Page: 4 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -46.5

Start Date:

10/11/2008

Core Size : NQLogged Date: 11/5/2008

Diamond Drill Log

HOLE ID

ES08-003

From_m

149.80

To_m

177.00

Code

GWK

Description

BIOTITIC GREYWACKE: pale grey, white; fgr, massive; biotite and wkly chloritic; moderatelyfoliated at +40 to +65, downhole. Downhole, unit grades into blocky, broken sections whichhave cherty and/or silicified patches (poss. Conglomeratic textures?) From 155-156m, localkspar infiltrations. Entire interval is broken by low angle TCA fracturing at +75, -60.

Sample

16208

From_m

149.80

To_m

150.80

Interval_m

1.00

Litho

BWK

%SiO2

60.20

%Fe2O3

5.88

%TFe

4.11

%Mt

SAT

0.10

%Hm

CALC

0.50

%FeMt

1.76

%FeHm

8.50

%Fe

Other

89.74

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-003 8.02 9.00 0.98 0.98 100.00% 0.59 60.20% NQ JT OCT 9 / 08ES08-003 9.00 12.00 3.00 2.74 91.33% 1.62 59.12% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 12.00 15.00 3.00 2.78 92.67% 1.84 66.19% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 15.00 18.00 3.00 2.95 98.33% 2.24 75.93% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 18.00 21.00 3.00 2.87 95.67% 0.75 26.13% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 21.00 24.00 3.00 2.88 96.00% 1.27 44.10% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 24.00 27.00 3.00 2.92 97.33% 2.05 70.21% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 27.00 30.00 3.00 2.93 97.67% 1.62 55.29% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 30.00 33.00 3.00 2.95 98.33% 1.92 65.08% NQ JT OCT 9 / 08 somewhat blocky and fracturedES08-003 33.00 36.00 3.00 3.00 100.00% 2.36 78.67% NQ JT OCT 9 / 08ES08-003 36.00 39.00 3.00 2.92 97.33% 2.57 88.01% NQ JT OCT 9 / 08ES08-003 39.00 42.00 3.00 3.07 102.33% 2.76 89.90% NQ JT OCT 9 / 08ES08-003 42.00 45.00 3.00 2.93 97.67% 2.17 74.06% NQ JT OCT 9 / 08ES08-003 45.00 48.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 9 / 08ES08-003 48.00 51.00 3.00 2.90 96.67% 1.90 65.52% NQ JT OCT 9 / 08ES08-003 51.00 54.00 3.00 2.90 96.67% 2.60 89.66% NQ JT OCT 9 / 08ES08-003 54.00 57.00 3.00 3.00 100.00% 2.45 81.67% NQ JT OCT 9 / 08ES08-003 57.00 60.00 3.00 3.00 100.00% 2.02 67.33% NQ JT OCT 9 / 08ES08-003 60.00 63.00 3.00 3.00 100.00% 2.15 71.67% NQ JT OCT 9 / 08ES08-003 63.00 66.00 3.00 3.00 100.00% 2.66 88.67% NQ JT OCT 14 / 08ES08-003 66.00 69.00 3.00 3.00 100.00% 2.70 90.00% NQ JT OCT 14 / 08ES08-003 69.00 72.00 3.00 3.00 100.00% 2.07 69.00% NQ JT OCT 14 / 08 TestES08-003 72.00 75.00 3.00 3.00 100.00% 2.24 74.67% NQ JT OCT 14 / 08ES08-003 75.00 78.00 3.00 2.90 96.67% 1.07 36.90% NQ JT OCT 14 / 08ES08-003 78.00 81.00 3.00 3.10 103.33% 2.05 66.13% NQ JT OCT 14 / 08ES08-003 81.00 84.00 3.00 2.95 98.33% 2.69 91.19% NQ JT OCT 14 / 08ES08-003 84.00 87.00 3.00 2.84 94.67% 1.30 45.77% NQ JT OCT 14 / 08 27cm crushed coreES08-003 87.00 90.00 3.00 2.57 85.67% 1.52 59.14% NQ JT OCT 14 / 08 27cm crushed coreES08-003 90.00 93.00 3.00 2.92 97.33% 1.53 52.40% NQ JT OCT 14 / 08 28cm crushed coreES08-003 93.00 96.00 3.00 2.97 99.00% 2.50 84.18% NQ JT OCT 14 / 08ES08-003 96.00 99.00 3.00 3.00 100.00% 1.96 65.33% NQ JT OCT 14 / 08ES08-003 99.00 102.00 3.00 2.89 96.33% 0.83 28.72% NQ JT OCT 14 / 08 highly fracturedES08-003 102.00 105.00 3.00 2.90 96.67% 0.61 21.03% NQ JT OCT 14 / 08 highly fractured

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-003 105.00 108.00 3.00 2.70 90.00% 1.02 37.78% NQ JT OCT 14 / 08 highly fracturedES08-003 108.00 111.00 3.00 2.82 94.00% 1.13 40.07% NQ JT OCT 14 / 08 highly fracturedES08-003 111.00 114.00 3.00 2.75 91.67% 0.48 17.45% NQ JT OCT 14 / 08 mostly rubbleES08-003 114.00 117.00 3.00 2.64 88.00% 0.25 9.47% NQ JT OCT 14 / 08 All RubbleES08-003 117.00 120.00 3.00 2.78 92.67% 0.96 34.53% NQ JT OCT 14 / 08 highly fracturedES08-003 120.00 123.00 3.00 2.93 97.67% 1.95 66.55% NQ JT OCT 14 / 08 TestES08-003 123.00 126.00 3.00 2.90 96.67% 2.29 78.97% NQ JT OCT 14 / 08ES08-003 126.00 129.00 3.00 2.85 95.00% 2.27 79.65% NQ JT OCT 14 / 08ES08-003 129.00 132.00 3.00 2.95 98.33% 1.38 46.78% NQ JT OCT 14 / 08ES08-003 132.00 135.00 3.00 3.00 100.00% 1.00 33.33% NQ JT OCT 14 / 08 highly fracturedES08-003 135.00 138.00 3.00 2.62 87.33% 0.70 26.72% NQ JT OCT 14 / 08 48cm crushed core, highly fracturedES08-003 138.00 141.00 3.00 2.83 94.33% 2.19 77.39% NQ JT OCT 14 / 08ES08-003 141.00 144.00 3.00 3.00 100.00% 2.65 88.33% NQ JT OCT 14 / 08ES08-003 144.00 147.00 3.00 3.00 100.00% 2.77 92.33% NQ JT OCT 14 / 08ES08-003 147.00 150.00 3.00 3.00 100.00% 2.37 79.00% NQ JT OCT 14 / 08ES08-003 150.00 153.00 3.00 2.77 92.33% 1.18 42.60% NQ JT OCT 14 / 08 3cm fault gouge, 1.23m crushed coreES08-003 153.00 156.00 3.00 2.61 87.00% 0.51 19.54% NQ JT OCT 14 / 08 all crushed coreES08-003 156.00 159.00 3.00 2.14 71.33% 0.00 0.00% NQ JT OCT 14 / 08 156.70m bit change, all crushed coreES08-003 159.00 162.00 3.00 3.05 101.67% 0.71 23.28% NQ JT OCT 14 / 08 5cm fault gouge, all crushed coreES08-003 162.00 165.00 3.00 3.00 100.00% 2.61 87.00% NQ JT OCT 14 / 08ES08-003 165.00 168.00 3.00 2.49 83.00% 1.05 42.17% NQ JT OCT 14 / 08 95cm crushed coreES08-003 168.00 171.00 3.00 3.00 100.00% 1.78 59.33% NQ JT OCT 14 / 08ES08-003 171.00 174.00 3.00 2.22 74.00% 0.86 38.74% NQ JT OCT 14 / 08 Possible misplaced block, blocky, survey testES08-003 174.00 177.00 3.00 3.17 105.67% 2.84 89.59% NQ JT OCT 14 / 08 E.O.H.

Hole: ES08-004

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644501.7

Elevation (m):

543317.76

Depth (m): 417.24Logged By:

10/11/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

171.0

Page: 1 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -45.5

Start Date:

10/13/2008

Core Size : NQLogged Date: 11/6/2008

Diamond Drill Log

HOLE ID

ES08-004ES08-004ES08-004

ES08-004

ES08-004

ES08-004

ES08-004

From_m

0.002.1310.50

60.20

63.62

67.00

75.00

To_m

2.1310.5060.20

63.62

67.00

75.00

84.00

Code

CASOVERGWK

IFL

IFM

IFMJ

IFM

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:GREYWACKE: Pale to med grey, fgr, massive with faint bedding/banding at +45 to +50. Localinterbeds of biotite wacke and 10-50cm sections of lamininated, silty mudstone intervals +/-0.5-1cm boudinaged qtz vnlts with biotite/chlorite margins. Interval is cut by <2% 1-3mmqtz+/-calcite, pyrite fractures at -45 and +60 to +85, also NNW trending/steeply W dipping.Pyrite fracture coatings common. From 22.60-24.40m: Low angle TCA net of qtz-calcitemicrofractures cutting biotite wacke interbed.CHLORITIC MUDSTONE with CHERT BANDS: Laminated, grey-green chloritic mudstonewith 25-30% 1-3mm chert bands, increasing downhole. Interval is non-magnetic. 5% qtz vns,boudins are parallel to banding at +50. 3% pyrite overall as seams, bands and along marginsof qtz vns (up to 1cm thick).MAGNETITE-CHERT IRON FORMATION with Grunerite: Grades from above with increasedmagnetite and chert component. Well banded mt-chert (0.3-1cm) at +45. Minor cm scalechlorite mudstone/sediment interbeds. Moderite grunerite development throughout. Intervalis mostly competent, broken along -45 and -60 to -70 fractures. From 64.30-65.50m, bandsare crenulated and disrupted by +67 and +40 fractures.MAGNETITE-JASPER IRON FORMATION: Well babded magnetite> jasper iron formation,with 60% mt and 40% chert to jasper bands 2mm-2cm thick. Magnetite sections are up to10cm thick, granular textured. Banding is mostly at +50. Interval is cut by local microfracturesof calcite-qtz +/- chlorite at +80, -65. Cm to dm scale offset of bands observed.MAGNETITE-CHERT IRON FORMATION: Well banded 50:50 magnetite-chert ironformation with bands 0.5-2cm thick. Magnetite is finer grained than above interval, chert ispale grey. Local 1-3cm interbeds of chloritic mudstone. Minor wk grunerite development.Banding is mostly straight at +45, with local sections of asymmetrical folds and boudins. Upto 3% pyrite in mudstone sections. Interval is cut by -45 and low angle TCA fractures ofcalcite +/- qtz. From 78.00-78.85m: Asymmetrical fold of mt-chert with somemicrobrecciation along +40, with up to 3% pyrite as late replacments. From 78.85-79.20m:Mt.chert (med grey-blue) with wk hematite; bands are folded, boudinaged and attenuated.From 81.00-84.00m Mt>cher (med grey-blue), wk grunerite.

Sample

16209

16210

1621116212

162131621416215

162161621716219

From_m

57.00

60.20

63.6266.00

67.0069.0072.00

75.0078.0081.00

To_m

60.20

63.62

66.0067.00

69.0072.0075.00

78.0081.0084.00

Interval_m

3.20

3.42

2.381.00

2.003.003.00

3.003.003.00

Litho

GWK

ILC

IMCIMC

IMJIMJIMJ

IMCIMCIMCR

%SiO2

67.60

55.90

43.3039.30

41.3039.2039.90

39.8041.3540.70

%Fe2O3

4.93

11.80

43.1045.00

51.8053.5053.10

52.1048.9549.60

%TFe

3.45

8.25

30.1531.48

36.2437.4337.15

36.4534.2434.70

%Mt

SAT

0.20

0.70

39.9035.40

48.7050.5046.00

47.8042.6542.30

%Hm

CALC

0.31

2.02

0.000.05

0.000.674.72

0.000.680.11

%FeMt

4.20

6.14

83.0281.37

96.0297.6489.61

93.7390.1388.21

%FeHm

6.37

17.09

0.000.12

0.001.268.89

0.001.390.22

%Fe

Other

89.43

76.77

16.9818.51

3.981.101.50

6.278.4811.57

CLAIM: KRL 3019667

Hole: ES08-004

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644501.7

Elevation (m):

543317.76

Depth (m): 417.24Logged By:

10/11/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

171.0

Page: 2 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -45.5

Start Date:

10/13/2008

Core Size : NQLogged Date: 11/6/2008

Diamond Drill Log

HOLE ID

ES08-004

ES08-004

ES08-004

From_m

84.00

108.47

114.62

To_m

108.47

114.62

138.00

Code

IFMJ

IFMS

IFML

Description

MAGNETITE>>CHERT-JASPER IRON FORMATION (High Grade): Interval grades downholefrom well banded mt-white chert-jasper (0.2-1cm), into mostly fgr granular magnetite in dmsections with 0.2-1cm pale grey chert +/- hematite. Chert bands are folded, boudinaged andhighly attenuated. Banding and main foliation is at +50, fold axes are at +65 to +70. Cut byminor qtz-ca-chlorite fractures at -45 to -55 and +75. From 94.06-94.18m: banding parallel,foliated fgr biotitic dyke. From 100.15-104.75m: +30 banded section of fgr magnetite>chert+/-wk hematite. Cut by 30% intervals of granitic dykes and pale grey silica with biotite-chloritewisps foliated parallel to banding. Dykes are 3-60cm sections, with both straight andundulating contacts subparalllel to banding. From 104.75-108.47m: Section of finer grainedmagnetite (2-20cm) >> jasper (0.5-1cm) > chert (<1cm) bands. Stronger hematite/jasperbands. Mostly straight banded at +45, with local folds. Cut by minor -45 qtz-calcite fractures,also NNW, steeply W dipping fracture set.CHLORITIC MUDSTONE/SILTSTONE with interbeds of CHERT-MAGNETITE IRONFORMATION: Pale grey-green mudstone to pale grey siltstone as mm to 5cm beds at +40,with 30-40% (increased DH) of 5-20cm section of cm banded fgr argillaceous mt and whitechert. Banding is mostly straight, with rare asymmetrical folds over <5cm. 1% pyrite asbanding parallel fractures, Fractures also at -50. From 112.18-113.30m: Massive greysiltstone with 5% cm scale chl-chert-py bands. From 113.32-114.62m: Fgr, grey-brown,biotite dyke with calcite grains. Upper contact is undulating at +65, lower is banding parallel at+45. Moderate internal foliation at +45.MAGNETITE-CHERT-CHLORITE IRON FORMATION: Transitional from above, withincreased mt-chert content and increased band thickness to 1-2cm. 10-20% 1-3cm bands ofchloritic mudstone and grey siltstone +/-pyrite. Banding is at +55 to +35, downhole, withsome refolded folds over 10-40cm, with a vertical axial plane. Local grunerite. From119.40-120.10m: Pale grey granitic dyke with banding parallel contacts and internal foliationat +50. Core is broken along -45 to -70 fractures, also along NNW trending, W dippingfractures. Local spaced cleavage overprints banding at +50 to +60, imparting a raggedappearance to the bands.

Sample

16221575116222162231622416225162261622716228

1622916230

162311623216234162355752162361623816239

From_m

84.0087.0090.0093.0096.0098.0099.00102.00104.75

108.47112.18

114.62117.00120.10123.00126.00129.00132.00135.00

To_m

87.0090.0093.0096.0098.0099.00102.00104.75108.47

112.18114.62

117.00120.10123.00126.00129.00132.00135.00138.00

Interval_m

3.003.003.003.002.001.003.002.753.72

3.712.44

2.383.102.903.003.003.003.003.00

Litho

IMCJIMCJIMCJIMCJIMCJIMCJIMCJIMCJIMCJ

ILCMILCM

IMCLIMCLIMCLIMCLIMCLIMCLIMCLIMCL

%SiO2

41.5042.2042.3043.7041.7039.5541.3047.1043.60

53.0055.30

54.3045.8047.2045.5045.3043.4046.2043.20

%Fe2O3

51.2050.9052.7049.1054.5055.8553.4039.8051.20

30.9011.70

35.2040.2042.2047.9045.7050.0047.4049.30

%TFe

35.8235.6136.8734.3538.1339.0737.3627.8435.82

21.628.18

24.6228.1229.5233.5131.9734.9833.1634.49

%Mt

SAT

51.7049.5048.3047.6047.6043.3050.9036.8048.25

16.901.40

25.5534.2532.2033.7039.1045.0041.4038.40

%Hm

CALC

0.000.001.500.005.2610.840.750.000.97

1.381.42

0.850.040.330.590.000.000.000.00

%FeMt

100.098.2394.8099.2690.3480.2098.6095.2797.48

56.5712.38

75.0888.1378.9372.7787.3892.8990.0880.56

%FeHm

0.000.002.850.009.6619.401.400.001.90

4.4612.16

2.410.090.781.240.000.000.000.00

%Fe

Other

0.001.772.350.740.000.410.004.730.63

38.9775.46

22.5111.7820.3025.9912.627.119.9219.44

Hole: ES08-004

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644501.7

Elevation (m):

543317.76

Depth (m): 417.24Logged By:

10/11/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

171.0

Page: 3 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -45.5

Start Date:

10/13/2008

Core Size : NQLogged Date: 11/6/2008

Diamond Drill Log

HOLE ID

ES08-004

ES08-004

From_m

138.00

141.47

To_m

141.47

171.00

Code

IFMS

GWK

Description

CHLORITE (GARNET)-CHERT-MAGNETITE IRON FORMATION with SEDIMENTINTERBEDS: Mixed, transitional interval with increased bands of chloritic mudstone withgarnets and greywacke bands in 2-40cm sections. Mt-chert bands are 0.5-2cm, at +35. Somerefolded folds and overprinting cleavage at +20 and +60, impart a ragged appearance (as ininterval above). Moderate grunerite. Garnets are 2mm-1cm in size and display pressureshadows. ).5% pyrite is disseminated in chlorite-chert sections. Upper contact is gradational,lower contact is sharp, at +40.GREYWACKE (Paragneiss): fgr-mgr granular, pale grey unit with common 1-20cm patchygranitic infiltrations of Kfeldspar+/- epidote +/- calcite as gneissic banding at +50. Unit isalso overprinted by a cloudy bleaching, silicification front. All components are cut by -55 and-70 frin calcite +/- epidote fractures and some +70 and banding parallel qtz-calcite vnlts(0.2-0.5cm).. Local minor pyrite.

Sample

16240

16286

From_m

138.00

141.47

To_m

141.47

144.00

Interval_m

3.47

2.53

Litho

ILCM

GWK

%SiO2

49.95

62.90

%Fe2O3

36.35

4.60

%TFe

25.43

3.22

%Mt

SAT21.25

0.10

%Hm

CALC2.41

0.34

%FeMt

60.47

2.25

%FeHm

6.62

7.43

%Fe

Other32.91

90.32

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksESO8-004 10.68 12.00 1.32 1.32 100.00% 0.33 25.00% NQ JT OCT 15 / 08 Broken and blockyESO8-004 12.00 15.00 3.00 2.90 96.67% 2.08 71.72% NQ JT OCT 15 / 08ESO8-004 15.00 18.00 3.00 2.88 96.00% 2.55 88.54% NQ JT OCT 15 / 08ESO8-004 18.00 21.00 3.00 2.86 95.33% 1.18 41.26% NQ JT OCT 15 / 08 blockyESO8-004 21.00 24.00 3.00 2.95 98.33% 1.74 58.98% NQ JT OCT 15 / 08ESO8-004 24.00 27.00 3.00 3.00 100.00% 1.38 46.00% NQ JT OCT 15 / 08ESO8-004 27.00 30.00 3.00 3.00 100.00% 2.79 93.00% NQ JT OCT 15 / 08ESO8-004 30.00 33.00 3.00 2.94 98.00% 2.55 86.73% NQ JT OCT 15 / 08ESO8-004 33.00 36.00 3.00 3.00 100.00% 1.97 65.67% NQ JT OCT 15 / 08ESO8-004 36.00 39.00 3.00 2.93 97.67% 2.35 80.20% NQ JT OCT 15 / 08ESO8-004 39.00 42.00 3.00 2.90 96.67% 2.41 83.10% NQ JT OCT 15 / 08ESO8-004 42.00 45.00 3.00 3.00 100.00% 2.70 90.00% NQ JT OCT 15 / 08ESO8-004 45.00 48.00 3.00 2.94 98.00% 2.57 87.41% NQ JT OCT 15 / 08ESO8-004 48.00 51.00 3.00 3.00 100.00% 2.33 77.67% NQ JT OCT 15 / 08ESO8-004 51.00 54.00 3.00 2.90 96.67% 1.66 57.24% NQ JT OCT 15 / 08ESO8-004 54.00 57.00 3.00 3.00 100.00% 2.02 67.33% NQ JT OCT 15 / 08ESO8-004 57.00 60.00 3.00 3.05 101.67% 2.66 87.21% NQ JT OCT 15 / 08 blockyESO8-004 60.00 63.00 3.00 2.75 91.67% 1.67 60.73% NQ JT OCT 15 / 08 blockyESO8-004 63.00 66.00 3.00 2.90 96.67% 1.58 54.48% NQ JT OCT 15 / 08ESO8-004 66.00 69.00 3.00 3.00 100.00% 2.32 77.33% NQ JT OCT 15 / 08ESO8-004 69.00 72.00 3.00 2.91 97.00% 2.44 83.85% NQ JT OCT 15 / 08 TestESO8-004 72.00 75.00 3.00 2.94 98.00% 1.76 59.86% NQ JT OCT 15 / 08ESO8-004 75.00 78.00 3.00 3.00 100.00% 2.27 75.67% NQ JT OCT 15 / 08ESO8-004 78.00 81.00 3.00 3.00 100.00% 2.24 74.67% NQ JT OCT 15 / 08ESO8-004 81.00 84.00 3.00 2.88 96.00% 2.56 88.89% NQ JT OCT 15 / 08ESO8-004 84.00 87.00 3.00 2.86 95.33% 1.36 47.55% NQ JT OCT 15 / 08ESO8-004 87.00 90.00 3.00 3.00 100.00% 2.19 73.00% NQ JT OCT 15 / 08ESO8-004 90.00 93.00 3.00 2.93 97.67% 2.15 73.38% NQ JT OCT 15 / 08ESO8-004 93.00 96.00 3.00 3.00 100.00% 1.47 49.00% NQ JT OCT 15 / 08ESO8-004 96.00 99.00 3.00 2.70 90.00% 2.46 91.11% NQ JT OCT 15 / 08ESO8-004 99.00 102.00 3.00 3.20 106.67% 2.28 71.25% NQ JT OCT 15 / 08ESO8-004 102.00 105.00 3.00 2.94 98.00% 2.52 85.71% NQ JT OCT 15 / 08ESO8-004 105.00 108.00 3.00 2.93 97.67% 1.97 67.24% NQ JT OCT 15 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksESO8-004 108.00 111.00 3.00 3.00 100.00% 1.39 46.33% NQ JT OCT 15 / 08ESO8-004 111.00 114.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 15 / 08ESO8-004 114.00 117.00 3.00 2.90 96.67% 2.27 78.28% NQ JT OCT 15 / 08ESO8-004 117.00 120.00 3.00 2.84 94.67% 1.83 64.44% NQ JT OCT 15 / 08ESO8-004 120.00 123.00 3.00 3.00 100.00% 2.08 69.33% NQ JT OCT 15 / 08 TestESO8-004 123.00 126.00 3.00 3.00 100.00% 2.79 93.00% NQ JT OCT 15 / 08ESO8-004 126.00 129.00 3.00 3.00 100.00% 2.68 89.33% NQ JT OCT 15 / 08ESO8-004 129.00 132.00 3.00 3.00 100.00% 2.06 68.67% NQ JT OCT 15 / 08ESO8-004 132.00 135.00 3.00 3.00 100.00% 2.29 76.33% NQ JT OCT 15 / 08ESO8-004 135.00 138.00 3.00 2.95 98.33% 2.33 78.98% NQ JT OCT 15 / 08ESO8-004 138.00 141.00 3.00 3.00 100.00% 2.61 87.00% NQ JT OCT 15 / 08ESO8-004 141.00 144.00 3.00 2.95 98.33% 2.35 79.66% NQ JT OCT 15 / 08ESO8-004 144.00 147.00 3.00 2.96 98.67% 2.09 70.61% NQ JT OCT 15 / 08ESO8-004 147.00 150.00 3.00 2.90 96.67% 2.21 76.21% NQ JT OCT 15 / 08ESO8-004 150.00 153.00 3.00 2.90 96.67% 1.95 67.24% NQ JT OCT 15 / 08ESO8-004 153.00 156.00 3.00 3.00 100.00% 1.68 56.00% NQ JT OCT 15 / 08ESO8-004 156.00 159.00 3.00 3.00 100.00% 2.57 85.67% NQ JT OCT 15 / 08ESO8-004 159.00 162.00 3.00 2.92 97.33% 2.40 82.19% NQ JT OCT 15 / 08ESO8-004 162.00 165.00 3.00 3.00 100.00% 2.77 92.33% NQ JT OCT 15 / 08ESO8-004 165.00 168.00 3.00 3.00 100.00% 2.62 87.33% NQ JT OCT 15 / 08ESO8-004 168.00 171.00 3.00 3.05 101.67% 2.95 96.72% NQ JT OCT 15 / 08 E.O.H.

Hole: ES08-005

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644501.7

Elevation (m):

543317.76

Depth (m): 417.24Logged By:

10/13/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

222.0

Page: 1 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -65.5

Start Date:

10/15/2008

Core Size : NQLogged Date: 11/8/2008

Diamond Drill Log

HOLE ID

ES08-005ES08-005ES08-005

ES08-005

ES08-005

From_m

0.001.678.25

90.00

95.38

To_m

1.678.2590.00

95.38

115.40

Code

CASOVERGWK

ARG

IFMJ

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:GREYWACKE: pale to med grey, massive, fgr-mgr granular. Local sections of med greylaminated argillite +/- subcm boudinaged qtz vns. Faint bedding and foliation mostly at +60 to+70, with some sections at +40. Cut by sections of dk brown-grey bioitite-qtz dykes from 5cmto >1m widths. Dykes have sharp contacts both parallel and oblique to bedding. They arehighly strained and host deformed qtz-ca wisps, gashes and vnlts and are also sites of latebrittle faulting: At 10.55m: dyke/fault at +80 and +65. From 21.90-24.85m: fault/dyke rollingat +80 and -75. Bedding at +70. From 26.50-27.45m: dyke/fault at -70, cuts bedding whichtrends +40. From 42.55-42.83m: dyke at +60 subparallel to bedding, wk foliation. Overall,interval is cut by minor -50 fractures but is competent. Trace pyrite is along bedding planesand late fractures.ARGILLITE: Gradation from above into pale to med grey, fgr silty to argillaceous laminae(2-10mm). Wk to mod chloritic, increasing from 93m. Laminae are straight, with commonisoclinal, asymmetrical folds with axes at +65. Up to 1% 1-2mm fractures-both beddingparallel and at -45, seams with qtz-ca-py infill. Minor cm scale boudinaged qtz-chl-py vnlts.From 94.00-94.53m: Section of 1-3 cm banded chloritic siltstone with fgr garnets and palewt chert bands and minor subcm seams of magnetite. With moderate grunerite overprint.MAGNETITE-JASPER-CHERT IRON FORMATION: Gradational from above with decreasedsediment and increased mt-chert components. Consists of 50-60% fgr granular magnetite as1-15cm bands with sections of 0.5-5cm banded pale grey-wt chert and jasper, with localchloritic interbeds. Jasper contents ranges up to 30%, concentrated in sections 30cm to 3mthick. Banding is straight, at +55 to +60; with local isoclinal asymmetrical folds. From 99.00– 101.25m: banding is as rolling open folds along the core axis at +80 to -70, and is cut byqtz-ca-py fractures at -50. +62. Core is competent and only broken along scattered -30 to -40fractures and NNW trending, steeply east dipping fractures/qtz vnlts. From 96.12-97.10m:Banding is dragged to -70 and -85, milled into breccia and graphite-chlorite fault zone at+65 and +80. From 111.38- 111.66m: Mgr, massive granitic dyke cuts parallel to banding at+50. Sharp contacts. Also cut by NNW, E dipping fracture.

Sample

164371645416478164965804

1624116242

1624316244162451624616247162481624916251

From_m

75.0078.0081.0084.0087.00

90.0093.00

95.3899.00100.00102.00105.00108.00111.00114.00

To_m

78.0081.0084.0087.0090.00

93.0095.38

99.00100.00102.00105.00108.00111.00114.00115.40

Interval_m

3.003.003.003.003.00

3.002.38

3.621.002.003.003.003.003.001.40

Litho

GWKGWKGWKGWKGWK

ARGISLC

IMJCIMJCIMJCIMJCIMJCIMJCIMJCIMJC

%SiO2

67.3067.2065.8066.1066.60

60.8056.40

40.8046.0041.6040.9042.0045.3040.5043.00

%Fe2O3

5.325.195.195.795.63

5.8913.20

46.8045.6050.4048.8052.6048.2050.7051.80

%TFe

3.723.633.634.053.94

4.129.23

32.7431.9035.2634.1436.8033.7235.4736.24

%Mt

SAT

0.300.500.400.450.60

0.501.60

38.9043.1046.9046.8059.9046.4038.3539.60

%Hm

CALC

0.170.230.280.290.07

0.991.50

0.000.000.000.000.000.2011.0310.64

%FeMt

5.839.977.978.0411.02

8.7812.54

85.6096.9295.7398.49100.099.5878.2479.08

%FeHm

3.164.515.415.021.27

16.8011.33

0.000.000.000.000.000.4221.7620.53

%Fe

Other

91.0085.5386.6286.9487.71

74.4276.13

14.403.084.271.510.000.000.000.39

CLAIM: KRL 3019667

Hole: ES08-005

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644501.7

Elevation (m):

543317.76

Depth (m): 417.24Logged By:

10/13/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

222.0

Page: 2 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -65.5

Start Date:

10/15/2008

Core Size : NQLogged Date: 11/8/2008

Diamond Drill Log

HOLE ID

ES08-005

ES08-005

ES08-005

ES08-005

ES08-005

ES08-005

From_m

115.40

128.07

133.65

138.27

144.94

151.33

To_m

128.07

133.65

138.27

144.94

151.33

162.00

Code

IFM

QP

IFM

QP

IFMJ

IFMS

Description

MAGNETITE-CHERT IRON FORMATION: Gradational from above, with decreased jaspercontent to 0-10%. Up to 55% mgr to fgr argillaceous, dk grey magnetite as massive tolaminated bands. Chert bands are wt to pale grey, 0.2-2cm thick. Jasper bands aremoderately to strongly hematitic, 0.2-1cm thick. Downhole, overall amount of mt increases,as well as the thickness of the mt bands. Contains some minor chloritic siltstone +/- mtbands and wk local grunerite. From 115.40-123.00m: Banding is mostly straight, at +60 to+70 and locally disrupted by -30 fractures. From 123.00-128.07m: Banding as isoclinal,asymmetrical folds which are boudinaged and disrupted at +55. Some grunerite. At 126.25m:1cm cgr aspy clot with marginal pyrite at chert-mt band.QUARTZ PORPHYRY: Pale grey-white, massive, fgr-mgr with 1-3mm quartz eyes. Sharpupper and lower contacts parallel to banding at +58 and +70, respectively. Moderate internalfoliation at +55. Cut by -70, -20 fractures and minor +60, +65 subcm quartz veinlets.MAGNETITE-CHERT IRON FORMATION: Continuation of IF interval above, with 50-55%fgr magnetite (1-10cm bands), with pale grey-white chert (0.2-2cm bands) and minor wkjasper, downhole. Bands are folded, boudinaged at +45. Trace fgr pyrite throughout. Upper40cm of interval hosts 5% fgr-mgr granular pyrite as 0.2-2cm beddling parallel seams. Cut byminor -15 fractures. Good competent core.QUARTZ PORPHYRY: As above interval, with sharp upper and lower contacts parallel tobanding at +60 and +65. Pyrite concentrated at both contacts, over 1-3cm in the IF. Wk-modinternal foliation at +40. Cut by -25 and -40 fractures. From 139.40-139.76m: section of highlysheared (+30) bioititic dyke with straight to undulating contacts. Focus of late strain.MAGNETITE>>GREY CHERT IRON FORMATION +/- JASPER: Gradational from IF above,with increased fgr granular IF to 70% magnetite in 1-40cm sections and med grey chert +/-jasper in 0.5-5cm sections. Banding is straight, at +55, with common asymmetrical folding asin previous IF sections. Common minor white calcite grains interstitial to mt grains and alongedges of bands. Imparts a speckled appearance. Competenet core cut by rare -30 calciticfractures.SEDIMENT WITH MAGNETITE-CHERT IRON FORMATION: Gradational from above, withless magnetite-chert and more grey siltstone/chloritic mudstone component, to 60%. To>163m, unit is dominated by 5-20cm sections of grey laminated siltstone, cm sections ofchloritic mudstone, with lesser 10-30cm sections of 0.5-3cm banded grey chert and fgrargillaceous magnetite. Banded at +50 to +65. From 153-156m, +65 to +75 trends appearoverprinted or transposed by +55 trends. Competent core, cut by minor +30, +80 calcitic hairfractures and along seams parallel to banding.

Sample

162521625316255575316256

1625716258

1625916260

1626116262

162631626416266

1626716268

From_m

115.40117.00120.00123.00126.00

128.07132.00

133.65136.00

138.27142.00

144.94147.00150.00

151.33153.00

To_m

117.00120.00123.00126.00128.07

132.00133.65

136.00138.27

142.00144.94

147.00150.00151.33

153.00156.00

Interval_m

1.603.003.003.002.07

3.931.65

2.352.27

3.732.94

2.063.001.33

1.673.00

Litho

IMCIMCIMCIMCIMC

QPQP

IMCIMC

QPQP

IMCIMCIMC

ISMCISMC

%SiO2

44.5041.2040.1043.8037.60

65.9065.80

45.1046.40

63.2065.00

42.9042.1040.60

53.1055.50

%Fe2O3

48.2050.9052.0045.0056.90

3.172.92

49.0048.30

4.162.85

51.1053.4753.50

33.2026.90

%TFe

33.7235.6136.3831.4839.80

2.222.04

34.2833.79

2.911.99

35.7537.4337.43

23.2218.82

%Mt

SAT46.5046.4048.3038.8555.40

0.250.10

46.1046.70

0.800.10

49.2043.8751.00

25.5012.70

%Hm

CALC0.000.000.800.000.00

0.500.44

0.000.00

0.460.31

0.007.880.71

0.001.12

%FeMt

97.3492.8096.0888.9798.68

8.163.54

96.4498.24

19.893.63

99.2884.8298.61

78.3348.84

%FeHm

0.000.001.540.000.00

15.6915.06

0.000.00

11.1511.03

0.0014.731.32

0.004.16

%Fe

Other2.667.202.3811.031.32

76.1581.40

3.561.76

68.9685.35

0.720.450.07

21.6747.01

Hole: ES08-005

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644501.7

Elevation (m):

543317.76

Depth (m): 417.24Logged By:

10/13/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

222.0

Page: 3 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -65.5

Start Date:

10/15/2008

Core Size : NQLogged Date: 11/8/2008

Diamond Drill Log

HOLE ID

ES08-005

ES08-005

ES08-005

ES08-005

ES08-005

From_m

162.00

168.50

175.10

180.20

192.30

To_m

168.50

175.10

180.20

192.30

197.90

Code

IFML

QP

IFML

QP

IFML

Description

MAGNETITE-CHERT-CHLORITIC MUDSTONE IRON FORMATION: Gradatiional fromabove with less sediment and more mt-chert-chl mudstone components. Fgr silty toargillaceous dk grey magnetite and grey chert as 0.5 to 10cm bands; 30% to 5% chloriticmudstone as 1 -3 cm bands. Banding is straight (+60 to +40 downhole) with someasymmetrical dm folds with axial planar cleavage parallel to banding at +40. Minor finecalcitic fractures at +70. Trace py in mudstone bands.QUARTZ PORPHYRY: As for previous. Upper contact is sharp but irregular, cuts bands.Lower contact is sharp and parallel to banding at +60. Wk-mod internal cleavage at +60 to+65. Minor -40 calcitic fractures and low TCA fractures +/- pyrite.MAGNETITE-CHERT+/- CHLORITE IRON FORMATION: Gradational from above IFsection, with decreased chloritic mudstone component. Magnetite > pale grey chert bands at+65 are 0.5-2cm thick. Local dm scale asymmetrical folds. Cut by minor calcitic fractures at+75.QUARTZ PORPHYRY: As described previously, upper 80cm is finer grained. Upper contactis sharp, parallel to banding at +40. Lower contact is +50. Internal section ofmt-chert-chlorite IF from 181.0-181.90m, also banded at +50. from 181.90-183.00m, dyke iscut by difuse granitic infilitrations at +80 and chl-calcite micro fractures at +80 and -70. Cutby minor calcite hair fractures at -25 to -45, and NNW trending, W dipping fractures.MAGNETITE-CHERT-CHLORITE-GARNET IRON FORMATION: Gradational from above IF,with 0.5-2cm fgr argillaceous mt and med grey chert bands with 2-20cm bands of chloriticmudstone with 2-5mm garnetis. Bands are straight to folded at +60, with progressively moreragged margins along secondary cleavage at +70. Moderate to strong grunerite at bandmargins and fgr amphibole development downhole. From 195.00-195.35m: Massive darkgrey-brown biotite dyke with banding parallel contacts. Unit is cut by minor calcite fracturesat -25, +40 and NNW trending fractures. Gradational lower contact.

Sample

1626916270

1627216273

1627416275

1627616277

16278162791628016281

1628216284

From_m

156.00159.00

162.00165.00

168.50172.00

175.10177.00

180.20183.00186.00189.00

192.30194.88

To_m

159.00162.00

165.00168.50

172.00175.10

177.00180.20

183.00186.00189.00192.30

194.88197.90

Interval_m

3.003.00

3.003.50

3.503.10

1.903.20

2.803.003.003.30

2.583.02

Litho

ISMCISMC

IMCLIMCL

QPQP

IMCLIMCL

QPMQPQPQP

IMCLIMCL

%SiO2

57.5057.30

51.0045.50

64.7064.90

41.5044.30

54.8064.0565.5065.40

45.4549.60

%Fe2O3

25.2022.00

34.1047.70

3.613.14

51.5047.20

21.103.062.803.03

47.5029.90

%TFe

17.6315.39

23.8533.37

2.532.20

36.0333.02

14.762.141.962.12

33.2320.92

%Mt

SAT10.707.30

21.3046.60

0.700.15

49.9043.10

17.100.100.000.30

38.4016.40

%Hm

CALC1.321.67

0.720.00

0.360.48

0.000.00

0.000.390.000.03

0.161.45

%FeMt

43.9234.32

64.6197.92

20.064.94

98.3693.64

83.733.380.0010.24

83.6256.74

%FeHm

5.247.57

2.120.00

9.9815.31

0.000.00

0.0012.770.001.12

0.344.83

%Fe

Other50.8458.11

33.272.08

69.9679.75

1.646.36

16.2783.85100.0088.63

16.0438.43

Hole: ES08-005

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644501.7

Elevation (m):

543317.76

Depth (m): 417.24Logged By:

10/13/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

222.0

Page: 4 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -65.5

Start Date:

10/15/2008

Core Size : NQLogged Date: 11/8/2008

Diamond Drill Log

HOLE ID

ES08-005

ES08-005

From_m

197.90

201.00

To_m

201.00

222.00

Code

GWK

GWK

Description

BIOTITIC WACKE: Gradational from above, with decreased chlorite-garnet and IF bands.Stongly foliated quartz-biotite schist at +65. Alternating mm scale white quartzose and dkgrey biotitic laminae. Gradationlal lower contact.PARAGNEISS: Finer grained quartz biotite groundmass overprinted by common masses ofmed grey silica+/-chloritie, amphibole. Sporadic overprinting by k feldspar-calcite+/-epidotebands, fractures at +55 gneisosity. Downhole, discrete chlorite-amphibole vnlets 0.5-2cm.

Sample

16285

From_m

197.90

To_m

201.00

Interval_m

3.10

Litho

BWK

%SiO2

58.70

%Fe2O3

6.87

%TFe

4.81

%Mt

SAT

0.10

%Hm

CALC

0.82

%FeMt

1.51

%FeHm

11.98

%Fe

Other

86.52

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-005 8.05 9.00 0.95 0.95 100.00% 0.25 26.32% NQ JT OCT 16 / 08 27cm OBES08-005 9.00 12.00 3.00 2.88 96.00% 1.26 43.75% NQ JT OCT 16 / 08ES08-005 12.00 15.00 3.00 2.92 97.33% 1.93 66.10% NQ JT OCT 16 / 08ES08-005 15.00 18.00 3.00 3.00 100.00% 1.82 60.67% NQ JT OCT 16 / 08ES08-005 18.00 21.00 3.00 3.00 100.00% 1.46 48.67% NQ JT OCT 16 / 08 TestES08-005 21.00 24.00 3.00 3.00 100.00% 1.30 43.33% NQ JT OCT 16 / 08ES08-005 24.00 27.00 3.00 2.93 97.67% 2.06 70.31% NQ JT OCT 16 / 08ES08-005 27.00 30.00 3.00 3.00 100.00% 2.08 69.33% NQ JT OCT 16 / 08ES08-005 30.00 33.00 3.00 2.90 96.67% 2.13 73.45% NQ JT OCT 16 / 08ES08-005 33.00 36.00 3.00 2.90 96.67% 2.52 86.90% NQ JT OCT 16 / 08ES08-005 36.00 39.00 3.00 3.00 100.00% 2.00 66.67% NQ JT OCT 16 / 08ES08-005 39.00 42.00 3.00 3.00 100.00% 2.44 81.33% NQ JT OCT 16 / 08ES08-005 42.00 45.00 3.00 3.00 100.00% 2.33 77.67% NQ JT OCT 16 / 08ES08-005 45.00 48.00 3.00 3.05 101.67% 2.29 75.08% NQ JT OCT 16 / 08ES08-005 48.00 51.00 3.00 2.92 97.33% 2.62 89.73% NQ JT OCT 16 / 08ES08-005 51.00 54.00 3.00 3.00 100.00% 2.51 83.67% NQ JT OCT 16 / 08ES08-005 54.00 57.00 3.00 2.96 98.67% 2.27 76.69% NQ JT OCT 16 / 08ES08-005 57.00 60.00 3.00 3.00 100.00% 2.38 79.33% NQ JT OCT 16 / 08ES08-005 60.00 63.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 16 / 08ES08-005 63.00 66.00 3.00 2.97 99.00% 2.79 93.94% NQ JT OCT 16 / 08ES08-005 66.00 69.00 3.00 3.00 100.00% 2.27 75.67% NQ JT OCT 16 / 08ES08-005 69.00 72.00 3.00 2.95 98.33% 2.46 83.39% NQ JT OCT 16 / 08ES08-005 72.00 75.00 3.00 3.00 100.00% 2.44 81.33% NQ JT OCT 16 / 08ES08-005 75.00 78.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 16 / 08ES08-005 78.00 81.00 3.00 3.00 100.00% 2.20 73.33% NQ JT OCT 16 / 08ES08-005 81.00 84.00 3.00 3.00 100.00% 2.73 91.00% NQ JT OCT 16 / 08 Missing blockES08-005 84.00 87.00 3.00 3.05 101.67% 2.49 81.64% NQ JT OCT 16 / 08ES08-005 87.00 90.00 3.00 2.90 96.67% 2.51 86.55% NQ JT OCT 16 / 08ES08-005 90.00 93.00 3.00 2.95 98.33% 2.06 69.83% NQ JT OCT 16 / 08ES08-005 93.00 96.00 3.00 2.95 98.33% 1.58 53.56% NQ JT OCT 16 / 08ES08-005 96.00 99.00 3.00 3.00 100.00% 2.35 78.33% NQ JT OCT 16 / 08ES08-005 99.00 102.00 3.00 2.95 98.33% 2.81 95.25% NQ JT OCT 16 / 08ES08-005 102.00 105.00 3.00 3.10 103.33% 2.43 78.39% NQ JT OCT 16 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-005 105.00 108.00 3.00 2.80 93.33% 2.50 89.29% NQ JT OCT 16 / 08ES08-005 108.00 111.00 3.00 3.00 100.00% 2.53 84.33% NQ JT OCT 16 / 08ES08-005 111.00 114.00 3.00 3.00 100.00% 2.38 79.33% NQ JT OCT 16 / 08ES08-005 114.00 117.00 3.00 3.00 100.00% 2.52 84.00% NQ JT OCT 16 / 08ES08-005 117.00 120.00 3.00 3.00 100.00% 2.32 77.33% NQ JT OCT 16 / 08ES08-005 120.00 123.00 3.00 3.00 100.00% 2.70 90.00% NQ JT OCT 16 / 08ES08-005 123.00 126.00 3.00 2.97 99.00% 2.62 88.22% NQ JT OCT 16 / 08ES08-005 126.00 129.00 3.00 3.00 100.00% 2.80 93.33% NQ JT OCT 16 / 08ES08-005 129.00 132.00 3.00 3.00 100.00% 2.25 75.00% NQ JT OCT 16 / 08ES08-005 132.00 135.00 3.00 3.00 100.00% 2.80 93.33% NQ JT OCT 16 / 08ES08-005 135.00 138.00 3.00 2.96 98.67% 2.83 95.61% NQ JT OCT 16 / 08ES08-005 138.00 141.00 3.00 3.00 100.00% 2.57 85.67% NQ JT OCT 16 / 08ES08-005 141.00 144.00 3.00 3.00 100.00% 2.79 93.00% NQ JT OCT 16 / 08ES08-005 144.00 147.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 17 / 08ES08-005 147.00 150.00 3.00 2.92 97.33% 2.47 84.59% NQ JT OCT 17 / 08ES08-005 150.00 153.00 3.00 3.03 101.00% 2.94 97.03% NQ JT OCT 17 / 08ES08-005 153.00 156.00 3.00 2.96 98.67% 2.79 94.26% NQ JT OCT 17 / 08ES08-005 156.00 159.00 3.00 2.90 96.67% 2.73 94.14% NQ JT OCT 17 / 08ES08-005 159.00 162.00 3.00 2.95 98.33% 2.63 89.15% NQ JT OCT 17 / 08ES08-005 162.00 165.00 3.00 3.05 101.67% 2.98 97.70% NQ JT OCT 17 / 08ES08-005 165.00 168.00 3.00 3.00 100.00% 2.29 76.33% NQ JT OCT 17 / 08ES08-005 168.00 171.00 3.00 2.95 98.33% 2.63 89.15% NQ JT OCT 17 / 08ES08-005 171.00 174.00 3.00 3.00 100.00% 2.76 92.00% NQ JT OCT 17 / 08 TestES08-005 174.00 177.00 3.00 3.00 100.00% 1.76 58.67% NQ JT OCT 17 / 08ES08-005 177.00 180.00 3.00 2.97 99.00% 2.48 83.50% NQ JT OCT 17 / 08ES08-005 180.00 183.00 3.00 2.96 98.67% 1.92 64.86% NQ JT OCT 17 / 08ES08-005 183.00 186.00 3.00 3.00 100.00% 2.38 79.33% NQ JT OCT 17 / 08ES08-005 186.00 189.00 3.00 3.00 100.00% 2.31 77.00% NQ JT OCT 17 / 08ES08-005 189.00 192.00 3.00 3.00 100.00% 2.89 96.33% NQ JT OCT 17 / 08ES08-005 192.00 195.00 3.00 3.00 100.00% 2.20 73.33% NQ JT OCT 17 / 08ES08-005 195.00 198.00 3.00 3.00 100.00% 2.22 74.00% NQ JT OCT 17 / 08ES08-005 198.00 201.00 3.00 3.00 100.00% 2.75 91.67% NQ JT OCT 17 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-005 201.00 204.00 3.00 2.94 98.00% 2.71 92.18% NQ JT OCT 17 / 08ES08-005 204.00 207.00 3.00 3.00 100.00% 2.80 93.33% NQ JT OCT 17 / 08ES08-005 207.00 210.00 3.00 2.92 97.33% 2.78 95.21% NQ JT OCT 17 / 08ES08-005 210.00 213.00 3.00 3.04 101.33% 2.75 90.46% NQ JT OCT 17 / 08ES08-005 213.00 216.00 3.00 3.00 100.00% 2.74 91.33% NQ JT OCT 17 / 08ES08-005 216.00 219.00 3.00 2.94 98.00% 2.87 97.62% NQ JT OCT 17 / 08ES08-005 219.00 222.00 3.00 3.05 101.67% 2.18 71.48% NQ JT OCT 17 / 08 E.O.H.

Hole: ES08-006

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644430.66

Elevation (m):

543008.72

Depth (m): 412.06Logged By:

10/15/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 1 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -45.0

Start Date:

10/17/2008

Core Size : NQLogged Date: 11/9/2008

Diamond Drill Log

HOLE ID

ES08-006ES08-006ES08-006

ES08-006

ES08-006

ES08-006

ES08-006ES08-006

ES08-006

ES08-006

From_m

0.001.417.83

85.65

89.85

98.90

100.15102.92

104.45

113.46

To_m

1.417.8385.65

89.85

98.90

100.15

102.92104.45

113.46

124.00

Code

CASOVERGWK

QP

GWK

QP

GWKQP

ARG

IFMR

Description

CASING: Casing pulled, anchor remains.OVERBURDEN;GREYWACKE: Pale grey, fgr, cm laminted to dm bedded. Wkly chloritic wacke with med-dkgrey siltstone. Both banded at +45 to +50. Local scours, flame structures and cross beddingsuggest stratigraphic tops are uphole (but may be rapidly reverse due to common folding andhigh strain in the area). At 15.25m and 16.60m: greywacke scours of laminated argillite. At24.60m: possible crossbedding and greywacke fining up hole. From 23.43m: core is blocky,broken along bedding planes, -40 fractures with pyrite, calcite and along NNW trending, Wdipping fractures. Fractures are water stained to 20m. From 24.00-85.65m: More massivegreywacke at +45 to +50 with minor -40 fractures. At 79-82m: Fractures are at low angles TCA.QUARTZ PORPHYRY: As described in previous drill holes. Mgr with 2-5mm qtz grains, chloritewisps along foliation planes at +50. Contacts are sharp, with some stoping.GREYWACKE: As described previously, massive to wkly laminted at +40 to +50, cut by rarecalcite fracture at -45 . Trace pyrite.QUARTZ PORPHYRY: As described previously, mgr-cgr, foliated at +50. Cut by minor calcite+/- pyrite fractures at -50. Upper contact is sharp, undulating at +40, lower contact at +55.GREYWACKE: As for previous interval; bedded at +45. Cut by -45 calcite-qtz-py microfractures.QUARTZ PORPHRY: As described previously. Lower contact and internal foliation is beddingparallel at +55.GREY ARGILLITE: Pale grey-green; greywacke to siltstone grades downhole into finelylaminated argillite; variably chlorite. Bedding at +45. Locus of increased strain, with minorsubcm banding parallel qtz boudins. 1% pyrite overall as foliation parallel seams, to 1cm in finechert-chlorite bands. Minor dm sections of chloritic mudstone and 2-10cm chert +/- pyrte bands.Core is blocky and fractured in lower 2 metres, along -65 to -80 choritic fractures.MAGNETITE-CHERT IRON FORMATION (High Grade) : 50-60% fgr granular to argillaceousdk grey magnetite as 5cm to mm scale laminae in 2-20cm sections +/- chloritic partings. Pale tomed grey chert as 2mm=2cm bands. Bands are straight, at +55 to +45, downhole, with raggedgruneritic margins at +70. Some asymmetrical folding. Downhole, unit becomes more finelylaminated magnetite, with 1-3 cm chert bands. Cut by calcite-qtz-py fractures at -40 to -50 and+70, -70 tension gashes, vnlts of qtz-ca.

Sample

16287

16288162901629116292

From_m

111.00

113.46117.00120.00123.00

To_m

113.46

117.00120.00123.00124.00

Interval_m

2.46

3.543.003.001.00

Litho

ARG

IMCIMCIMCIMCS

%SiO2

52.70

38.8041.0539.2037.80

%Fe2O3

9.79

45.8050.7551.3049.60

%TFe

6.85

32.0435.5035.8934.70

%Mt

SAT

0.10

34.4037.7540.3041.90

%Hm

CALC

1.18

0.000.000.000.00

%FeMt

1.06

77.0776.7181.0187.35

%FeHm

12.01

0.000.000.000.00

% FeOther

86.93

22.9323.2918.9912.65

CLAIM: KRL 3019667

Hole: ES08-006

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644430.66

Elevation (m):

543008.72

Depth (m): 412.06Logged By:

10/15/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 2 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -45.0

Start Date:

10/17/2008

Core Size : NQLogged Date: 11/9/2008

Diamond Drill Log

HOLE ID

ES08-006

ES08-006

ES08-006

ES08-006

ES08-006

ES08-006

ES08-006

From_m

124.00

129.40

135.00

141.70

143.72

145.37

147.26

To_m

129.40

135.00

141.70

143.72

145.37

147.26

167.00

Code

IFMJ

IFML

IFMJ

QP

IFM

QP

IFMJ

Description

MAGNETITE-JASPER IRON FORMATION: Alternating 1-5cm bands of fgr silty to argillaceousmagnetite and strong jasper bands +/- minor grey chert bands. Well banded at +40. Core iscompetent but more broken from 127m, along late calcite fractures at low angle TCA.MAGNETITE-JASPER IRON FORMATION: Alternating 0.5-2cm bands of fgr silty, dk greymagnetite and 0.5-2cm white-pale grey chert. Some chloritic partings to mt bands. Interval iswell banded at +40.MAGNETITE-CHERT-JASPER IRON FORMATION: Alternating bands of 0.5-10cm grey, siltymagnetite and 0.2-2cm white chert to moderate jasper. Mostly well banded at +30 to +25, withminor boudins and attenuated bands note, as well as minor folds. Interval is cut by qtz-ca-pyfractures at -40. From 137.09-137.33m: Highly strained biotite dyke parallel to banding at+30. From 137.65-138.10m: Wk-mod foliated quartz porphyry dyke with cgr pyrite at contacts.From 138.35-138.42m: Small banding parallel QP dyke From 138.42m: Jasper content is greaterthan chert, common cm to dm folds, with banding at +30 to 0, downhole. Second order mm scalefolds along larger scale folds have axial planes of 0 to -15.QUARTZ PORPHYRY: As described previously, Sharp banding parallel contacts at 0 and wkinternal foliation at +40.MAGNETITE-CHERT IRON FORMATION: Gradational from above IF, with decrease jasper andincreased strain resulting in broken, stretches and boudinaged 1-5mm bands of pale grey chertwith 0.1-1cm, med grey granular magnetite bands with chloritic partings. Overall bandingtrends from +20 to +5, downhole. From 144.25-144.45m: QP dyke parallel to banding at +20. Upto 5% pyrite in mt bands within 40cm of dyke contacts.QUARTZ PORPHYRY: As described previously. Sharp contacts at +20 to +25. Internal foliationat +20.MAGNETITE>>JASPER-CHERT IRON FORMATION (High Grade) : Section of up to 60-70%mgr granular magnetite and specularite as 2-50cm bands, with 15-40% wk-moderate jasper topale grey chert as 0.2-20cm bands. Thicker bands of both compenents are in the middle sectionof unit, with up to 50cm of semimassive magnetite. Upper 2 metres have folded, boudinagedbands. Downhole, thicker bands are more regular, straight, at +35 to +50, with rare 1m sectionsat +60 (possible limbs of larger scale asymmetrical folds). Good, compenent core is cut byminor calcite fractures at +40 to +50. Pyrite is concentrated to 3% over 10cm at contact with QPabove.

Sample

162935754

1629416295

1629616297

16299

16300

16301

1630216303163041630516306

From_m

124.00126.00

129.40132.00

135.00138.10

141.70

143.72

145.37

147.26150.00153.00156.00159.00

To_m

126.00129.40

132.00135.00

138.10141.70

143.72

145.37

147.26

150.00153.00156.00159.00162.00

Interval_m

2.003.40

2.603.00

3.103.60

2.02

1.65

1.89

2.743.003.003.003.00

Litho

IMJIMJ

IMCLIMCL

IMCJIMCJ

QP

IMC

QP

IMJCIMJCIMJCIMJCIMJC

%SiO2

39.6041.20

43.6041.90

44.3044.90

64.50

43.90

64.10

40.0044.0040.9049.3043.00

%Fe2O3

53.3051.20

49.8050.90

44.3049.80

2.96

45.60

3.06

54.3051.6055.0047.1053.40

%TFe

37.2935.82

34.8435.61

30.9934.84

2.07

31.90

2.14

37.9936.1038.4832.9537.36

%Mt

SAT

59.8046.05

47.7048.20

40.7042.70

0.70

39.50

0.30

53.0048.0546.9037.6045.20

%Hm

CALC

0.003.19

0.000.00

1.385.32

0.01

1.18

0.26

0.001.896.498.186.65

%FeMt

100.093.03

96.5096.05

95.0388.69

24.46

89.60

10.14

99.5596.3288.2082.5887.55

%FeHm

0.006.23

0.000.00

3.1110.68

0.35

2.59

8.63

0.003.6611.8017.3712.45

% FeOther

0.000.74

3.503.95

1.860.63

75.18

7.81

81.23

0.450.020.000.050.00

Hole: ES08-006

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644430.66

Elevation (m):

543008.72

Depth (m): 412.06Logged By:

10/15/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 3 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -45.0

Start Date:

10/17/2008

Core Size : NQLogged Date: 11/9/2008

Diamond Drill Log

HOLE ID

ES08-006

ES08-006

ES08-006

ES08-006

From_m

167.00

177.00

188.02

189.65

To_m

177.00

188.02

189.65

197.03

Code

IFMS

IFML

IFMJ

IFM

Description

CHLORITIC MUDSTONE-MAGNETITE-CHERT IRON FORMATION: 50% med to palegrey-green, variably chloritic mudstone as cm to dm bands, with 50% dm sections of 0.5-2cmbanded, fgr argillaceous magnetite and pale grey-white chert. Chloritic bands are locallymagnetic. Interval appears to have taken up increased strain, resulting in regular to transposedand isoclinally folded laminae at +35 to +50. Some remnant fold closures have axes at 0 to +25.Trace to 0.5% pyrite as fgr bedding parallel seams +/- calcite, qtz. Interval is cut by rare -60calcite+/- py fractures. From 173.80-174.32m: Massive bed of med-dk grey siltstone. From175.20-176.12m: Biotitic dyke. Upper and lower contacts parallel to banding at +35 and +40.Strong internal foliation at +35.MAGNETITE-CHERT-CHLORITE IRON FORMATION (High Grade): Well banded interval with50-60% dk grey, fgr silty to argillaceous magnetite in 1-10cm sections, and 30% pale-med greychert/jasper as 0.5-2cm bands. Chert has variably hematite content and grades into jaspersections 20cm to >1m wide. Up to 20% 1-3cm chloritic siltstone, mudstone bands +/- magnetiteand fine calcitic vnlts, grains. Banding is straight to asymmetrically folded at +40 to +55.Interval is cut by minor -30 and -60 calcite-py fractures. Jasper rich sections: 181.80-182.80m,183.60-184.00mMAGNETITE-JASPER IRON FORMATION+/-specularite: Gradation from above, with increasehematite content in chert bands. Interval is alterating 0.5-1cm bands of fgr granular dk greymagnetite-specularite and mod-strong jasper. Regular banding at +50.MAGNETITE-CHERT IRON FORMATION: Gradational from above with less hematite. Similar0.5-1cm alternating bands of vfgr dk grey magnetite and med grey chert. Bands are regular, at+50, to +65, downhole. Cut by minor calcite+/-py fractures at +65 to +70. From 190-195m:Increased strain with bands transposed, folded at +65 to +70 and locally overprinted by asecond cleavage at +80. Refolded fold structure at 193.50m. From 193-197.03m: Regularmt-chert bands with 20% chlorite-mt bands (3-7cm) at +60. From 196.40-197.03m Greywackeinterbed with sharp contacts parallel to bedding at +60 to +50.

Sample

1630716309

16310163111631216313

1631416315163161631716319

163201632116322

From_m

162.00165.00

167.00168.00171.00174.32

177.00180.00183.00186.00188.00

189.65192.00195.00

To_m

165.00167.00

168.00171.00174.32177.00

180.00183.00186.00188.00189.65

192.00195.00197.03

Interval_m

3.002.00

1.003.003.322.68

3.003.003.002.001.65

2.353.002.03

Litho

IMJCIMJC

IMCLIMCLIMCLILMC

IMCLIMCLIMCLIMCLIMJ

IMCIMCIMCS

%SiO2

40.6043.80

48.9051.3056.8052.70

48.1045.2544.6048.3043.90

41.4040.3049.40

%Fe2O3

53.6050.30

43.2033.1023.9021.00

42.0047.7547.7043.3052.30

52.5051.9034.50

%TFe

37.5035.19

30.2223.1516.7214.69

29.3833.4033.3730.2936.59

36.7336.3124.13

%Mt

SAT44.7044.10

39.8021.7012.506.00

36.3045.6046.1037.0045.30

52.4052.1039.65

%Hm

CALC7.364.68

0.000.100.852.24

0.000.000.000.005.44

0.000.000.00

%FeMt

86.2690.69

92.9567.8154.1029.55

88.9198.5197.2786.9589.59

100.0100.097.99

%FeHm

13.749.31

0.000.313.5410.66

0.000.000.000.0010.41

0.000.000.00

% FeOther

0.000.00

7.0531.8842.3659.78

11.091.492.7313.050.00

0.000.002.01

New Text

Hole: ES08-006

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644430.66

Elevation (m):

543008.72

Depth (m): 412.06Logged By:

10/15/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 4 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -45.0

Start Date:

10/17/2008

Core Size : NQLogged Date: 11/9/2008

Diamond Drill Log

HOLE ID

ES08-006

ES08-006

ES08-006

ES08-006

ES08-006

ES08-006

From_m

197.03

199.37

204.20

208.83

216.44

221.25

To_m

199.37

204.20

208.83

216.44

221.25

233.60

Code

IFL

IFL

IFMJ

ARG

GWK

GD

Description

CHLORITE-GARNET MUDSTONE with MAGNETITE-CHERT BANDS and strong gruneriteoverprint: Gradational from above with increase chloritic mudstone bands (205cm) and lessmt-chert banding (0.5-2cm). Common 1-3mm garnets in chlorite bands, with strong gruneriteoverprint, along along nt-chert margins. Banding is regular, at +50. At 197.40m, cut by minor -80calcitic fracture. From 198.85-198.98m: subparallel qtz vein with 5% semi massive, clots ofpyrrhotite>>pyrite.INTERBEDDED GREY SILTSTONE and CHLORITE-GARNET MUDSTONE +/- chert< mt:40-60% grey siltstone in 1-10cm sections with 40% 1-5cm bands of chloritic mudstone withdense mm scale garnets and subcm local chert bands. Weak local magnetite as fine bands, at+50.MAGNETITE-CHERT IRON FORMATION with JASPER: Similar to interval 189.65-197.03m,with 0.3-1cm vfgr magnetite and med grey chert bands. Up to 20% chlorite-garnet-gruneritebands (1-5cm) in upper and lower metre. Well banded at +45, with local secondary cleavage at+50 to +55, causing ragged margins to bands. Rare calcite fractures at -65. Trace pyrite asseams in chlorite bands. From 206.35-207.50m: Progressive increase in hematite content inchert bands and jasper. From 208.25m: 3-15cm interbeds of biotite wacke at +50.INTERBEDDED ARGILLITE with CHLORITIC-GARNET MUDSTONE+/-CHERT: As for interval199.37-204.20m, with thicker bands to 10cm. Mod-strong cleavage at +50. 5-10% relict 0.5-2cmchert bands +/- mt are strongly attenuated, boudinaged at +50. Trace-0.5% pyrrhotite grains inchlorite bands. Interval grades down hole into black argillite and greywacke. From211.55-213.62m: Interbed of argillite with chert bands, at +50. From 213.62m: Garnets arelarger, 0.5-1cm. IBIOTITE WACKE: Pale to dk grey sections of mgr, biotitic wacke; moderately foliated at +50.Local subcm elongate wt chert fragments with aspect ratio of 4:1. Unit is siliceous, with localchlorite+/- calcite-pyrite fracture partings.GRANODIORTIC DYKE: Massive, fgr-mgr dyke of pale grey qtz with finer interstitial grains ofgreen-black chlorite and/or amphiboles. Internal foliation at +40 to +45, parallel to flankingbanding. Foliation is weaker in central part of dyke. Lower contact is sharp, undulating at +45.Cut by minor 1-3mm qtz-ca+/-chl fractures, tension gashes at +50, -50 and -70 to -80. From227.80m: Calcite-chlorite fractures at -70/-80 with diffuse K feldspar halos.

Sample

16323

1632416325

1632616328

163291633016331

16332

From_m

197.03

199.37202.00

204.20207.00

208.83211.55213.62

216.44

To_m

199.37

202.00204.20

207.00208.83

211.55213.62216.44

219.00

Interval_m

2.34

2.632.20

2.801.83

2.722.072.82

2.56

Litho

ILMC

ISLCISLC

IMCJIMCJ

ARGARGARG

BWK

%SiO2

52.20

55.8054.90

43.6040.90

53.5058.2057.70

61.90

%Fe2O3

35.70

25.6024.00

49.7047.90

23.9017.3019.30

7.06

%TFe

24.97

17.9116.79

34.7733.51

16.7212.1013.50

4.94

%Mt

SAT11.60

3.150.30

40.9042.70

1.800.400.50

0.30

%Hm

CALC2.67

2.733.17

0.000.00

1.241.321.98

0.60

%FeMt

33.61

12.731.29

84.8390.75

7.792.392.68

4.40

%FeHm

7.47

10.6513.21

0.000.00

5.177.6510.24

8.46

% FeOther

58.92

76.6285.50

15.179.25

87.0489.9687.08

87.15

Hole: ES08-006

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644430.66

Elevation (m):

543008.72

Depth (m): 412.06Logged By:

10/15/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

234.0

Page: 5 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 358

Dip : -45.0

Start Date:

10/17/2008

Core Size : NQLogged Date: 11/9/2008

Diamond Drill Log

HOLE ID

ES08-006

From_m

233.60

To_m

234.00

Code

ARG

Description

GREY SILTSTONE to ARGILLITE: Massive, foliated at +40. Wkly magnetic.

Sample From_m To_m Interval_m Litho %

SiO2%

Fe2O3%

TFe%Mt

SAT

%Hm

CALC%

FeMt%

FeHm% FeOther

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-006 7.72 9.00 1.28 1.28 100.00% 0.35 27.34% NQ JT OCT 19 / 08 12cm OB, All blocky and fracturedES08-006 9.00 12.00 3.00 3.00 100.00% 1.13 37.67% NQ JT OCT 19 / 08 All blocky and fracturedES08-006 12.00 15.00 3.00 3.00 100.00% 1.58 52.67% NQ JT OCT 19 / 08 blocky and fracturedES08-006 15.00 18.00 3.00 2.92 97.33% 2.13 72.95% NQ JT OCT 19 / 08ES08-006 18.00 21.00 3.00 2.85 95.00% 1.50 52.63% NQ JT OCT 19 / 08 1.06m broken/ fractured/ crushed core, TestES08-006 21.00 24.00 3.00 2.94 98.00% 1.89 64.29% NQ JT OCT 19 / 08 39cm fractured/ crushed coreES08-006 24.00 27.00 3.00 3.00 100.00% 2.09 69.67% NQ JT OCT 19 / 08ES08-006 27.00 30.00 3.00 3.00 100.00% 2.38 79.33% NQ JT OCT 19 / 08ES08-006 30.00 33.00 3.00 3.00 100.00% 1.77 59.00% NQ JT OCT 19 / 08ES08-006 33.00 36.00 3.00 2.92 97.33% 2.47 84.59% NQ JT OCT 19 / 08ES08-006 36.00 39.00 3.00 3.00 100.00% 2.61 87.00% NQ JT OCT 19 / 08ES08-006 39.00 42.00 3.00 3.00 100.00% 2.49 83.00% NQ JT OCT 19 / 08ES08-006 42.00 45.00 3.00 3.06 102.00% 2.41 78.76% NQ JT OCT 19 / 08ES08-006 45.00 48.00 3.00 2.88 96.00% 2.39 82.99% NQ JT OCT 19 / 08ES08-006 48.00 51.00 3.00 3.00 100.00% 1.69 56.33% NQ JT OCT 19 / 08ES08-006 51.00 54.00 3.00 2.95 98.33% 2.17 73.56% NQ JT OCT 19 / 08ES08-006 54.00 57.00 3.00 3.00 100.00% 2.76 92.00% NQ JT OCT 19 / 08ES08-006 57.00 60.00 3.00 3.03 101.00% 2.19 72.28% NQ JT OCT 19 / 08ES08-006 60.00 63.00 3.00 2.84 94.67% 2.04 71.83% NQ JT OCT 19 / 08ES08-006 63.00 66.00 3.00 3.08 102.67% 2.75 89.29% NQ JT OCT 19 / 08ES08-006 66.00 69.00 3.00 2.95 98.33% 2.34 79.32% NQ JT OCT 19 / 08ES08-006 69.00 72.00 3.00 2.91 97.00% 2.25 77.32% NQ JT OCT 19 / 08 TestES08-006 72.00 75.00 3.00 2.95 98.33% 2.27 76.95% NQ JT OCT 19 / 08ES08-006 75.00 78.00 3.00 2.90 96.67% 2.59 89.31% NQ JT OCT 19 / 08ES08-006 78.00 81.00 3.00 3.08 102.67% 1.71 55.52% NQ JT OCT 19 / 08ES08-006 81.00 84.00 3.00 3.00 100.00% 2.45 81.67% NQ JT OCT 19 / 08ES08-006 84.00 87.00 3.00 3.00 100.00% 2.76 92.00% NQ JT OCT 19 / 08ES08-006 87.00 90.00 3.00 3.03 101.00% 2.85 94.06% NQ JT OCT 19 / 08ES08-006 90.00 93.00 3.00 2.96 98.67% 2.56 86.49% NQ JT OCT 19 / 08ES08-006 93.00 96.00 3.00 2.95 98.33% 2.81 95.25% NQ JT OCT 19 / 08ES08-006 96.00 99.00 3.00 3.07 102.33% 2.80 91.21% NQ JT OCT 19 / 08ES08-006 99.00 102.00 3.00 3.00 100.00% 2.61 87.00% NQ JT OCT 19 / 08ES08-006 102.00 105.00 3.00 2.94 98.00% 2.75 93.54% NQ JT OCT 19 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-006 105.00 108.00 3.00 3.06 102.00% 2.47 80.72% NQ JT OCT 19 / 08ES08-006 108.00 111.00 3.00 3.00 100.00% 2.51 83.67% NQ JT OCT 19 / 08ES08-006 111.00 114.00 3.00 3.00 100.00% 1.43 47.67% NQ JT OCT 19 / 08ES08-006 114.00 117.00 3.00 3.00 100.00% 2.97 99.00% NQ JT OCT 19 / 08ES08-006 117.00 120.00 3.00 3.00 100.00% 2.73 91.00% NQ JT OCT 19 / 08ES08-006 120.00 123.00 3.00 2.95 98.33% 2.46 83.39% NQ JT OCT 19 / 08 TestES08-006 123.00 126.00 3.00 2.95 98.33% 2.74 92.88% NQ JT OCT 19 / 08ES08-006 126.00 129.00 3.00 2.94 98.00% 1.76 59.86% NQ JT OCT 19 / 08ES08-006 129.00 132.00 3.00 2.87 95.67% 2.20 76.66% NQ JT OCT 19 / 08ES08-006 132.00 135.00 3.00 3.00 100.00% 2.62 87.33% NQ JT OCT 19 / 08ES08-006 135.00 138.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 19 / 08ES08-006 138.00 141.00 3.00 2.94 98.00% 2.53 86.05% NQ JT OCT 19 / 08ES08-006 141.00 144.00 3.00 3.00 100.00% 2.55 85.00% NQ JT OCT 19 / 08ES08-006 144.00 147.00 3.00 2.49 83.00% 2.54 102.01% NQ JT OCT 20 / 08ES08-006 147.00 150.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 20 / 08ES08-006 150.00 153.00 3.00 3.00 100.00% 2.69 89.67% NQ JT OCT 20 / 08ES08-006 153.00 156.00 3.00 3.00 100.00% 2.74 91.33% NQ JT OCT 20 / 08ES08-006 156.00 159.00 3.00 3.00 100.00% 2.95 98.33% NQ JT OCT 20 / 08ES08-006 159.00 162.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 20 / 08ES08-006 162.00 165.00 3.00 3.00 100.00% 2.52 84.00% NQ JT OCT 20 / 08ES08-006 165.00 168.00 3.00 3.00 100.00% 2.78 92.67% NQ JT OCT 20 / 08ES08-006 168.00 171.00 3.00 2.76 92.00% 2.73 98.91% NQ JT OCT 20 / 08ES08-006 171.00 174.00 3.00 3.03 101.00% 1.80 59.41% NQ JT OCT 20 / 08ES08-006 174.00 177.00 3.00 3.05 101.67% 2.00 65.57% NQ JT OCT 20 / 08ES08-006 177.00 180.00 3.00 3.03 101.00% 2.86 94.39% NQ JT OCT 20 / 08ES08-006 180.00 183.00 3.00 2.88 96.00% 2.74 95.14% NQ JT OCT 20 / 08ES08-006 183.00 186.00 3.00 3.08 102.67% 2.79 90.58% NQ JT OCT 20 / 08ES08-006 186.00 189.00 3.00 2.70 90.00% 2.25 83.33% NQ JT OCT 20 / 08 Block moved 75cm ( misplaced)ES08-006 189.00 192.00 3.00 3.00 100.00% 2.42 80.67% NQ JT OCT 20 / 08ES08-006 192.00 195.00 3.00 3.00 100.00% 1.83 61.00% NQ JT OCT 20 / 08ES08-006 195.00 198.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 20 / 08ES08-006 198.00 201.00 3.00 2.58 86.00% 1.51 58.53% NQ JT OCT 20 / 08 blocky and fractured

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-006 201.00 204.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 20 / 08ES08-006 204.00 207.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 20 / 08ES08-006 207.00 210.00 3.00 3.00 100.00% 2.87 95.67% NQ JT OCT 20 / 08ES08-006 210.00 213.00 3.00 2.94 98.00% 2.44 82.99% NQ JT OCT 20 / 08ES08-006 213.00 216.00 3.00 3.00 100.00% 2.54 84.67% NQ JT OCT 20 / 08ES08-006 216.00 219.00 3.00 3.00 100.00% 2.68 89.33% NQ JT OCT 20 / 08ES08-006 219.00 222.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 20 / 08ES08-006 222.00 225.00 3.00 2.95 98.33% 2.68 90.85% NQ JT OCT 20 / 08ES08-006 225.00 228.00 3.00 3.03 101.00% 2.59 85.48% NQ JT OCT 20 / 08ES08-006 228.00 231.00 3.00 2.95 98.33% 2.68 90.85% NQ JT OCT 20 / 08ES08-006 231.00 234.00 3.00 3.03 101.00% 2.99 98.68% NQ JT OCT 20 / 08 E.O.H.

Hole: ES08-007

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/18/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

168.0

Page: 1 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -46.0

Start Date:

10/19/2008

Core Size : NQLogged Date: 11/10/2008

Diamond Drill Log

HOLE ID

ES08-007ES08-007ES08-007

ES08-007

ES08-007

ES08-007

From_m

0.001.118.50

24.00

34.25

46.43

To_m

1.118.5024.00

34.25

46.43

52.55

Code

CASOVERCONG

GWK

IFMS

QP

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:CONGLOMERATE: Pale grey, massive, mgr greywacke to conglomeratic sections with 0.3-1cmthick white siliceous fragments (poorly graded sorted). Wk to moderate chloritic parttngs. Intervalis moderately foliated at +30 to +35. Clasts have 2:1 to 5:1 aspect ratios. Cut by minor lowangle TCA fractures at +80 to -80. Water stains on foliation parallel and oblique fracture surfaces.BIOTITE WACKE: Gradational from above with increase biotite content as diffuse gneissicbands at +40 to +45, alternating with pale grey siliceous patches with chorite wisps. Imparts amottled appearance. Unit is similar to that logged at the base of drillholes ES08-001 to -004. Cutby -45 to -55 fractures +/- calcite, pyrite. Minor fractures are NNW trending, steeply E dipping.Water stains on fractures to 31m. From 33.50m, increase biotite content and fining into moreargillaceous unit.CHLORITE-GARNET MUDSTONE-CHERT IRON FORMATION with SILTSTONEINTERBEDS: Transitional between siltstone and chloritic mudstone beds (0.5-10cm) with0.1-2cm cloudy wt to pale grey chert bands. Common 0.2-0.5cm subround garnets overprintingchlorite-chert sections. Interval is mod-strongly foliated and banded at +45. Chert bands arestretched, boudinaged and dismembered, locally appears ragged and overprinted by gruneritewith minor remnant mt bands. Trace to 0.5% pyrite as grains, seams in chlorite bands +/-calcite. Some larger inter beds of dk grey-brown laminated siltstone to argillite: 38.70-40.35m,41.52-42.20m. From 42.40-42.65m: late wt qtz vein cutting subparalllel to banding. From42.40m: Increased chl-gt sections and larger, folded 1-10cm chert bands. Mod grunerite. Minorlocal calcite+/- pyrite fracture. Near base of interval, some 20cm fgr gabbroic (?) dykes cutsubparallle to banding. Contacts are sharp.QUARTZ PORPHYRY: 75% fgr-mgr pale to med grey dykes, as 60-170cm sections with sharp,banding parallel contacts at +45. Wk to mod internal foliation at +45. Intervening sections(15-75cm) of garnetiferous, chloritic mudstone. Dykes have chloritic wisps parallel to foliation.Unit is cut by calcite +/- py fractures at -40 to -50 and -75. Pyrite to 5% over 10cmconcentrated in chloritic mudstone at contacts. From 51.09-52.55m: Cut by biotite dyke alongNNW trending, W dipping structure, foliated at +55, similar to flanking IF. From 50m:magnetite-chert bands are preserved between dykes.

Sample

16333

1633416335163361633716339

1634016341

From_m

32.00

34.2536.0038.7040.3542.20

46.4350.00

To_m

34.25

36.0038.7040.3542.2046.43

50.0052.55

Interval_m

2.25

1.752.701.651.854.23

3.572.55

Litho

BWK

ILCSILCSILCSILCSILCS

QPQPM

%SiO2

59.10

55.0053.7558.2053.6057.00

63.2054.30

%Fe2O3

6.61

20.2026.3513.8021.7020.40

9.6918.00

%TFe

4.62

14.1318.439.6515.1814.27

6.7812.59

%Mt

SAT

0.20

1.002.300.500.080.10

0.8010.70

%Hm

CALC

0.34

2.092.861.773.272.95

0.930.79

%FeMt

3.13

5.129.033.750.380.51

8.5461.49

%FeHm

5.12

10.3310.8612.7915.0514.47

9.564.37

% FeOther

91.75

84.5580.1183.4684.5785.02

81.9034.14

CLAIM: KRL 3019667

Hole: ES08-007

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/18/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

168.0

Page: 2 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -46.0

Start Date:

10/19/2008

Core Size : NQLogged Date: 11/10/2008

Diamond Drill Log

HOLE ID

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

From_m

52.55

64.40

70.05

72.70

74.61

81.82

92.33

To_m

64.40

70.05

72.70

74.61

81.82

92.33

93.90

Code

IFM

QP

IFM

QP

IFMJ

QP

IFM

Description

MAGNETITE-CHERT IRON FORMATION: Alternating 0.5-2cm) bands of gr magnetite and palegrey to white chert, with some dm scale interbeds of chloritic mudstone, to 55m. Bands arestraight to isoclinally folded at +40 to +45. Refolded fold at 56.40m. Interval is cut by -55 to-65 calcite +/- pyrite fractures. Minor dm scale shear zones and secondary cleavage at +60,which cuts +40 banding. Minor biotite wacke interbeds. From 60m, up to 25% cm scale jasperbands at +65.QUARTZ PORPHYRY: As described previously. Cut by low angle TCA fractures from66.50-68m. Upper contact is obscured by fracturing, lower contact is sharp and parallel tobanding at +60.MAGNETITE-CHERT IRON FORMATION: Similar to above IF interval, with 0.5-2cm bands, butlacking chloritic interbeds. Well banded at +45 and cut by minor fractures +/- calcite at -50.From 70.14-70.52m: grey brown, strongly foliated biotitic wacke (?) interbed parallel to bandingat +60 (upper contact) and +45 (lower contact).QUARTZ PORPHYRY: As described previously; wkly foliated at +65 and cut by minor fracturesat +65 and -40. Late cm qtz veinlets at +80. Sharp lower contact at -10, parallel to dragged bedsof IF along limb of 50cm open fold.MAGNETITE-CHERT-JASPER IRON FORMATION: Increased proportion of fgr, dk greymagnetite as 1-10cm beds with 35-40% 0.5-2cm thick bands of med grey chert and wk jasperbands. Upper 50cm is open fold, with +0 to -70, to -65 banding. From 76m, banding rolls to+30. Lower metre has finer cm to subcm banding of both mt-chert. Minor asymmetrical, isoclinalfolds (cm scale) of chert - jasper bands.QUARTZ PORPHYRY with intervening sections of MAGNETITE-CHERT IRON FORMATION:As described previously, with 20% internal sections of mt-chert iron formation (30-50cm). Dykeshave sharp contacts parallel to banding at +40 to +65, downhole. Banding is straight to folded.Up to 10% pyrite concentrated as seams, bands in contact zones of dykes. From83.65-83.85m: Chloritic microfracture, breccia zone at -70, +70.MAGNETITE-CHERT IRON FORMATION: Broader section of remnant iron formation betweenQP dykes, as above interval. Alternating 0.5-1cm bands of fgr granular mt and med grey-bluechert. Highly folded, dismembered and attenuated at +60. Up to 5% late pyrite +/- chloriteseams concentrated at contacts. Upper contact is sharp and oblique to banding at -40. Internalfoliation is parallel to banding at +50. Some low angle TCA fracturing and drag of bandingbetween +65 to -65, from 93.30-93.75m- may be asymmetrical fold.

Sample

1634216343163451634616347

1634816349

16350

16351

16352163531635416355

16357163581635916360

16361

From_m

52.5554.0057.0060.0062.00

64.4067.00

70.05

72.70

74.6677.0078.0080.00

81.8284.0087.0090.00

92.33

To_m

54.0057.0060.0062.0064.40

67.0070.05

72.70

74.66

77.0078.0080.0081.82

84.0087.0090.0092.33

93.90

Interval_m

1.453.003.002.002.40

2.603.05

2.65

1.96

2.341.002.001.82

2.183.003.002.33

1.57

Litho

IMCLIMCIMCIMCIMC

QPQP

IMCS

QP

IMCJIMCJIMCJIMCJ

QPMQPMQPQP

IMC

%SiO2

45.0043.7048.0042.8039.70

64.5064.50

42.20

64.90

38.3042.0041.7042.80

59.4060.8064.6063.10

46.30

%Fe2O3

39.6044.0042.2051.5055.00

3.002.99

47.90

3.25

56.1052.9053.5051.43

12.7016.002.925.35

43.90

%TFe

27.7030.7829.5236.0338.48

2.102.09

33.51

2.27

39.2437.0137.4335.98

8.8811.192.043.74

30.71

%Mt

SAT

30.2038.7038.7551.7054.20

0.100.60

45.60

0.30

55.8049.8049.2050.30

9.2512.000.201.20

36.70

%Hm

CALC

0.130.000.000.000.00

0.430.08

0.00

0.35

0.001.392.610.00

0.420.490.350.78

1.80

%FeMt

78.8989.5193.21100.099.68

3.4520.76

96.28

9.55

99.9397.3895.1298.09

75.3477.587.0823.20

86.47

%FeHm

0.330.000.000.000.00

14.362.54

0.00

10.89

0.002.624.880.00

3.313.0711.9414.54

4.11

% FeOther

20.7910.496.790.000.32

82.1976.70

3.72

79.56

0.070.000.001.91

21.3519.3580.9862.26

9.42

Hole: ES08-007

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/18/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

168.0

Page: 3 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -46.0

Start Date:

10/19/2008

Core Size : NQLogged Date: 11/10/2008

Diamond Drill Log

HOLE ID

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

From_m

93.90

102.10

105.15

107.20

112.78

118.72

To_m

102.10

105.15

107.20

112.78

118.72

119.84

Code

QP

QP

IFMJ

IFMJ

QP

IFMJ

Description

QUARTZ PORPHYRY: As described previously. Moderate internal foliation at +55 to +65.Upper contact is sharp, oblique to banding at -45, lower contact is ragged at +50. From99.62-99.77m: remnant section of mt-chert IF with 3% pyrite, pyrrhotite. Cut by minor -45 to -55fractures. From 97.00-97.60m: Cut by diffuse wt qtz-tourmaline veinlets (0.5-1cm) at -80 and+80; these are cut and offsect by later calcitic fractures at -55.BIOTITIC QUARTZ PORPHRY with sections of MAGNETIT-CHERT IRON FORMATION:Dominated by fgr QP dyke with increase biotite contact to groundmass. Mod-strongly foliated at+65. From 102.10-109.90m: Section of mt-grey chert IF with chloritic partings, banded at +50.2% py at lower contact. From 103.35-103.80m: Increased strain, to mylonitic textures. 2% pyriteseams and weathered out calcitic vugs. Appears similar to highly strained biotite dykes by moresiliceous.MAGNETITE-CHERT-JASPER IRON FORMATION with BIOTITIC DYKES: Gradational fromprevious IF section, with increased jasper component. Alternating 0.2-2cm bands of mt-greychert and 0.5cm wk jasper bands, at +55. Bands are straight to stretched, attenuated. Cut bybiotite-calcite dykes parallel to banding, from 105.75-106.10m and 106.75-107.20m. Dykes arehighly strained, mylonitic at +55, +45. Both dykes and IF are cut by -50 calcitic fractures.MAGNETITE-CHERT-JASPER IRON FORMATION: Gradational from above. 50-55% fgr siltyto argillaceous magnetite as 0.2-5cm bands, with med grey-blue chert and med jasper as0.2-1cm bands. Banding varies from straight (=50 to +35 downhole) to tightly asymmetricalfolded along +60 axes. Broken, sheared along +70. Cut by minor NNW trending, steeply Wdipping pyrite +/- calcite fractures.QUARTZ PORPHYRY: As described previously. Wkly foliated at +60 to +50. Sharp uppercontact is banding parallel at +50. Lower contact is banding parallel at +40. Cut by minor -50fractures, also a NS trending, vertical fracture which is subparalllel to core axis.MAGNETITE-JASPER-CHERT IRON FORMATION: Gradational from above IF section, withincreased jasper>chert and thicker bands to 0.5-5cm. Well banded at +35. Section is blocky,broken along fractures parallel TCA. A portion of this interval is a quartz porphyry dyke.

Sample

1636216363

16364

16365

163661636716368

1636916370

16371

From_m

93.9098.00

102.10

105.15

107.20110.00111.00

112.78116.00

118.72

To_m

98.00102.10

105.15

107.20

110.00111.00112.78

116.00118.72

121.87

Interval_m

4.104.10

3.05

2.05

2.801.001.78

3.222.72

3.15

Litho

QPQP

QPM

IMCS

IMCJIMCJIMCJ

QPQP

QPMJ

%SiO2

63.6062.80

55.00

44.30

40.3042.9047.60

64.1064.80

57.80

%Fe2O3

3.235.52

19.90

36.30

53.5050.8045.30

2.982.70

18.60

%TFe

2.263.86

13.92

25.39

37.4335.5431.69

2.081.89

13.01

%Mt

SAT

0.302.20

16.80

33.40

48.9046.2044.40

0.100.10

15.70

%Hm

CALC

0.420.47

0.07

0.00

2.692.960.00

0.660.46

0.42

%FeMt

9.6141.23

87.33

94.40

94.5494.0799.90

3.473.83

87.31

%FeHm

13.098.50

0.35

0.00

5.035.830.00

21.9917.19

2.24

% FeOther

77.3050.27

12.32

5.60

0.430.100.10

74.5478.97

10.44

Hole: ES08-007

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/18/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

168.0

Page: 4 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -46.0

Start Date:

10/19/2008

Core Size : NQLogged Date: 11/10/2008

Diamond Drill Log

HOLE ID

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

ES08-007

From_m

119.84

121.87

129.00

131.60

133.33

137.05

140.00

142.85

To_m

121.87

129.00

131.60

133.33

137.05

140.00

142.85

143.13

Code

QP

IFMJ

IFM

IFM

QP

IFM

ARG

QP

Description

QUARTZ PORPHYRY: As described previously. Sharp contacts at +35, parallel to banding. Cutby -55 to -65 fractures +/- chlorite, calcite.MAGNETITE-JASPER-CHERT IRON FORMATION with specularite: Up to 55% fgr, granular toargillaceous black magnetite (with specularite) as 0.5-15cm sections. Variable proportions ofstrong jasper and pale to med grey fgr chert bands 0.2-3cm thick. Well banded at +35 to +58,downhole, with local tight asymmetrical folds. Interval is cut by -45, +75 and banding parallelcalcite-py-qtz fractures, vnlts. Larger dm scale magnetite bands have concentrations of palegrey “rhombic” crystals as possible overprint. From 124.91-125.55m, QP dyke cutting parallel tobanding at +35.MAGNETITE-CHERT IRON FORMATION: Well banded 0.5-5cm alternating vgr granular toargillaceous magnetite and med grey- blue chert. Bands are straight, at +50.MAGNETITE-CHERT-GRUNERITE IRON FORMATION: Finely laminated to bandedmagnetite and med-pale grey chert with strong overprint of grunerite. Banding at +60. Cut byminor calcite-chlorite- pyrite fractures at -50.QUARTZ PORPHYRY-brecciated: As described previously, but finer grained and cut by adense net of chloritic microfractures at +40 to -60, grading into a breccia of milled, QPfragments in a milled, chloritic matrix, from 134.55-135m and 135.55-135.85m. Later brecciasections have edges at +60. From 135-135.10m: QP appears silicified, host seams (to 0.5cm)of pyrite. Lower contact is diffuse and chloritized.MAGNETITE-CHERT-GRUNERITE IRON FORMATION: Well banded, mm to 3cm sections ofvfgr argillaceous, dk grey-black magnetite with 0.5-3cm bands of pale-med grey chert at +50 to+55. Bands are straight to ragged and progressively stronger grunerite overprint, downhole. Cutby minor -60 fractures.GREY ARGILLITE: Pale to med grey, mm to cm laminated argillite with weak local 1-3mmchloritic partings. Minor mm scale pyrite +/- qtz seams. Laminae are straight, but highlytransposed to +50. From 140-141.72m: QP dyke parallel to laminae, at +55 to +60.QUARTZ PORPHYRY: mgr, massive, with scattered biotite wisps defining wk-mod internalfoliation at +40 to +50. Contacts are parallel to banding at +40.

Sample

16372163741637516376

16377

16378

16379

16380

16381

From_m

121.87124.00125.55128.00

129.00

131.60

133.33

137.05

140.00

To_m

124.00125.55128.00129.00

131.60

133.33

137.05

140.00

142.85

Interval_m

2.131.552.451.00

2.60

1.73

3.72

2.95

2.85

Litho

IMJCIMJCIMJCIMJC

IMC

IMCR

QPBX

IMCR

ARG

%SiO2

37.4049.6043.3043.40

39.20

41.70

54.40

39.80

60.20

%Fe2O3

56.5036.8051.0051.80

55.80

45.00

15.80

49.95

6.77

%TFe

39.5225.7435.6836.24

39.03

31.48

11.05

34.94

4.74

%Mt

SAT

54.5035.2044.8052.60

51.95

25.00

1.20

26.65

1.00

%Hm

CALC

0.020.003.810.00

0.00

0.19

0.89

1.04

0.84

%FeMt

99.7897.5790.86100.0

93.67

57.47

7.86

55.19

15.28

%FeHm

0.030.007.460.00

0.00

0.43

5.66

2.08

12.34

% FeOther

0.192.431.670.00

6.33

42.11

86.49

42.74

72.38

Hole: ES08-007

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/18/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

168.0

Page: 5 of 5

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -46.0

Start Date:

10/19/2008

Core Size : NQLogged Date: 11/10/2008

Diamond Drill Log

HOLE ID

ES08-007

From_m

143.13

To_m

168.00

Code

GWK

Description

GREYWACKE: Med grey-brown to pale grey downhole, with decreasing biotite content. Mostlymassive with <10% sections of 10-30cm banded, fgr argillaceous sections at +45. Cut by minor-45 and +45 calcite +/- qtz fractures.

Sample From_m To_m Interval_m Litho %

SiO2%

Fe2O3%

TFe%Mt

SAT

%Hm

CALC%

FeMt%

FeHm% FeOther

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-007 8.34 9.00 0.66 0.66 100.00% 0.37 56.06% NQ JT OCT 21 / 08ES08-007 9.00 12.00 3.00 2.80 93.33% 0.77 27.50% NQ JT OCT 21 / 08 All fractured and crushed coreES08-007 12.00 15.00 3.00 2.91 97.00% 2.46 84.54% NQ JT OCT 21 / 08ES08-007 15.00 18.00 3.00 2.86 95.33% 2.02 70.63% NQ JT OCT 21 / 08ES08-007 18.00 21.00 3.00 2.71 90.33% 1.08 39.85% NQ JT OCT 21 / 08 35cm crushed coreES08-007 21.00 24.00 3.00 2.80 93.33% 1.29 46.07% NQ JT OCT 21 / 08ES08-007 24.00 27.00 3.00 2.95 98.33% 1.46 49.49% NQ JT OCT 21 / 08 57cm crushed coreES08-007 27.00 30.00 3.00 2.94 98.00% 2.43 82.65% NQ JT OCT 21 / 08ES08-007 30.00 33.00 3.00 3.00 100.00% 2.21 73.67% NQ JT OCT 21 / 08ES08-007 33.00 36.00 3.00 2.87 95.67% 2.13 74.22% NQ JT OCT 21 / 08ES08-007 36.00 39.00 3.00 3.00 100.00% 2.69 89.67% NQ JT OCT 21 / 08ES08-007 39.00 42.00 3.00 2.95 98.33% 1.83 62.03% NQ JT OCT 21 / 08ES08-007 42.00 45.00 3.00 2.95 98.33% 2.08 70.51% NQ JT OCT 21 / 08ES08-007 45.00 48.00 3.00 2.95 98.33% 2.44 82.71% NQ JT OCT 21 / 08ES08-007 48.00 51.00 3.00 2.96 98.67% 1.98 66.89% NQ JT OCT 21 / 08ES08-007 51.00 54.00 3.00 2.92 97.33% 1.68 57.53% NQ JT OCT 21 / 08ES08-007 54.00 57.00 3.00 2.93 97.67% 2.49 84.98% NQ JT OCT 21 / 08ES08-007 57.00 60.00 3.00 2.94 98.00% 1.06 36.05% NQ JT OCT 21 / 08 All fractured and crushed coreES08-007 60.00 63.00 3.00 2.93 97.67% 2.34 79.86% NQ JT OCT 21 / 08ES08-007 63.00 66.00 3.00 3.00 100.00% 2.43 81.00% NQ JT OCT 21 / 08ES08-007 66.00 69.00 3.00 3.00 100.00% 2.85 95.00% NQ JT OCT 21 / 08 TestES08-007 69.00 72.00 3.00 2.94 98.00% 2.78 94.56% NQ JT OCT 21 / 08ES08-007 72.00 75.00 3.00 2.05 68.33% 3.01 146.83% NQ JT OCT 21 / 08ES08-007 75.00 78.00 3.00 3.00 100.00% 2.80 93.33% NQ JT OCT 21 / 08ES08-007 78.00 81.00 3.00 3.00 100.00% 2.95 98.33% NQ JT OCT 21 / 08ES08-007 81.00 84.00 3.00 2.88 96.00% 2.10 72.92% NQ JT OCT 21 / 08ES08-007 84.00 87.00 3.00 3.08 102.67% 2.60 84.42% NQ JT OCT 21 / 08ES08-007 87.00 90.00 3.00 3.00 100.00% 2.21 73.67% NQ JT OCT 21 / 08ES08-007 90.00 93.00 3.00 2.96 98.67% 2.47 83.45% NQ JT OCT 21 / 08ES08-007 93.00 96.00 3.00 3.00 100.00% 2.61 87.00% NQ JT OCT 21 / 08ES08-007 96.00 99.00 3.00 3.00 100.00% 2.82 94.00% NQ JT OCT 21 / 08ES08-007 99.00 102.00 3.00 2.93 97.67% 2.62 89.42% NQ JT OCT 21 / 08 12cm crushed coreES08-007 102.00 105.00 3.00 2.97 99.00% 2.05 69.02% NQ JT OCT 21 / 08 16cm crushed core

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-007 105.00 108.00 3.00 2.92 97.33% 1.72 58.90% NQ JT OCT 21 / 08ES08-007 108.00 111.00 3.00 3.00 100.00% 2.89 96.33% NQ JT OCT 21 / 08ES08-007 111.00 114.00 3.00 3.00 100.00% 2.71 90.33% NQ JT OCT 21 / 08ES08-007 114.00 117.00 3.00 2.95 98.33% 2.42 82.03% NQ JT OCT 21 / 08ES08-007 117.00 120.00 3.00 3.09 103.00% 1.13 36.57% NQ JT OCT 21 / 08 28cm crushed core, TestES08-007 120.00 123.00 3.00 2.85 95.00% 1.84 64.56% NQ JT OCT 21 / 08ES08-007 123.00 126.00 3.00 3.00 100.00% 2.59 86.33% NQ JT OCT 21 / 08ES08-007 126.00 129.00 3.00 2.92 97.33% 2.67 91.44% NQ JT OCT 21 / 08ES08-007 129.00 132.00 3.00 3.05 101.67% 2.55 83.61% NQ JT OCT 21 / 08ES08-007 132.00 135.00 3.00 2.87 95.67% 2.26 78.75% NQ JT OCT 21 / 08ES08-007 135.00 138.00 3.00 2.90 96.67% 2.11 72.76% NQ JT OCT 21 / 08ES08-007 138.00 141.00 3.00 3.00 100.00% 2.77 92.33% NQ JT OCT 21 / 08ES08-007 141.00 144.00 3.00 3.00 100.00% 2.49 83.00% NQ JT OCT 21 / 08ES08-007 144.00 147.00 3.00 2.95 98.33% 2.39 81.02% NQ JT OCT 21 / 08ES08-007 147.00 150.00 3.00 3.00 100.00% 2.69 89.67% NQ JT OCT 21 / 08ES08-007 150.00 153.00 3.00 3.00 100.00% 2.68 89.33% NQ JT OCT 21 / 08ES08-007 153.00 156.00 3.00 2.90 96.67% 2.42 83.45% NQ JT OCT 21 / 08ES08-007 156.00 159.00 3.00 3.00 100.00% 2.48 82.67% NQ JT OCT 21 / 08ES08-007 159.00 162.00 3.00 3.00 100.00% 2.48 82.67% NQ JT OCT 21 / 08ES08-007 162.00 165.00 3.00 2.94 98.00% 2.59 88.10% NQ JT OCT 21 / 08ES08-007 165.00 168.00 3.00 3.00 100.00% 2.79 93.00% NQ JT OCT 21 / 08 E.O.H. , Test

Hole: ES08-008

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/19/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

228.0

Page: 1 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -59.5

Start Date:

10/21/2008

Core Size : NQLogged Date: 11/12/2008

Diamond Drill Log

HOLE ID

ES08-008ES08-008ES08-008

ES08-008

ES08-008

ES08-008

ES08-008

From_m

0.000.926.78

29.40

48.00

52.30

60.00

To_m

0.926.7829.40

48.00

52.30

60.00

65.80

Code

CASOVERCONG

GWK

GWK

ARG

IFL

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:CONGLOMERATE: Pale grey, massive, mgr granular to conglomeratic downhole. From17.50m, conglomerate consists of poorly sorted, 0.5-1cm white siliceous fragments withaspect ratios of 4:1 to 6:1, aligned with moderate foliaton at +50 to +55. From 25m,groundmass becomes more biotitic. Core is broken and blocky to 18m, along low angle TCAand bedding parallel fractures with water stains +/- qtz-calcite vnlts. Upper sections havebedding parallel, patch Kspar infiltrations cut by -30 fine calcite fractures +/- epidote. Waterstaining to 21m.BIOTITE WACKE/PARAGNEISS: Gradational from above, with increased biotite as diffusebands alternating with pale grey siliceous sections with fgr chloritic wisps, at +55. Somediscrete edges to silica-chlorite patches discerable, but appear to be mostly gneissicsegregations. From 37m, unit become more biotitic with silica patches elongate at +60(pseudo conglomerate?). Entire interval is cut by -40 to -50 fractures +/- calcite, pyrite.Strain appears to increase downhole, but may be apparent due to increase biotite. Fine calcitefractures at +75.BIOTITE WACKE with interbeds OF CHLORITE-GARNET MUDSTONE: Dk grey-brownbiotite wacke with 30-40% sections (20-50cm) of chloritic siltstone/mudstone with 0.5-1cmchert bands and 0.5-1cm cgr overprinting garnets, local grunerite. Highly strained, transposedbands and mylonitic cleavage at +60 to +70. Trace py clots in chloritic sections. Gradesdownhole into fgr siltstone, argillite with less biotite, chlorite. Cut by minor -30 to -40qtz-ca+/-py fractures.GREY ARGILLITE: Pale grey-green, finely laminated, highly strained at +55 to +60. Local0.5-1cm qtz vns are folded, boudinaged and dismembered. Cut by rare low angle TCAstructures. Trace py along fractures and vnlts. From 57.05m: interbedded section ofchlorite-garnet-chert, highly strained along +60. Wk local magnetite, in chert bands.CHLORITE-GARNET MUDSTONE and CHERT-MAGNETITE IRON FORMATION:Gradational from above with 35-55% med grey-brown argillite (1-15cm) and 65-45% sectionsof chloritic siltstone, mudstone with pale grey chert +/- magnetite bands (1-10cm). Common0.3-1cm garnets and local grunerite. Strongly banded and cleaved at +50 to +70. Cut by -40,-60 ca-py fractures. Some py as fine seams, as well.

Sample

16382

1638316384

From_m

57.00

60.0063.00

To_m

60.00

63.0065.80

Interval_m

3.00

3.002.80

Litho

ARG

ILCMgtILCMgt

%SiO2

54.20

55.6058.20

%Fe2O3

25.00

23.3015.90

%TFe

17.49

16.3011.12

%Mt

SAT

9.60

0.270.60

%Hm

CALC

0.00

4.091.54

%FeMt

34.01

1.203.90

%FeHm

0.00

17.569.69

%Fe

Other

65.99

81.2586.41

CLAIM: KRL 3019667

Hole: ES08-008

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/19/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

228.0

Page: 2 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -59.5

Start Date:

10/21/2008

Core Size : NQLogged Date: 11/12/2008

Diamond Drill Log

HOLE ID

ES08-008

ES08-008

ES08-008

ES08-008

ES08-008

From_m

65.80

68.20

72.35

84.65

94.20

To_m

68.20

72.35

84.65

94.20

111.00

Code

IFML

QP

IFM

QP

IFMJ

Description

MAGNETITE-CHERT-CHLORITE IRON FORMATION: Up to 65% alternating 0.5-1cm fgrargillaceous magnetie and pale grey chert bands with up to 35% 1-40cm sections of chloriticmudstone with thicker 1-3cm chert bands, diss’d garnets and local grunerite. Interval is wellbanded at +60 to +50.BIOTITIC QUARTZ PORPHRY: Mgr, massive unit with possible subcm siliceous fragments,common biotite-sericite wisps parallel to foliation at +50. Upper contact is obscured by qtzveining cutting foliation obliquely at +80 and offset by -75 fractures. Lower contact is sharp, at+65. Unit cut by -65 to -50 calcitic fractures.MAGNETITE-CHERT +/- JASPER IRON FORMATION: Similar to above 65.80-68.20m, withless chloritic bands and equal proportions of 0.2-1cm bands of dke grey, silty toargillaceous magnetite and med grey chert with minor chloritic partings. Bands are straightto asymmetrically folded over 5-40cm, at +65. Fine waxy grey rhombic crystals in magnetite,as noted in DDH 007. Some refolded folds. From 77m, mod-strong grunerite. From75.85-76.18m: fgr biotite dyke, foliated at +45, with sharp contacts both parallel to bandingat +45 and oblique at -20. From 76.18m interval is cut by NE trending, SE dipping spacedfractures with cm offsets of bands. From 79-80.12m: biotite QP dyke. From 80.12-84.65m:Magnetite content increases to 60%, with med grey chert bands and up to 15% chloriticmudstone in lower section. Folded with axial planar cleavage of +55 to +65 and -45 plunge tothe east.QUARTZ PORPHYRY: As described previously, moderately foliated at +45. Upper contactobscured by fracturing, lower contact is bedding parallel at +45. Cut by -50 and +60 fractures+/- qtz vnlts. Highly broken along +50, -60 and +80 trends, from 91-93m.MAGNETITE-CHERT+/- JASPER IRON FORMATION (High Grade): Compared with previousIF section, this interval grades from well banded, cm scale mt-chert bands, into increasedmagnetite to 75% as thicker 2-20cm, finely laminated sections which are dk grey, silty. Lesserchert bands are 0.5-3cm, pale to med grey, to red jasper. Bands are straight to folded at +50to +60. Minor chloritic partings in upper 5m. Cut by -40 to -50 calcite +/- pyrite fractures.

Sample

16385

16386

1638716388163901639116392

1639316394163951639616397163981639916400

From_m

65.80

68.20

72.3575.0078.0080.1282.00

84.6588.0091.0094.2096.1499.00102.00103.98

To_m

68.20

72.35

75.0078.0080.1282.0084.65

88.0091.0094.2096.1499.00102.00103.98105.00

Interval_m

2.40

4.15

2.653.002.121.882.65

3.353.003.201.942.863.001.981.02

Litho

IMCL

QP

IMCIMCIMCQPIMCIMCL

QPQPQPIMCJIMCJIMCJIMCJIMCJ

%SiO2

50.80

65.30

42.6042.1556.9044.2049.70

65.3064.7064.3043.6046.1042.8044.2040.30

%Fe2O3

36.50

4.06

49.2046.3323.8048.6038.00

3.423.703.21

42.6047.3051.5051.2053.40

%TFe

25.53

2.84

34.4232.7216.6534.0026.58

2.392.592.2529.8033.0936.0335.8237.36

%Mt

SAT

20.70

0.40

46.4040.8515.2045.4032.20

0.600.950.2040.8047.5050.1051.2052.50

%Hm

CALC

0.60

0.38

0.000.000.430.000.00

0.020.000.270.000.000.000.000.00

%FeMt

58.66

10.19

95.4988.4566.0695.4385.88

18.1526.486.4496.9999.7799.18100.0100.0

%FeHm

1.65

9.46

0.000.001.800.000.00

0.500.008.470.000.000.000.000.00

%Fe

Other

39.69

80.35

4.5111.5532.144.5714.12

81.3573.5285.083.010.230.820.000.00

Hole: ES08-008

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/19/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

228.0

Page: 3 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -59.5

Start Date:

10/21/2008

Core Size : NQLogged Date: 11/12/2008

Diamond Drill Log

HOLE ID

ES08-008

ES08-008

ES08-008

ES08-008

From_m

111.00

117.00

124.10

150.00

To_m

117.00

124.10

150.00

164.33

Code

IFMJ

IFM

IFMJ

IFM

Description

MAGNETITE- JASPER IRON FORMATION with Specularite (High Grade): Gradational fromabove with >60% fgr granular silty magnetite with some vfgr specularite, with 0.5-3cm bandsof md-strongly hematitic jasper bands. Banding is straight at +65 to +70, with local isoclinalfolds at +25 to +70. Cut by minor qtz-ca-py fractures +/- chloritic gouge, at -30.MAGNETITE-CHERT IRON FORMATION (High Grade): Well banded section of 45-65% dkgrey, silty magnetite as 0.5-20cm bands, with 35-45% med grey chert as 0.2-3cm bands.Banding is mostly straight to stretched, attenuated at +65, with some tight isoclinal foldswith axes at +80 to -80, along core axis.Interval is cut by and broken along -30 and -60calcitic fractures. Some 1-2mm chloritic bands and partings. From 118.38-118.66m: Wellfoliated biotitic QP dyke at +55. From 123.38-123.65m: Strained, dismembered chert bandswith up to 3% py as clots, grains +/- chlorite.MAGNETITE-JASPER IRON FORMATION with Specularite (High Grade): Increasedproportion of fgr magnetite and variable fgr specularite as 1-30cm bands with lesser 20-40%0.5-2cm bands of jasper, pale grey chert bands. Most massive magnetite section is from127-130m. To 132m, banding is mostly straight, at +65 to +70, with some subcm folds parallelto banding and oblique at -75. Specularite as fine disseminated grains interstitial tomagnetite and also concentrated in mm scale laminae. Late cleavage overprints and dragssome of the original bands. From 130m: Early folds transposed into main banding, cleavagetrend, with fold axes at +65. From 132-134.50m: More regular bands trend +30, with fold axesat +65. From 134.50-146.04m: banding is locally transposed to +75, to +80. Entire unit is cutby sporadic calcite-py fractures at +35 to +45.

MAGNETITE-CHERT IRON FORMATION: Gradational from above with less jasper and morechert. Well banded, equal proportions of mgr granular, silty magnetite +/- specularite andwhite to pale grey chert bands 0.5-2cm thick. Common mm scale laminae, partings ofchlorite. Local mgr diss’d pyrite. Interval is banded at +65 and dragged to +80 from155-156m. Interval is cut by minor +35 to +45 fractures. From 160.28-160.72m: QP dyke.

Sample

16401164031640416405

164061640716409

1641016411164121641357551641416415164161641716418164191642116422164231642416425

From_m

105.00108.00111.00114.00

117.00120.00123.00

124.10126.00129.00130.00132.00135.00138.00141.00144.00146.04147.00150.00153.00156.00159.00162.00

To_m

108.00111.00114.00117.00

120.00123.00124.10

126.00129.00130.00132.00135.00138.00141.00144.00146.04147.00150.00153.00156.00159.00162.00164.33

Interval_m

3.003.003.003.00

3.003.001.10

1.903.001.002.003.003.003.003.002.040.963.003.003.003.003.002.33

Litho

IMCJIMCJIMJIMJ

IMCIMCIMC

IMJIMJIMJIMJIMJIMJIMJIMJIMJIMJIMJIMCIMCIMCIMCIMC

%SiO2

39.6039.0044.8039.70

43.8040.3042.90

40.1041.4036.9043.2040.2042.1043.9042.6042.3039.4041.9545.5044.0041.7048.3041.00

%Fe2O3

55.6055.3048.7053.35

46.6054.1552.40

54.7054.9059.9050.5053.7049.2049.3050.7050.1054.2051.9545.9047.9050.3039.8052.00

%TFe

38.8938.6834.0737.32

32.6037.8836.66

38.2738.4141.9035.3337.5734.4234.4935.4735.0537.9236.3432.1133.5135.1927.8436.38

%Mt

SAT53.4056.1048.1051.60

44.4055.5050.90

48.5045.5056.8045.0044.8046.4044.3046.6044.7054.2048.8545.1048.8050.0039.1050.50

%Hm

CALC0.000.000.000.00

0.000.000.00

4.537.841.153.957.360.963.172.503.860.001.420.000.000.000.000.00

%FeMt

98.9499.8699.88100.0

98.4299.8597.90

91.7185.7398.0992.1786.3097.5592.9595.0792.29100.097.2798.8399.1597.9396.7998.33

%FeHm

0.000.000.000.00

0.000.000.00

8.2914.271.917.8313.701.956.434.937.710.002.730.000.000.000.000.00

%Fe

Other1.060.140.120.00

1.580.152.10

0.000.000.000.000.000.500.620.000.000.000.001.170.852.073.211.67

Hole: ES08-008

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644581.14

Elevation (m):

542803.3

Depth (m): 418.04Logged By:

10/19/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

228.0

Page: 4 of 4

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 179

Dip : -59.5

Start Date:

10/21/2008

Core Size : NQLogged Date: 11/12/2008

Diamond Drill Log

HOLE ID

ES08-008

ES08-008

ES08-008

ES08-008

ES08-008

From_m

164.33

170.05

190.75

197.65

203.06

To_m

170.05

190.75

197.65

203.06

228.00

Code

IFMJ

IFM

IFM

ARG

GWK

Description

MAGNETITE-JASPER-CHERT IRON FORMATION (High Grade): Interval grades from thick10-15cm bands of med-dk grey granular, laminated magnetite and less 0.5-3cm jasperbands. Downhole from 168m, there is increased jasper, cher as 0.5-1cm bands which areisoclinally folded and dismembered. Magnetite sections have fine laminae +/- hematite,chlorite partings. Banding/cleavage is at +50 to +60. Cut by scattered qtz-calcite gashessubparallel to banding and at -30 to -40. Overall, increase pale grey, white chert componentdownhole.MAGNETITE-CHERT IRON FORMATION; Similar to interval 150-164.33m, above. Wellbanded fgr silty, magnetite as 0.5-15cm bands separated by 0.5-2cm pale grey chert bands.Fine mm scale chloritic partings along mt laminae. Bands are mostly straight at +45 to +55and are locally dragged, and transposed into +75 to +85 trends. Some relict asymmetricalfold closures. Interval is cut by minor -35 fractures. Rare dm scale, banding parallel quartzveins. Wk local grunerite. From 188-193m, unit is cut by dm spaced bedding along NNWtrend, dipping steeply W. Cut and offset by -30 to -40 fractures.

MAGNETITE-CHERT-GRUNERITE IRON FORMATION (High Grade): Alternating sectionsof 2-20cm finely laminated magnetite-grunerite and pale to med grey chert bands in sections10-50cm thick. Banded at +70 to +60. Cut by oblique fractures in upper section, and -30 to-40 fractures throughout. From 194.55-196m: Dk grey-black breccia of dense magnetite andyellow grunerite. Very heavy and hard. Breccia contacts are parallel to banding at +75 and+65. Late fracturing is at +80.GREY ARGILLITE: (with carbonaceous sections). Finely laminated, med grey to paleyellow-grey argillite. Highly strained to mylonitic at +75 to +85. Locally wkly chloritic. Cut byscattered qtz-ca+/- py vnlts, boudins which are also deformed by high strain. Cut by late -40calcitic fractures.BIOTITE WACKE: fgr, med grey-brown. Massive, with rare beds at +60 to +50. Cut by localbiotite QP dykes parallel to bedding over 40-60cm.

Sample

164261642716429

1643016431164321643316434164351643616438164391644016441

16442

From_m

164.33166.00168.00

170.05171.00174.00177.00180.00183.00186.00189.00190.75192.00194.55

197.65

To_m

166.00168.00170.05

171.00174.00177.00180.00183.00186.00189.00190.75192.00194.55197.65

201.00

Interval_m

1.672.002.05

0.953.003.003.003.003.003.001.751.252.553.10

3.35

Litho

IMJCIMJCIMJC

IMCIMCIMCIMCIMCIMCIMCIMCIMCRIMCRIMCR

ARG

%SiO2

44.4041.3041.30

43.4043.7039.2042.7045.6043.0039.9041.0039.7042.9039.50

56.50

%Fe2O3

48.9053.4052.10

49.5549.4049.4047.7047.8051.8054.1054.2553.4048.0040.00

12.30

%TFe

34.2137.3636.45

34.6634.5634.5633.3733.4436.2437.8537.9537.3633.5827.98

8.60

%Mt

SAT47.5046.1053.30

51.6551.4048.3045.3048.6051.5047.7050.8035.3031.6015.10

1.10

%Hm

CALC0.004.610.00

0.000.000.000.000.000.000.000.000.000.000.00

1.09

%FeMt

99.3989.30100.0

100.0100.096.1294.4299.1796.1988.2090.6764.9565.6338.70

9.25

%FeHm

0.008.630.00

0.000.000.000.000.000.000.000.000.000.000.00

8.82

%Fe

Other0.612.070.00

0.000.003.885.580.833.8111.809.3335.0534.3761.30

81.93

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-008 6.78 9.00 2.22 2.22 100.00% 0.76 34.23% NQ JT OCT 22 / 08ES08-008 9.00 12.00 3.00 3.00 100.00% 1.92 64.00% NQ JT OCT 22 / 08ES08-008 12.00 15.00 3.00 2.66 88.67% 1.32 49.62% NQ JT OCT 22 / 08 Broken and blockyES08-008 15.00 18.00 3.00 2.72 90.67% 0.93 34.19% NQ JT OCT 22 / 08 Broken and blockyES08-008 18.00 21.00 3.00 3.05 101.67% 1.74 57.05% NQ JT OCT 22 / 08ES08-008 21.00 24.00 3.00 3.00 100.00% 2.42 80.67% NQ JT OCT 22 / 08ES08-008 24.00 27.00 3.00 3.00 100.00% 2.68 89.33% NQ JT OCT 22 / 08ES08-008 27.00 30.00 3.00 3.00 100.00% 2.76 92.00% NQ JT OCT 22 / 08ES08-008 30.00 33.00 3.00 2.92 97.33% 2.57 88.01% NQ JT OCT 22 / 08ES08-008 33.00 36.00 3.00 2.96 98.67% 2.16 72.97% NQ JT OCT 22 / 08ES08-008 36.00 39.00 3.00 3.00 100.00% 2.79 93.00% NQ JT OCT 22 / 08ES08-008 39.00 42.00 3.00 2.96 98.67% 1.69 57.09% NQ JT OCT 22 / 08ES08-008 42.00 45.00 3.00 2.92 97.33% 2.72 93.15% NQ JT OCT 22 / 08ES08-008 45.00 48.00 3.00 2.95 98.33% 2.80 94.92% NQ JT OCT 22 / 08ES08-008 48.00 51.00 3.00 2.95 98.33% 2.26 76.61% NQ JT OCT 22 / 08ES08-008 51.00 54.00 3.00 3.00 100.00% 2.65 88.33% NQ JT OCT 22 / 08ES08-008 54.00 57.00 3.00 3.00 100.00% 2.79 93.00% NQ JT OCT 22 / 08ES08-008 57.00 60.00 3.00 3.00 100.00% 2.46 82.00% NQ JT OCT 22 / 08ES08-008 60.00 63.00 3.00 2.95 98.33% 2.49 84.41% NQ JT OCT 22 / 08ES08-008 63.00 66.00 3.00 2.91 97.00% 2.24 76.98% NQ JT OCT 22 / 08ES08-008 66.00 69.00 3.00 2.95 98.33% 2.79 94.58% NQ JT OCT 22 / 08ES08-008 69.00 72.00 3.00 3.00 100.00% 2.73 91.00% NQ JT OCT 22 / 08 TestES08-008 72.00 75.00 3.00 3.00 100.00% 1.63 54.33% NQ JT OCT 22 / 08ES08-008 75.00 78.00 3.00 2.95 98.33% 2.35 79.66% NQ JT OCT 22 / 08ES08-008 78.00 81.00 3.00 3.04 101.33% 2.72 89.47% NQ JT OCT 22 / 08ES08-008 81.00 84.00 3.00 2.95 98.33% 2.60 88.14% NQ JT OCT 22 / 08ES08-008 84.00 87.00 3.00 2.91 97.00% 1.84 63.23% NQ JT OCT 22 / 08ES08-008 87.00 90.00 3.00 3.00 100.00% 2.77 92.33% NQ JT OCT 22 / 08ES08-008 90.00 93.00 3.00 2.84 94.67% 1.18 41.55% NQ JT OCT 22 / 08 1.49m crushed coreES08-008 93.00 96.00 3.00 2.90 96.67% 2.10 72.41% NQ JT OCT 22 / 08ES08-008 96.00 99.00 3.00 3.00 100.00% 2.14 71.33% NQ JT OCT 22 / 08ES08-008 99.00 102.00 3.00 2.97 99.00% 2.71 91.25% NQ JT OCT 23 / 08ES08-008 102.00 105.00 3.00 3.00 100.00% 2.61 87.00% NQ JT OCT 23 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-008 105.00 108.00 3.00 3.00 100.00% 2.41 80.33% NQ JT OCT 23 / 08ES08-008 108.00 111.00 3.00 3.00 100.00% 2.59 86.33% NQ JT OCT 23 / 08ES08-008 111.00 114.00 3.00 2.94 98.00% 2.69 91.50% NQ JT OCT 23 / 08ES08-008 114.00 117.00 3.00 2.93 97.67% 2.48 84.64% NQ JT OCT 23 / 08ES08-008 117.00 120.00 3.00 2.95 98.33% 2.02 68.47% NQ JT OCT 23 / 08ES08-008 120.00 123.00 3.00 2.94 98.00% 2.65 90.14% NQ JT OCT 23 / 08 TestES08-008 123.00 126.00 3.00 3.04 101.33% 2.44 80.26% NQ JT OCT 23 / 08ES08-008 126.00 129.00 3.00 2.95 98.33% 2.37 80.34% NQ JT OCT 23 / 08ES08-008 129.00 132.00 3.00 2.95 98.33% 2.61 88.47% NQ JT OCT 23 / 08ES08-008 132.00 135.00 3.00 3.00 100.00% 2.85 95.00% NQ JT OCT 23 / 08ES08-008 135.00 138.00 3.00 3.00 100.00% 2.81 93.67% NQ JT OCT 23 / 08ES08-008 138.00 141.00 3.00 3.00 100.00% 2.44 81.33% NQ JT OCT 23 / 08ES08-008 141.00 144.00 3.00 3.00 100.00% 2.88 96.00% NQ JT OCT 23 / 08ES08-008 144.00 147.00 3.00 3.06 102.00% 2.64 86.27% NQ JT OCT 23 / 08ES08-008 147.00 150.00 3.00 2.80 93.33% 1.95 69.64% NQ JT OCT 23 / 08ES08-008 150.00 153.00 3.00 3.03 101.00% 2.82 93.07% NQ JT OCT 23 / 08ES08-008 153.00 156.00 3.00 2.96 98.67% 2.58 87.16% NQ JT OCT 23 / 08ES08-008 156.00 159.00 3.00 3.00 100.00% 2.91 97.00% NQ JT OCT 23 / 08ES08-008 159.00 162.00 3.00 2.94 98.00% 2.40 81.63% NQ JT OCT 23 / 08ES08-008 162.00 165.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 23 / 08ES08-008 165.00 168.00 3.00 3.00 100.00% 2.58 86.00% NQ JT OCT 23 / 08ES08-008 168.00 171.00 3.00 3.00 100.00% 2.83 94.33% NQ JT OCT 23 / 08ES08-008 171.00 174.00 3.00 2.94 98.00% 2.84 96.60% NQ JT OCT 23 / 08 TestES08-008 174.00 177.00 3.00 3.06 102.00% 2.97 97.06% NQ JT OCT 23 / 08ES08-008 177.00 180.00 3.00 2.93 97.67% 2.79 95.22% NQ JT OCT 23 / 08ES08-008 180.00 183.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 23 / 08ES08-008 183.00 186.00 3.00 3.00 100.00% 3.00 100.00% NQ JT OCT 23 / 08ES08-008 186.00 189.00 3.00 3.04 101.33% 2.78 91.45% NQ JT OCT 23 / 08ES08-008 189.00 192.00 3.00 2.96 98.67% 2.70 91.22% NQ JT OCT 23 / 08ES08-008 192.00 195.00 3.00 3.00 100.00% 2.81 93.67% NQ JT OCT 23 / 08ES08-008 195.00 198.00 3.00 2.84 94.67% 1.64 57.75% NQ JT OCT 23 / 08 71cm crushed coreES08-008 198.00 201.00 3.00 3.00 100.00% 1.99 66.33% NQ JT OCT 23 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-008 201.00 204.00 3.00 3.00 100.00% 2.28 76.00% NQ JT OCT 23 / 08ES08-008 204.00 207.00 3.00 3.00 100.00% 2.36 78.67% NQ JT OCT 23 / 08ES08-008 207.00 210.00 3.00 3.00 100.00% 2.65 88.33% NQ JT OCT 23 / 08ES08-008 210.00 213.00 3.00 2.96 98.67% 2.35 79.39% NQ JT OCT 23 / 08ES08-008 213.00 216.00 3.00 3.00 100.00% 2.74 91.33% NQ JT OCT 23 / 08ES08-008 216.00 219.00 3.00 2.96 98.67% 2.30 77.70% NQ JT OCT 23 / 08ES08-008 219.00 222.00 3.00 3.00 100.00% 2.25 75.00% NQ JT OCT 23 / 08ES08-008 222.00 225.00 3.00 3.00 100.00% 2.34 78.00% NQ JT OCT 23 / 08ES08-008 225.00 228.00 3.00 2.95 98.33% 2.70 91.53% NQ JT OCT 23 / 08 E.O.H.

Hole: ES08-009

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644248.96

Elevation (m):

541791.32

Depth (m): 418.76Logged By:

10/21/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

201.0

Page: 1 of 2

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -45.0

Start Date:

10/23/2008

Core Size : NQLogged Date: 11/14/2008

Diamond Drill Log

HOLE ID

ES08-009ES08-009ES08-009

ES08-009

ES08-009

ES08-009

From_m

0.001.132.70

101.35

120.00

150.00

To_m

1.132.70101.35

120.00

150.00

165.00

Code

CASOVERGWK

IFMJ

IFM

IFML

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:GREYWACKE: Pale grey-brown, wk-mod biotite, mostly massive with 10-30cm argillaceousintervals at +45 to +35. Cut by sections/dykes(?) of biotitic quartz porphyry, foliated at +40. Unitis cut by -45 to -35 calcite +/- py fractures, with local low angle TCA fractures of calcite-py (NNWtrending, W dipping). Near the lower contact with iron formation, unit is cut by net of chloriticmicrofractures with fine grains and gashes of qtz-K feldspar. Lower contact is 5cm, fine milledbreccia with chloritic matrix, at +45 (parallel to banding).MAGNETITE-JASPER-CHERT IRON FORMATION (High Grade): Alternating 0.5-3cm bandsof med-dk grey laminated fgr argillaceous magnetite and specular hematite, and mod-strongjasper, grey chert. Well banded at +30 to +45. From 111m, magnetite proportion increases to60%, in 5-20cm argillaceous sections, separated by thicker jasper, chert bands 2-5cm. Cut byragged calcite wisps, gashes and banding parallel seams, as well as oblique fractures at -60and along NNW trends. Downhole, banding is straight to asymmetrically folded, with small scalerefolded folds from 117m. From 115.84-116.14m: Cgr, dioritic dyke with sharp, banding parallelcontacts at +30 and +20. Foliated at +30. From 112.22-112.60m 10cm thick jigsaw fitmicrobreccia of calcite, at -75.MAGNETITE-CHERT IRON FORMATION (High Grade): Gradational from above, with lessjasper and more chert, as 0.5-2cm bands at +35 to +40 and asymmetrically folded. Fold axestrend +55 to +60. Some refolded folds discernable. Both magnetite and chert bands are vgr,with decreasing specularite content downhole. Interval is cut by dm spaced -50calcite+/-py+/-qtz fractures, also along banding. From 130.57-138.30m: Section with 20%biotite-calcite dykes 5cm to >1m thick; subparalllel to banding and also foliated and foldedalong main banding, cleavage trends. From 142m: Magnetite sections are more silty, with mmscale laminae +/- chloritic partings +/- rare pyrite, minor qtz-ca boudins. From145.80-146.15m: and 146.67-147.00m: biotitic dykes at +20, oblique to banding at +50. From148m: cut by spaced ca-py-chl fractures at -65 to -80, grading into a blocky+E80 section withfault gouge section from 150.20-151m . At 150.69m: 10cm carbonaceous fault gouge.MAGNETITE-CHERT-CHLORITE IRON FORMATION: Fgr, argillaceous and finely laminatedmagnetite with 1-5cm sections of pale-med grey zoned chert and mm to 5cm bands ofmagnetic,chloritic mudstone. Magnetite sections seem sooty, carbonaceous. Well banded at+35. Increasing chlorite content and decreasing magnetite downhole. Cut by spaced -60 to -45calcite-qtz-py +/- chlorite fractures, with minor fault gouge. Core is broken, blocky to154.50m. From 156m, chloritic mudstone +/- mt bands are more defined and from 159m,contain mm scale garnets in 1-5cm bands with wk local grunerite.

Sample

16443

16444164451644616448164491645016451

164521645316455164561645716458164591646016461164621646316464

From_m

99.00

101.35104.00105.00108.00111.00114.00117.00

120.00123.00126.00129.00132.00135.25138.30141.00142.00144.00147.00150.00

To_m

101.35

104.00105.00108.00111.00114.00117.00120.00

123.00126.00129.00132.00135.25138.30141.00142.00144.00147.00150.00153.00

Interval_m

2.35

2.651.003.003.003.003.003.00

3.003.003.003.003.253.052.701.002.003.003.003.00

Litho

GWK

IMJCIMJCIMJCIMJCIMJCIMJCIMJC

IMCIMCIMCIMCSIMCIMCIMCIMCIMCIMCIMCIMCL

%SiO2

63.30

41.4042.4041.9041.6042.5042.0038.90

39.8040.9042.5545.6039.8043.8044.2043.7041.1043.4541.1042.60

%Fe2O3

8.70

46.6051.3050.7552.3049.9049.8053.80

53.4052.3050.8033.7053.7042.7048.5049.6052.6044.3551.8045.90

%TFe

6.09

32.6035.8935.5036.5934.9134.8437.64

37.3636.5935.5423.5737.5729.8733.9334.7036.8031.0236.2432.11

%Mt

SAT

0.00

41.8039.0044.9041.5039.3049.1046.00

51.5052.0050.6031.4055.7542.1049.1048.4051.5042.2053.4037.50

%Hm

CALC

0.00

2.5010.034.319.248.670.005.55

0.000.000.000.000.000.000.000.000.000.000.000.00

%FeMt

0.00

92.7878.6491.5282.0881.47100.088.44

99.11100.099.7382.16100.097.9697.7796.3497.2493.9699.3484.34

%FeHm

0.00

5.3619.558.4817.6617.360.0010.31

0.000.000.000.000.000.000.000.000.000.000.000.00

% FeOther

100.00

1.861.820.000.261.170.001.25

0.890.000.2717.840.002.042.233.662.766.040.6615.66

CLAIM: KRL 3019666

Hole: ES08-009

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644248.96

Elevation (m):

541791.32

Depth (m): 418.76Logged By:

10/21/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

201.0

Page: 2 of 2

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -45.0

Start Date:

10/23/2008

Core Size : NQLogged Date: 11/14/2008

Diamond Drill Log

HOLE ID

ES08-009

ES08-009

ES08-009

From_m

165.00

170.80

181.00

To_m

170.80

181.00

201.00

Code

IFML

ARG

ARG

Description

MAGNETITE-CHERT-CHLORITE-GARNET IRON FORMATION: With mod-strong gruneriteoverprint. Gradational from above, with incr. grunerite, imparting grey-black-yellow bandedappearance. Relict diss’d magnetite in grunerite bands 1-5cm wide. From 166.65m, mm scalegarnets in 2-15cm bands of chloritic siltstone, mudstone. Some intercalated grey argillitesections. Entire interval is well banded at +40, cut by minor late calcite-py fractures. From169.75-170.52m: Biotitic QP dyke with chilled margins. Contacts are sharp and parallel tobanding at +40 to +35.GREY ARGILLITE: Med grey, finely laminated argillite at +35 to +40. Weakly carbonaceous.Intensely strained with moderate sericite alteration along cleavage planes. Rare +50 fractures ofcalcite-py +/- chlorite.BANDED ARGILLLITE/QUARTZ-SERICITE-CHLORITE SCHIST: Gradational from above, intoalternating bands of med grey siliceous siltstone (with dk grey specks) and thick 0.2-1cmsections of pale grey-green, soft sericitic and possibly argillaceous material. Highly strainedinto quartz – sericte schist with relict subcm qtz boudins. Textures may have beenconglomeratic (?). Banding and schistosity at +35 to +40. Trace to 0.5% pyrite disseminatedalong schistosity planes. At 182.75m. Some refolded folds.

Sample

16465164661646816469

1647016471

16472

From_m

153.00156.00159.00162.00

165.00168.00

170.80

To_m

156.00159.00162.00165.00

168.00170.80

172.60

Interval_m

3.003.003.003.00

3.002.80

1.80

Litho

IMCLIMCLIMCLIMCL

IMCLRIMCLR

ARG

%SiO2

44.6044.2543.6046.00

45.2056.40

59.60

%Fe2O3

44.1041.9540.1041.20

43.1018.70

10.40

%TFe

30.8529.3528.0528.82

30.1513.08

7.28

%Mt

SAT36.1031.2527.4027.70

21.200.35

0.80

%Hm

CALC0.000.000.000.00

0.001.97

0.66

%FeMt

82.1075.4769.8767.73

50.761.94

7.96

%FeHm

0.000.000.000.00

0.0010.53

6.34

% FeOther

17.9024.5330.1332.27

49.2487.54

85.71

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-009 2.70 3.00 0.30 0.30 100.00% 0.12 40.00% NQ JT OCT 24 / 08ES08-009 3.00 6.00 3.00 2.77 92.33% 0.78 28.16% NQ JT OCT 24 / 08ES08-009 6.00 9.00 3.00 3.08 102.67% 1.21 39.29% NQ JT OCT 24 / 08ES08-009 9.00 12.00 3.00 3.05 101.67% 1.55 50.82% NQ JT OCT 24 / 08ES08-009 12.00 15.00 3.00 3.00 100.00% 2.05 68.33% NQ JT OCT 24 / 08ES08-009 15.00 18.00 3.00 3.00 100.00% 2.59 86.33% NQ JT OCT 24 / 08ES08-009 18.00 21.00 3.00 3.00 100.00% 2.78 92.67% NQ JT OCT 24 / 08ES08-009 21.00 24.00 3.00 3.00 100.00% 2.27 75.67% NQ JT OCT 24 / 08ES08-009 24.00 27.00 3.00 2.90 96.67% 2.51 86.55% NQ JT OCT 24 / 08ES08-009 27.00 30.00 3.00 3.00 100.00% 2.21 73.67% NQ JT OCT 24 / 08ES08-009 30.00 33.00 3.00 3.00 100.00% 1.64 54.67% NQ JT OCT 24 / 08ES08-009 33.00 36.00 3.00 2.94 98.00% 1.27 43.20% NQ JT OCT 24 / 08ES08-009 36.00 39.00 3.00 2.83 94.33% 1.75 61.84% NQ JT OCT 24 / 08 7cm gouge / 49cm crushed coreES08-009 39.00 42.00 3.00 3.00 100.00% 2.30 76.67% NQ JT OCT 24 / 08ES08-009 42.00 45.00 3.00 2.93 97.67% 1.80 61.43% NQ JT OCT 24 / 08ES08-009 45.00 48.00 3.00 3.00 100.00% 2.71 90.33% NQ JT OCT 24 / 08ES08-009 48.00 51.00 3.00 2.95 98.33% 2.39 81.02% NQ JT OCT 24 / 08ES08-009 51.00 54.00 3.00 2.93 97.67% 1.38 47.10% NQ JT OCT 24 / 08ES08-009 54.00 57.00 3.00 3.00 100.00% 2.08 69.33% NQ JT OCT 24 / 08ES08-009 57.00 60.00 3.00 2.86 95.33% 2.13 74.48% NQ JT OCT 24 / 08ES08-009 60.00 63.00 3.00 3.05 101.67% 2.46 80.66% NQ JT OCT 24 / 08 TestES08-009 63.00 66.00 3.00 3.00 100.00% 2.75 91.67% NQ JT OCT 24 / 08ES08-009 66.00 69.00 3.00 3.00 100.00% 2.18 72.67% NQ JT OCT 24 / 08ES08-009 69.00 72.00 3.00 3.00 100.00% 2.73 91.00% NQ JT OCT 24 / 08ES08-009 72.00 75.00 3.00 2.95 98.33% 1.95 66.10% NQ JT OCT 24 / 08ES08-009 75.00 78.00 3.00 2.95 98.33% 2.46 83.39% NQ JT OCT 24 / 08ES08-009 78.00 81.00 3.00 3.00 100.00% 1.60 53.33% NQ JT OCT 24 / 08 79.15m Bit change / 7cm caveES08-009 81.00 84.00 3.00 3.04 101.33% 1.61 52.96% NQ JT OCT 24 / 08ES08-009 84.00 87.00 3.00 2.92 97.33% 2.66 91.10% NQ JT OCT 24 / 08ES08-009 87.00 90.00 3.00 3.00 100.00% 2.09 69.67% NQ JT OCT 24 / 08ES08-009 90.00 93.00 3.00 3.00 100.00% 2.62 87.33% NQ JT OCT 24 / 08ES08-009 93.00 96.00 3.00 2.93 97.67% 2.76 94.20% NQ JT OCT 24 / 08ES08-009 96.00 99.00 3.00 3.00 100.00% 2.37 79.00% NQ JT OCT 24 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-009 99.00 102.00 3.00 3.00 100.00% 1.94 64.67% NQ JT OCT 24 / 08ES08-009 102.00 105.00 3.00 2.93 97.67% 2.55 87.03% NQ JT OCT 24 / 08ES08-009 105.00 108.00 3.00 3.00 100.00% 2.73 91.00% NQ JT OCT 24 / 08ES08-009 108.00 111.00 3.00 3.00 100.00% 2.65 88.33% NQ JT OCT 24 / 08ES08-009 111.00 114.00 3.00 3.00 100.00% 2.76 92.00% NQ JT OCT 24 / 08 TestES08-009 114.00 117.00 3.00 3.06 102.00% 2.73 89.22% NQ JT OCT 24 / 08ES08-009 117.00 120.00 3.00 2.94 98.00% 2.44 82.99% NQ JT OCT 24 / 08ES08-009 120.00 123.00 3.00 3.00 100.00% 2.78 92.67% NQ JT OCT 24 / 08ES08-009 123.00 126.00 3.00 3.00 100.00% 2.60 86.67% NQ JT OCT 24 / 08ES08-009 126.00 129.00 3.00 3.00 100.00% 2.33 77.67% NQ JT OCT 24 / 08ES08-009 129.00 132.00 3.00 2.95 98.33% 2.63 89.15% NQ JT OCT 24 / 08ES08-009 132.00 135.00 3.00 3.10 103.33% 2.72 87.74% NQ JT OCT 24 / 08ES08-009 135.00 138.00 3.00 2.94 98.00% 2.73 92.86% NQ JT OCT 24 / 08ES08-009 138.00 141.00 3.00 3.02 100.67% 2.82 93.38% NQ JT OCT 25 / 08ES08-009 141.00 144.00 3.00 3.00 100.00% 2.72 90.67% NQ JT OCT 25 / 08ES08-009 144.00 147.00 3.00 3.00 100.00% 2.53 84.33% NQ JT OCT 25 / 08ES08-009 147.00 150.00 3.00 2.89 96.33% 2.43 84.08% NQ JT OCT 25 / 08ES08-009 150.00 153.00 3.00 2.59 86.33% 1.26 48.65% NQ JT OCT 25 / 08 79cm gouge and crushed coreES08-009 153.00 156.00 3.00 2.88 96.00% 2.06 71.53% NQ JT OCT 25 / 08 13cm gouge and crushed coreES08-009 156.00 159.00 3.00 3.03 101.00% 2.05 67.66% NQ JT OCT 25 / 08ES08-009 159.00 162.00 3.00 3.00 100.00% 2.95 98.33% NQ JT OCT 25 / 08ES08-009 162.00 165.00 3.00 3.00 100.00% 2.80 93.33% NQ JT OCT 25 / 08 TestES08-009 165.00 168.00 3.00 3.06 102.00% 2.95 96.41% NQ JT OCT 25 / 08ES08-009 168.00 171.00 3.00 3.00 100.00% 2.94 98.00% NQ JT OCT 25 / 08ES08-009 171.00 174.00 3.00 3.07 102.33% 2.72 88.60% NQ JT OCT 25 / 08ES08-009 174.00 177.00 3.00 2.95 98.33% 2.04 69.15% NQ JT OCT 25 / 08ES08-009 177.00 180.00 3.00 3.00 100.00% 2.86 95.33% NQ JT OCT 25 / 08ES08-009 180.00 183.00 3.00 2.98 99.33% 2.32 77.85% NQ JT OCT 25 / 08ES08-009 183.00 186.00 3.00 3.05 101.67% 2.71 88.85% NQ JT OCT 25 / 08ES08-009 186.00 189.00 3.00 2.97 99.00% 2.64 88.89% NQ JT OCT 25 / 08ES08-009 189.00 192.00 3.00 2.95 98.33% 2.68 90.85% NQ JT OCT 25 / 08ES08-009 192.00 195.00 3.00 3.06 102.00% 2.98 97.39% NQ JT OCT 25 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-009 195.00 198.00 3.00 2.98 99.33% 2.75 92.28% NQ JT OCT 25 / 08ES08-009 198.00 201.00 3.00 3.00 100.00% 2.42 80.67% NQ JT OCT 25 / 08 E.O.H.

Hole: ES08-010

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644263.98

Elevation (m):

541982.95

Depth (m): 417.8Logged By:

10/23/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

189.0

Page: 1 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -46.5

Start Date:

10/24/2008

Core Size : NQLogged Date: 11/15/2008

Diamond Drill Log

HOLE ID

ES08-010ES08-010ES08-010

ES08-010

ES08-010

ES08-010

From_m

0.001.256.65

87.92

98.60

105.43

To_m

1.256.6587.92

98.60

105.43

115.04

Code

CASOVERGWK

IFMJ

IFMJ

IFMJ

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:GREYWACKE: Pale to med grey-brown, massive. Mostly silty quartoze beds with local5-40cm sections of pale grey-green argillite. Minor bedding at +45 to +30 downhole. Cut byminor -50 to -60 calcite – py fractures. Some sections with +70 to +80 and -70 fractures, aswell. To 9m, core is blocky and water stained. From 14.55-15.25m: Cgr dioritic dyke. From27.00-31.00m Interbeds of grey-green siltstone, argillite at +40. Cut by strained and raggedqtz veins (3-7cm). From 42.00m, alternating argillaceous and silty beds indicate fininguphole at several locations: 44.80m, 47.00m, 49.90m. From 87.65-87.92m Highly milled tobrecciated, mylontic at +30. 10-15% pyrite as wisps, seams from mm to 1cm thick; alongfoliation, within microfolds and cleavage of schist.MAGNETITE-CHERT +/- JASPER IRON FORMATION: Alternating 0.5-2cm section of dkgrey, finely laminated silty magnetite and med-dk grey chert at +40 to +30. Minor wk-modjasper bands from 93-94.40m. Mod to wk grunerite along mt-chert bands. Banding is mostlystraight, with 20-50cm open asymmetrical folds from 93m, with axial plane at +35. Interval iscut by minor -50 to -60 and some +65 calcite –py fractures. Trace cgr pyrite grains, clots to0.5cm which overprint cleavage. From 97.65-98.45m: Grey-brown interbed or dyke of biotitewacke (?). Sharp contacts and internal foliation at +35.MAGNETITE-JASPER IRON FORMATION with SPECULARITE (High Grade): Well banded,alternating sections of 0.5-5cm laminated, med-dk grey silty magnetite and specularite, with0.502cm bands of jasper. Rare pale grey chert bands to 1cm. Banding is mostly straight, at+35. Some refolded folds noted. Interval is cut by -65 to -80 calcite +/- py fractures. Rareqtz-ca seams along band margins.MAGNETITE-CHERT-JASPER IRON FORMATION: Gradational from above, with increasedchert>jasper bands and local banding parallel biotitic to dioritic dykes 10-40cm thick.Magnetite occurs as 0.5-10cm laminated to massive sections of dk to med grey silty grains +/-interstitial qtz/calcite grains. Variably hematitic jasper bands 0.2-2cm with minor med grey,wkly hematitic chert bands. Some vfgr specularite with mt laminae. Banding is straight, at+30 to +45, to +55 locally. Some asymmetrical folds over 5-20cm. Downhole, mm scalepartings of ca-chl-py are more common. Local 15-30cm biotitic dykes.

Sample

16473

16474164751647616477

164791648016481

16482164831648416486

From_m

86.00

87.9290.0093.0096.00

98.60100.00102.00

105.43108.00111.00114.00

To_m

87.92

90.0093.0096.0098.60

100.00102.00105.43

108.00111.00114.00115.04

Interval_m

1.92

2.083.003.002.60

1.402.003.43

2.573.003.001.04

Litho

GWK

IMCJIMCJIMCJIMCJ

IMJIMJIMJ

IMCJIMCJIMCJIMCJ

%SiO2

57.90

40.7039.2040.2044.40

37.4040.1538.75

44.7040.0042.3041.20

%Fe2O3

10.10

48.5050.7051.2038.20

54.6053.4555.30

42.6051.5048.9552.70

%TFe

7.07

33.9335.4735.8226.72

38.2037.3938.68

29.8036.0334.2436.87

%Mt

SAT

0.00

35.9047.3053.1037.05

38.6039.9545.00

41.5049.4049.1553.90

%Hm

CALC

0.00

0.110.000.000.00

13.9312.138.75

0.000.000.000.00

%FeMt

0.00

76.5791.51100.096.17

73.1377.3184.17

97.4798.6299.89100.0

%FeHm

0.00

0.220.000.000.00

25.5022.6915.83

0.000.000.000.00

%Fe

Other

100.00

23.218.490.003.83

1.370.000.00

2.531.380.110.00

CLAIM: KRL 3019666

Hole: ES08-010

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644263.98

Elevation (m):

541982.95

Depth (m): 417.8Logged By:

10/23/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

189.0

Page: 2 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -46.5

Start Date:

10/24/2008

Core Size : NQLogged Date: 11/15/2008

Diamond Drill Log

HOLE ID

ES08-010

ES08-010

ES08-010

ES08-010

From_m

115.04

118.05

135.00

153.00

To_m

118.05

135.00

153.00

166.27

Code

IFMS

IFM

IFML

IFML

Description

MAGNETITE-CHERT-GREY ARGILLITE: Alternating 0.5-10cm bands of med grey silty toargillaceous magnetite and pale to med grey chert bands with subcm chloritic partings.Banded at +45. From 116.70m, argillite is foliated at +55. From 115.62-116.15m: Qtz-biotiteschist at +40. From 117.00-117.53m: QP dyke with silica and patchy qtz-chl-ca and Kfeldsparoverprint, veinlets. Foliated at +45. 5cm qtz vein at lower contact.MAGNETITE-CHERT IRON FORMATION: Alternating 0.5-3cm bands of dk grey-black, siltyto argillaceous magnetite, minor specularite seams as mm laminae and 0.5-1cm bands ofmed grey-blue chert. Local chloritic partings +/- calcite, pyrite. Mostly well banded at +35to +45, with some folding over 10-50cm; axial planar cleavage at +55. Folds mostly plungesteeply to the west ; however some plunge shallowly W, as well. Trace to 0.5% pyrite as fgrdisseminations and in seams at band margins. Entire interval is cut by minor -45 to -50fractures. From 118.05-119.13m: Asymmetrical folds with axial plane at +53, plunging steeplywest. 1-2% late, cgr pyrite. From 121.05-128.92m: Sporadic 2-30cm sections of grey-brownbiotite-quartz-felspar dykes with calcite wisps, gashes. Dykes are parallel to banding and cutoff folds at 123.35m as well, but are also strongly foliated.MAGNETITE-CHERT > CHLORITE IRON FORMATION: Gradational from above. Moreargillaceous, fgr to vfgr magnetite bands (1-15cm), as mm scale laminae with chloriticpartings and pale to dk grey-blue chert bands (0.5-15cm). Progressive increase in proportionand thickness of bands of chloritic mudstone +/- magnetite, to 10cm. Moderate gruneritealong mt laminae. Banding is mostly straight, at +35 to +40, with local asymmetrical folds andcrenulations. Axial planar cleavage at +55, plunging steeply to the west. Interval is cut byminor -40 to -50 calcite +/- pyrite fractures.MAGNETITE-CHERT-CHLORITE with strong grunerite overprint: Rythmnically banded(0.5-1cm) fgr argillaceous dk grey-black magnetite and pale to med grey chert, (0.1-0.5cm)chlorite +/- mt bands. Well banded at +30, with strong, pale yellow, grunerite overprint.Interval is cut by minor -40 to -50 calcite +/- py fractures. From 158.00-159.13m QP dyke (?)

Sample

16487

164881648916490164911649216493

1649416495164971649816499165005801580258035805580658075808

From_m

115.04

118.05120.00123.00126.00129.00132.00

135.00138.00141.00144.00147.00148.00150.00153.00156.00159.35162.00165.00166.27

To_m

118.05

120.00123.00126.00129.00132.00135.00

138.00141.00144.00147.00148.00150.00153.00156.00159.35162.00165.00166.27168.00

Interval_m

3.01

1.953.003.003.003.003.00

3.003.003.003.001.002.003.003.003.352.653.001.271.73

Litho

IMCS

IMCIMCIMCIMCIMCIMC

IMCLIMCLIMCLIMCLIMCLIMCLIMCLIMCLRIMCLRIMCLRIMCLRIMCLRARG

%SiO2

51.20

41.5042.7041.6042.7045.1040.70

42.7040.9044.2041.1043.5044.8042.8045.8052.4045.6347.0054.3060.90

%Fe2O3

27.60

54.7051.7049.8046.9049.8052.30

51.1050.0044.0049.8049.1047.6049.9042.4032.7042.6739.8028.709.54

%TFe

19.31

38.2736.1734.8432.8134.8436.59

35.7534.9830.7834.8434.3533.3034.9129.6622.8829.8527.8420.086.67

%Mt

SAT

23.90

54.1051.6048.0045.0049.5052.30

48.3036.9030.5040.0039.7036.4037.7030.4019.0029.0016.700.330.90

%Hm

CALC

0.00

0.000.000.000.000.000.00

0.000.000.000.000.000.000.000.000.000.000.091.660.26

%FeMt

87.90

98.7899.5399.4197.5298.9798.70

94.2575.3171.2281.2880.8477.8177.0272.8160.1069.0343.401.199.76

%FeHm

0.00

0.000.000.000.000.000.00

0.000.000.000.000.000.000.000.000.000.000.235.782.76

%Fe

Other

12.10

1.220.470.592.481.031.30

5.7524.6928.7818.7219.1622.1922.9827.1939.9030.9756.3693.0387.48

Hole: ES08-010

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644263.98

Elevation (m):

541982.95

Depth (m): 417.8Logged By:

10/23/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

189.0

Page: 3 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 360

Dip : -46.5

Start Date:

10/24/2008

Core Size : NQLogged Date: 11/15/2008

Diamond Drill Log

HOLE ID

ES08-010

From_m

166.27

To_m

189.00

Code

ARG

Description

GREY ARGILLITE (KNOTTED PHYLLITE): Med grey, vgr, well laminated and/or tectonicallybanded at +30 to +40. To 173m, some cm to m scale interbeds of greywacke, siltstone. Wklyto moderately carbonaceous. Becomes serictic downhole, with increased strain. From175-180m, cut by -60 fractures. From 172.65m: Argillite is more strained, hosts localdismembered, boudinaged subcm veins of qtz-ca +/- py, po. Vfgr garnet grains to 174m.Common fine euhedral amphibole grains which are locally aligned along cleavage at +32.From 184m: 20% cm scale porphyroblasts within knotted phyllite. Unit also iscarbonaceous. Common 1-2% pyrrhotite throughout, as mm seams, increasing in abundancedowhole.

Sample From_m To_m Interval_m Litho %

SiO2%

Fe2O3%

TFe%Mt

SAT

%Hm

CALC%

FeMt%

FeHm%Fe

Other

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-010 0.00 6.00 6.00 0.00 0.00% #DIV/0! NQ JT / JF NOV 16 / 08ES08-010 6.00 9.00 3.00 2.85 95.00% 1.10 38.60% NQ JT / JF NOV 16 / 08ES08-010 9.00 12.00 3.00 3.00 100.00% 2.74 91.33% NQ JT / JF NOV 16 / 08ES08-010 12.00 15.00 3.00 3.00 100.00% 1.65 55.00% NQ JT / JF NOV 16 / 08ES08-010 15.00 18.00 3.00 2.89 96.33% 2.67 92.39% NQ JT / JF NOV 16 / 08ES08-010 18.00 21.00 3.00 3.13 104.33% 2.45 78.27% NQ JT / JF NOV 16 / 08ES08-010 21.00 24.00 3.00 2.98 99.33% 2.74 91.95% NQ JT / JF NOV 16 / 08ES08-010 24.00 27.00 3.00 3.00 100.00% 3.00 100.00% NQ JT / JF NOV 16 / 08ES08-010 27.00 30.00 3.00 3.02 100.67% 2.53 83.77% NQ JT / JF NOV 16 / 08ES08-010 30.00 33.00 3.00 2.98 99.33% 1.69 56.71% NQ JT / JF NOV 16 / 08ES08-010 33.00 36.00 3.00 3.00 100.00% 2.33 77.67% NQ JT / JF NOV 16 / 08ES08-010 36.00 39.00 3.00 2.94 98.00% 2.03 69.05% NQ JT / JF NOV 16 / 08ES08-010 39.00 42.00 3.00 3.02 100.67% 2.22 73.51% NQ JT / JF NOV 16 / 08ES08-010 42.00 45.00 3.00 2.89 96.33% 2.04 70.59% NQ JT / JF NOV 16 / 08ES08-010 45.00 48.00 3.00 3.06 102.00% 2.68 87.58% NQ JT / JF NOV 16 / 08ES08-010 48.00 51.00 3.00 3.00 100.00% 2.25 75.00% NQ JT / JF NOV 16 / 08ES08-010 51.00 54.00 3.00 2.84 94.67% 1.84 64.79% NQ JT / JF NOV 16 / 08ES08-010 54.00 57.00 3.00 2.94 98.00% 1.93 65.65% NQ JT NOV 16 / 08ES08-010 57.00 60.00 3.00 3.00 100.00% 2.42 80.67% NQ JT NOV 16 / 08ES08-010 60.00 63.00 3.00 3.00 100.00% 1.25 41.67% NQ JT NOV 16 / 08ES08-010 63.00 66.00 3.00 3.00 100.00% 2.04 68.00% NQ JT NOV 16 / 08ES08-010 66.00 69.00 3.00 2.90 96.67% 1.96 67.59% NQ JT NOV 16 / 08ES08-010 69.00 72.00 3.00 2.90 96.67% 1.63 56.21% NQ JT NOV 16 / 08ES08-010 72.00 75.00 3.00 2.95 98.33% 1.50 50.85% NQ JT NOV 16 / 08ES08-010 75.00 78.00 3.00 2.94 98.00% 2.38 80.95% NQ JT NOV 16 / 08ES08-010 78.00 81.00 3.00 2.96 98.67% 2.68 90.54% NQ JT NOV 16 / 08ES08-010 81.00 84.00 3.00 3.00 100.00% 2.34 78.00% NQ JT NOV 16 / 08ES08-010 84.00 87.00 3.00 3.00 100.00% 2.22 74.00% NQ JT NOV 16 / 08ES08-010 87.00 90.00 3.00 2.96 98.67% 2.09 70.61% NQ JT NOV 16 / 08ES08-010 90.00 93.00 3.00 3.00 100.00% 2.34 78.00% NQ JT NOV 16 / 08ES08-010 93.00 96.00 3.00 2.90 96.67% 2.09 72.07% NQ JT NOV 16 / 08ES08-010 96.00 99.00 3.00 3.03 101.00% 2.86 94.39% NQ JT NOV 16 / 08ES08-010 99.00 102.00 3.00 2.97 99.00% 2.18 73.40% NQ JT NOV 16 / 08

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-010 102.00 105.00 3.00 2.86 95.33% 1.42 49.65% NQ JT NOV 16 / 08ES08-010 105.00 108.00 3.00 3.09 103.00% 2.34 75.73% NQ JT NOV 16 / 08ES08-010 108.00 111.00 3.00 3.00 100.00% 2.25 75.00% NQ JT NOV 16 / 08ES08-010 111.00 114.00 3.00 3.00 100.00% 2.73 91.00% NQ JT NOV 16 / 08ES08-010 114.00 117.00 3.00 2.95 98.33% 2.82 95.59% NQ JT NOV 16 / 08ES08-010 117.00 120.00 3.00 3.00 100.00% 2.75 91.67% NQ JT NOV 16 / 08ES08-010 120.00 123.00 3.00 2.94 98.00% 2.84 96.60% NQ JT NOV 16 / 08ES08-010 123.00 126.00 3.00 2.97 99.00% 2.72 91.58% NQ JT NOV 16 / 08ES08-010 126.00 129.00 3.00 3.00 100.00% 2.80 93.33% NQ JT NOV 16 / 08ES08-010 129.00 132.00 3.00 3.00 100.00% 2.83 94.33% NQ JT NOV 16 / 08ES08-010 132.00 135.00 3.00 3.00 100.00% 2.34 78.00% NQ JT NOV 16 / 08ES08-010 135.00 138.00 3.00 3.00 100.00% 3.00 100.00% NQ JT NOV 16 / 08ES08-010 138.00 141.00 3.00 3.00 100.00% 2.55 85.00% NQ JT NOV 16 / 08ES08-010 141.00 144.00 3.00 3.00 100.00% 2.29 76.33% NQ JT NOV 16 / 08ES08-010 144.00 147.00 3.00 2.95 98.33% 2.58 87.46% NQ JT NOV 16 / 08ES08-010 147.00 150.00 3.00 2.97 99.00% 2.71 91.25% NQ JT NOV 16 / 08ES08-010 150.00 153.00 3.00 3.00 100.00% 2.61 87.00% NQ JT NOV 17 / 08ES08-010 153.00 156.00 3.00 3.00 100.00% 2.91 97.00% NQ JT NOV 17 / 08ES08-010 156.00 159.00 3.00 2.93 97.67% 2.73 93.17% NQ JT NOV 17 / 08ES08-010 159.00 162.00 3.00 3.00 100.00% 2.74 91.33% NQ JT NOV 17 / 08ES08-010 162.00 165.00 3.00 3.00 100.00% 2.83 94.33% NQ JT NOV 17 / 08ES08-010 165.00 168.00 3.00 2.94 98.00% 2.79 94.90% NQ JT NOV 17 / 08ES08-010 168.00 171.00 3.00 3.00 100.00% 2.48 82.67% NQ JT NOV 17 / 08ES08-010 171.00 174.00 3.00 2.96 98.67% 2.62 88.51% NQ JT NOV 17 / 08ES08-010 174.00 177.00 3.00 2.97 99.00% 2.89 97.31% NQ JT NOV 17 / 08ES08-010 177.00 180.00 3.00 2.94 98.00% 1.98 67.35% NQ JT NOV 17 / 08ES08-010 180.00 183.00 3.00 2.96 98.67% 2.44 82.43% NQ JT NOV 17 / 08ES08-010 183.00 186.00 3.00 3.00 100.00% 2.59 86.33% NQ JT NOV 17 / 08ES08-010 186.00 189.00 3.00 2.93 97.67% 2.48 84.64% NQ JT NOV 17 / 08 E.O.H.

Hole: ES08-011

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644265.62

Elevation (m):

540810

Depth (m): 429.2Logged By:

10/25/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

186.0

Page: 1 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 180

Dip : -46.0

Start Date:

10/26/2008

Core Size : NQLogged Date: 11/16/2008

Diamond Drill Log

HOLE ID

ES08-011ES08-011ES08-011

ES08-011

ES08-011

ES08-011

From_m

0.001.111.95

14.40

63.00

79.50

To_m

1.111.9514.40

63.00

79.50

95.00

Code

CASOVERCONG

GWK

GWK

GWK

Description

CASING: Casing pulled, anchor remains.OVERBURDEN:CONGLOMERATE: Fgr, silty to sandy grey-brown matrix with subcm to 15cm thick pale greysiliceous fragments. Clasts have sharp to ragged and diffuse margins; subrounded toelongate parallel to mod-strong cleavage at +50 to +60. Clasts show poor size sorting andare elongate at 3:1 to 6:1 aspect ratios. Both matrix and clasts overprinted by 1-3mmsubhedral grains of chloritized mafics. Core is moderately blocky to 7m. Entire interval isbroken along -40 to -60, and +80 to +60 fractures with water stains.BIOTITIC WACKE with Kspar overprint: Med grey-brown, silty to sandy; massive with minorbedding, foliation at +45. Cut by minor bleached fracture nets of calcite +/- kfeldspar at -55.Water stains to 18m. From 24.80m: diffuse, patchy infiltrations and fracture halos of mgrequigranular diorite and pale y-green patches of kfeldspar +/- epidote +/- calcite. From39.00m: unit is more mottled, diorite and gneissic textured (pseudo conglomerate?) Waterstained fractures continue to 35m.GREYWACKE: Pale grey, massive, with biotite, chlorite as fine grains, wisps parallel to modfoliation at +45. Some poorly sorted (size) conglomerate section with pale grey-white sandyclasts in an equivalent finer grained matrix with biotite. Some diffuse silica overprint impartsa cloudy grey colouration. Interval is cut by minor whit subcm calcite vnlts along foliation.From 71.30-74.15m: Sections of diffuse Kfeldspar – epidote +/- calcite flooding over 5-30cmintervals. Minor calcite fractures at +45.GREYWACKE: Med grey, massive greywacke overprinted by diffuse patches of pale to medgrey-blue silica patches and sections of mgr, foliated (+25) diorite from 88.10-89.95m,92.37-93.10m. Diorite has sharp contacts, which are ragged where overprinted by cleavage.From 88.50-92.30m, unit appears bleached to silicified, to cloudy grey “QP” phase. The QP,quartz porphyry section is overprinted by a net of mostly foliation parallel yellowkfeldspar-epidote +/- calcite flooding. Dioritic section are not overprinted by this, andtherefore may be later. Entire interval is cut by +25 and +40 calcitic fractures and minor +80calcite +/- chlorite fractures.

Sample From_m To_m Interval_m Litho %

SiO2%

Fe2O3%

TFe%Mt

SAT

%Hm

CALC%

FeMt%

FeHm%Fe

Other

CLAIM: KRL 3019665

Hole: ES08-011

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644265.62

Elevation (m):

540810

Depth (m): 429.2Logged By:

10/25/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

186.0

Page: 2 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 180

Dip : -46.0

Start Date:

10/26/2008

Core Size : NQLogged Date: 11/16/2008

Diamond Drill Log

HOLE ID

ES08-011

ES08-011

ES08-011

ES08-011

ES08-011

ES08-011

From_m

95.00

100.68

107.73

130.35

138.62

140.84

To_m

100.68

107.73

130.35

138.62

140.84

147.00

Code

ARG

IFML

GWK

IFMJ

QP

IFMJ

Description

GREY ARGILLITE to QTZ-SER-CHL-PO SCHIST: Pale grey-green , finely laminatedgreywacke; highly strained to quartz-sericite-chlorite +/- garnet schist at +55. Some relictchert bands as discontinuous boudins. 0.5-1% pyrrhotite along schistosity, within qtz boudinsand in minor cm scale veins of grey qtz +/- tourmaline. Unit is NOT carbonaceous. From99.50m: Argillite is intercalated with chlorite-garnet and pael grey chert bands; boudinagedand dismembered. Interval is intensely fracture and cut by qtz-tourmaline brecciasoverprinted by a fine net of pale yellow kspar-carbonate-epidote fracture halos. Mod grunerite.CHERT-MAGNETITE-CHLORITE-GARNET IRON FORMATION: Ragged, discontinuous0.2-1cm bands of med grey-blue chert and wisps, laminae of dk grey-black magnetite with1-2cm bands of dk green chlorite-mt +/- garnet bands. Mod-strong grunerite margins tomagnete. Common 1-2% mm scale foliation parallel seams of py +/- po at +55 to +50, alsoalong local shear zones at +70. Interval is cut by minor -35 to -50 fractures. From 105m,increased chlorite-garnet bands (5-15cm). A strong grunerite overprint imparts a raggedappearance to the bands.BIOTITE WACKE to GREY ARGILLITE: Upper metre is strongly foliated to mylonitebiotite-quartz schist with minor, subcm chlorite +/- garnet bands. Grades downhole into medto pale grey argillite and wacke laminae (mm to cm) at +60. Interval is cut by minor -40 and-60 calcite +/- py fractures. Blocky core from 123-124.50m.MAGNETITE-CHERT-JASPER IRON FORMATION with Specularite: Well banded, 0.5-3cmbands of dk grey-black argillaceous magnetite with med grey-blue chert. From 135m, chertgrades into a wk –mod jasper and magnetite with fgr specularite. Banding is straight, at +50but dragged to +75 at upper contact with argillite. Grunerite also at upper contact. Interval iscut by -40 to -50 calcite +/- py fractures.QUARTZ PORPHYRY: Pale grey-white, mgr with fine chill margins. Contacts are sharp andparallel to banding at +55. Mod foliated at +50. From 139.88-140.58m: section of magnetiteand wt chert with marginal pyrite.MAGNETITE-CHERT-JASPER with specularite: As for interval 130.35-138.62m. Wellbanded at +55, with local cm scale asymmetrical folding at +60 to +65. Cut by -40 to -50fractures of calcite –chlorite +/- pyrite fractures and minor -60 to -70 fractures from 144.50m.

Sample

58095810

581158125813

58145815

5816581758195820

5821

58225823

From_m

96.0099.00

100.68102.00105.00

107.73129.00

130.35132.00135.00136.10

138.62

140.84144.00

To_m

99.00100.68

102.00105.00107.73

111.00130.35

132.00135.00136.10138.62

140.84

144.00147.00

Interval_m

3.001.68

1.323.002.73

3.271.35

1.653.001.102.52

2.22

3.163.00

Litho

ARGARG

ICMLgtICMLgtICMLgt

BWKBWK

IMCJIMCJIMCJIMCJ

QP

IMCJIMCJ

%SiO2

60.8058.30

48.4047.6051.10

60.9060.50

40.8042.3041.9039.10

57.50

40.9040.60

%Fe2O3

9.3611.90

36.3038.6035.30

10.9012.50

50.5051.8052.9056.00

20.90

53.2051.90

%TFe

6.558.32

25.3927.0024.69

7.638.74

35.3336.2437.0139.17

14.62

37.2236.31

%Mt

SAT0.400.70

25.4023.1016.20

0.700.65

34.2047.2552.2042.00

18.30

45.5043.40

%Hm

CALC0.540.39

0.000.190.99

0.541.02

0.000.000.0012.09

0.08

5.576.59

%FeMt

4.426.08

71.6261.9047.47

6.645.38

69.4891.8098.1077.58

90.57

88.4786.50

%FeHm

5.763.31

0.000.502.82

4.948.14

0.000.000.0021.59

0.38

10.4612.70

%Fe

Other89.8290.60

28.3837.6049.71

88.4186.48

30.528.201.900.83

9.05

1.070.80

Hole: ES08-011

Property: EL SOL

Target: A Zone

Northing (m):

Easting (m):

5644265.62

Elevation (m):

540810

Depth (m): 429.2Logged By:

10/25/2008

Drilled By: Hy-Tec Drilling Ltd.

J. Fingler

End Date:

186.0

Page: 3 of 3

RAYTEC METALS CORP.Datum : UTM83Z15E

Azimuth: 180

Dip : -46.0

Start Date:

10/26/2008

Core Size : NQLogged Date: 11/16/2008

Diamond Drill Log

HOLE ID

ES08-011

ES08-011

ES08-011

From_m

147.00

149.70

156.00

To_m

149.70

156.00

186.00

Code

IFL

ARG

GWK

Description

CHLORITE-GARNET-CHERT-MAGNETITE IRON FORMATION: Gradational from above,with less magnetite and more chloritic mudstone bands. Latter bands become thickerdownhole, from 0.5 to 5cm. Well banded at +60 to +50, with local axial planar cleavage to dmscale folds is at +45, oblique to banding. Some moderate grunerite development in uppermetre. Interval is cut by dm spaced -50 calcite +/- py, chl fractures.GREY ARGILLITE/SILTSTONE: Med grey, with patchy, pale grey section; wklylaminated/cleaved at +50; wkly carbonaceous. Downhole, unit becomes coarser, lesscarbonaceous and more sericitic. Minor subcm vnlts and boudins fo qtz-carbonate-chlorite +/-pyrrhotite are parallel to banding.BIOTITIC WACKE: Pale –med grey brown unit, mostly massive with +50 to +60 dm beds.Appears to grade into some qtz eye bearing intervals (tuffaceous?).Minor dm scaleargillaceous interbeds. Wk-mod foliated. From 183.35-184.35m: Possible QP dyke, withsharp upper contact at +60, parallel to foliation.

Sample

5824

5825

From_m

147.00

149.70

To_m

149.70

153.00

Interval_m

2.70

3.30

Litho

ILCMgt

ARG

%SiO2

52.70

59.30

%Fe2O3

29.50

7.19

%TFe

20.64

5.03

%Mt

SAT11.80

1.50

%Hm

CALC2.57

0.58

%FeMt

41.38

21.58

%FeHm

8.72

8.03

%Fe

Other49.90

70.39

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-011 1.95 3.00 1.05 1.05 100.00% 0.74 70.48% NQ JT NOV 4 / 08ES08-011 3.00 6.00 3.00 2.72 90.67% 0.78 28.68% NQ JT NOV 4 / 08 Broken and blockyES08-011 6.00 9.00 3.00 2.90 96.67% 1.80 62.07% NQ JT NOV 4 / 08 49cm Broken and blockyES08-011 9.00 12.00 3.00 2.75 91.67% 1.37 49.82% NQ JT NOV 4 / 08 Broken and blockyES08-011 12.00 15.00 3.00 3.00 100.00% 1.52 50.67% NQ JT NOV 4 / 08ES08-011 15.00 18.00 3.00 2.93 97.67% 1.82 62.12% NQ JT NOV 4 / 08ES08-011 18.00 21.00 3.00 3.00 100.00% 2.12 70.67% NQ JT NOV 4 / 08ES08-011 21.00 24.00 3.00 2.90 96.67% 1.90 65.52% NQ JT NOV 4 / 08ES08-011 24.00 27.00 3.00 2.92 97.33% 2.03 69.52% NQ JT NOV 4 / 08ES08-011 27.00 30.00 3.00 2.94 98.00% 1.47 50.00% NQ JT NOV 4 / 08ES08-011 30.00 33.00 3.00 2.94 98.00% 1.88 63.95% NQ JT NOV 4 / 08ES08-011 33.00 36.00 3.00 2.87 95.67% 2.00 69.69% NQ JT NOV 4 / 08ES08-011 36.00 39.00 3.00 3.00 100.00% 1.92 64.00% NQ JT NOV 4 / 08ES08-011 39.00 42.00 3.00 3.00 100.00% 2.43 81.00% NQ JT NOV 4 / 08ES08-011 42.00 45.00 3.00 2.94 98.00% 1.28 43.54% NQ JT NOV 4 / 08ES08-011 45.00 48.00 3.00 2.93 97.67% 1.65 56.31% NQ JT NOV 4 / 08ES08-011 48.00 51.00 3.00 2.93 97.67% 1.93 65.87% NQ JT NOV 4 / 08ES08-011 51.00 54.00 3.00 2.96 98.67% 2.53 85.47% NQ JT NOV 4 / 08ES08-011 54.00 57.00 3.00 2.98 99.33% 2.54 85.23% NQ JT NOV 4 / 08ES08-011 57.00 60.00 3.00 2.94 98.00% 2.77 94.22% NQ JT NOV 4 / 08ES08-011 60.00 63.00 3.00 2.97 99.00% 2.70 90.91% NQ JT NOV 4 / 08ES08-011 63.00 66.00 3.00 3.07 102.33% 2.10 68.40% NQ JT NOV 4 / 08ES08-011 66.00 69.00 3.00 2.95 98.33% 1.71 57.97% NQ JT NOV 4 / 08ES08-011 69.00 72.00 3.00 3.00 100.00% 2.06 68.67% NQ JT NOV 4 / 08ES08-011 72.00 75.00 3.00 2.88 96.00% 1.83 63.54% NQ JT NOV 4 / 08ES08-011 75.00 78.00 3.00 3.00 100.00% 2.50 83.33% NQ JT NOV 4 / 08ES08-011 78.00 81.00 3.00 2.92 97.33% 1.79 61.30% NQ JT NOV 4 / 08ES08-011 81.00 84.00 3.00 2.97 99.00% 1.96 65.99% NQ JT NOV 4 / 08ES08-011 84.00 87.00 3.00 2.94 98.00% 1.47 50.00% NQ JT NOV 4 / 08ES08-011 87.00 90.00 3.00 2.97 99.00% 2.52 84.85% NQ JT NOV 4 / 08ES08-011 90.00 93.00 3.00 2.92 97.33% 1.68 57.53% NQ JT NOV 4 / 08ES08-011 93.00 96.00 3.00 3.00 100.00% 2.30 76.67% NQ JT NOV 4 / 08ES08-011 96.00 99.00 3.00 2.87 95.67% 2.07 72.13% NQ JT NOV 4 / 08

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

ES08-0

10

CASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASOVER

OVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVER

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.935.9

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.535.5

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.0

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.347.353.1

53.153.153.153.153.153.1

53.153.153.153.153.153.153.1

53.153.153.153.153.153.153.1

53.153.153.153.153.153.1

53.153.153.153.153.153.153.1

53.153.153.153.153.153.153.1

53.153.153.153.153.153.153.153.137.1

37.137.137.137.137.137.1

37.137.137.137.137.137.137.1

37.137.137.137.137.137.137.1

37.137.137.137.137.137.1

37.137.137.137.137.137.137.1

37.137.137.137.137.137.137.1

37.137.137.137.137.137.137.137.1

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.933.9

7.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.17.1

35.835.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.835.835.826.7

26.726.726.726.726.726.7

26.726.726.726.726.726.726.7

26.726.726.726.726.726.726.7

26.726.726.726.726.726.7

26.726.726.726.726.726.726.7

26.726.726.726.726.726.726.7

26.726.726.726.726.726.726.726.738.2

38.238.238.238.238.238.2

38.238.238.238.238.238.238.2

38.238.238.238.238.238.238.2

38.238.238.238.238.238.2

38.238.238.238.238.238.238.2

38.238.238.238.238.238.238.2

38.238.238.238.238.238.238.238.2

38.638.638.638.638.638.638.6

38.638.638.638.638.638.638.6

38.638.638.638.638.638.638.6

38.638.638.638.638.638.6

38.638.638.638.638.638.638.6

38.638.638.638.638.638.638.6

38.638.638.638.638.638.638.638.640.040.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.040.040.045.0

45.045.045.045.045.045.0

45.045.045.045.045.045.045.0

45.045.045.045.045.045.045.0

45.045.045.045.045.045.0

45.045.045.045.045.045.045.0

45.045.045.045.045.045.045.0

45.045.045.045.045.045.045.045.0

16473164731647316473164731647316473

16473164731647316473164731647316473

16473164731647316473164731647316473

164731647316473164731647316473

16473164731647316473164731647316473

16473164731647316473164731647316473

16473164731647316473164731647316473

16473

16474164741647416474164741647416474

16474164741647416474164741647416474

16474164741647416474164741647416474

164741647416474164741647416474

16474164741647416474164741647416474

16474164741647416474164741647416474

16474164741647416474164741647416474

16474

16475164751647516475164751647516475

16475164751647516475164751647516475

16475164751647516475164751647516475

164751647516475164751647516475

16475164751647516475164751647516475

16475164751647516475164751647516475

16475164751647516475164751647516475

1647537.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.437.438.7

38.738.738.738.738.738.7

38.738.738.738.738.738.738.7

38.738.738.738.738.738.738.7

38.738.738.738.738.738.7

38.738.738.738.738.738.738.7

38.738.738.738.738.738.738.7

38.738.738.738.738.738.738.738.7

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.541.5

16477164771647716477164771647716477

16477164771647716477164771647716477

16477164771647716477164771647716477

164771647716477164771647716477

16477164771647716477164771647716477

16477164771647716477164771647716477

16477164771647716477164771647716477

16477

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16476164761647616476164761647616476

16476164761647616476164761647616476

16476164761647616476164761647616476

164761647616476164761647616476

16476164761647616476164761647616476

16476164761647616476164761647616476

16476164761647616476164761647616476

1647616479164791647916479164791647916479

16479164791647916479164791647916479

16479164791647916479164791647916479

164791647916479164791647916479

16479164791647916479164791647916479

16479164791647916479164791647916479

16479164791647916479164791647916479

16479

16480164801648016480164801648016480

16480164801648016480164801648016480

16480164801648016480164801648016480

164801648016480164801648016480

16480164801648016480164801648016480

16480164801648016480164801648016480

16480164801648016480164801648016480

1648053.953.953.953.953.953.953.9

53.953.953.953.953.953.953.9

53.953.953.953.953.953.953.9

53.953.953.953.953.953.9

53.953.953.953.953.953.953.9

53.953.953.953.953.953.953.9

53.953.953.953.953.953.953.953.9

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.829.836.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.036.0

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.449.449.1

49.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.149.1

36.936.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.936.936.9

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.234.219.3

19.319.319.319.319.319.3

19.319.319.319.319.319.319.3

19.319.319.319.319.319.319.3

19.319.319.319.319.319.3

19.319.319.319.319.319.319.3

19.319.319.319.319.319.319.3

19.319.319.319.319.319.319.319.338.3

38.338.338.338.338.338.3

38.338.338.338.338.338.338.3

38.338.338.338.338.338.338.3

38.338.338.338.338.338.3

38.338.338.338.338.338.338.3

38.338.338.338.338.338.338.3

38.338.338.338.338.338.338.338.3

48.048.048.048.048.048.048.0

48.048.048.048.048.048.048.0

48.048.048.048.048.048.048.0

48.048.048.048.048.048.0

48.048.048.048.048.048.048.0

48.048.048.048.048.048.048.0

48.048.048.048.048.048.048.048.0

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.923.954.1

54.154.154.154.154.154.1

54.154.154.154.154.154.154.1

54.154.154.154.154.154.154.1

54.154.154.154.154.154.1

54.154.154.154.154.154.154.1

54.154.154.154.154.154.154.1

54.154.154.154.154.154.154.154.151.6

51.651.651.651.651.651.6

51.651.651.651.651.651.651.6

51.651.651.651.651.651.651.6

51.651.651.651.651.651.6

51.651.651.651.651.651.651.6

51.651.651.651.651.651.651.6

51.651.651.651.651.651.651.651.6

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16481164811648116481164811648116481

16481164811648116481164811648116481

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16481164811648116481164811648116481

16481164811648116481164811648116481

16481164811648116481164811648116481

16481

16482164821648216482164821648216482

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16482164821648216482164821648216482

16482

16483164831648316483164831648316483

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16483164831648316483164831648316483

16483164831648316483164831648316483

16483

16484164841648416484164841648416484

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16484

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16486

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16487

16488164881648816488164881648816488

16488164881648816488164881648816488

16488164881648816488164881648816488

164881648816488164881648816488

16488164881648816488164881648816488

16488164881648816488164881648816488

16488164881648816488164881648816488

16488

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.236.2

52.352.352.352.352.352.352.3

52.352.352.352.352.352.352.3

52.352.352.352.352.352.352.3

52.352.352.352.352.352.3

52.352.352.352.352.352.352.3

52.352.352.352.352.352.352.3

52.352.352.352.352.352.352.352.3

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.832.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.8

45.045.045.045.045.045.045.0

45.045.045.045.045.045.045.0

45.045.045.045.045.045.045.0

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45.045.045.045.045.045.045.0

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45.045.045.045.045.045.045.045.049.5

49.549.549.549.549.549.5

49.549.549.549.549.549.549.5

49.549.549.549.549.549.549.5

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49.549.549.549.549.549.549.549.5

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.636.6

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.8

35.735.735.735.735.735.735.7

35.735.735.735.735.735.735.7

35.735.735.735.735.735.735.7

35.735.735.735.735.735.7

35.735.735.735.735.735.735.7

35.735.735.735.735.735.735.7

35.735.735.735.735.735.735.735.7

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16489164891648916489164891648916489

16489

16490164901649016490164901649016490

16490164901649016490164901649016490

16490164901649016490164901649016490

164901649016490164901649016490

16490164901649016490164901649016490

16490164901649016490164901649016490

16490164901649016490164901649016490

16490

16491164911649116491164911649116491

16491164911649116491164911649116491

16491164911649116491164911649116491

164911649116491164911649116491

16491164911649116491164911649116491

16491164911649116491164911649116491

16491164911649116491164911649116491

16491

16492164921649216492164921649216492

16492164921649216492164921649216492

16492164921649216492164921649216492

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16492164921649216492164921649216492

16492164921649216492164921649216492

16492

16493164931649316493164931649316493

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16493164931649316493164931649316493

164931649316493164931649316493

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16493164931649316493164931649316493

16493164931649316493164931649316493

1649335.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.035.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.040.0

40.040.040.040.040.040.040.040.0

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.348.336.9

36.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.936.9

36.936.936.936.936.936.936.936.930.5

30.530.530.530.530.530.5

30.530.530.530.530.530.530.5

30.530.530.530.530.530.530.5

30.530.530.530.530.530.5

30.530.530.530.530.530.530.5

30.530.530.530.530.530.530.5

30.530.530.530.530.530.530.530.5

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.830.8

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.334.334.9

34.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.934.9

33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.333.3 39.7

39.739.739.739.739.739.7

39.739.739.739.739.739.739.7

39.739.739.739.739.739.739.7

39.739.739.739.739.739.7

39.739.739.739.739.739.739.7

39.739.739.739.739.739.739.7

39.739.739.739.739.739.739.739.7

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.436.437.7

37.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.737.737.730.4

30.430.430.430.430.430.4

30.430.430.430.430.430.430.4

30.430.430.430.430.430.430.4

30.430.430.430.430.430.4

30.430.430.430.430.430.430.4

30.430.430.430.430.430.430.4

30.430.430.430.430.430.430.430.4

IFML

IFML

IFML

IFML

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16494164941649416494164941649416494

16494164941649416494164941649416494

164941649416494164941649416494

16494164941649416494164941649416494

16494164941649416494164941649416494

16494164941649416494164941649416494

16494

16495164951649516495164951649516495

16495164951649516495164951649516495

16495164951649516495164951649516495

164951649516495164951649516495

16495164951649516495164951649516495

16495164951649516495164951649516495

16495164951649516495164951649516495

16495

16497164971649716497164971649716497

16497164971649716497164971649716497

16497164971649716497164971649716497

164971649716497164971649716497

16497164971649716497164971649716497

16497164971649716497164971649716497

16497164971649716497164971649716497

16497

16498164981649816498164981649816498

16498164981649816498164981649816498

16498164981649816498164981649816498

164981649816498164981649816498

16498164981649816498164981649816498

16498164981649816498164981649816498

16498164981649816498164981649816498

16498

16499164991649916499164991649916499

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16499164991649916499164991649916499

16499164991649916499164991649916499

16499

16500165001650016500165001650016500

16500165001650016500165001650016500

16500165001650016500165001650016500

165001650016500165001650016500

16500165001650016500165001650016500

16500165001650016500165001650016500

16500165001650016500165001650016500

16500

5801580158015801580158015801

5801580158015801580158015801

5801580158015801580158015801

580158015801580158015801

5801580158015801580158015801

5801580158015801580158015801

58015801580158015801580158015801

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

IFMS

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.729.722.9

22.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.922.922.9

19.019.019.019.019.019.019.0

19.019.019.019.019.019.019.0

19.019.019.019.019.019.019.0

19.019.019.019.019.019.0

19.019.019.019.019.019.019.0

19.019.019.019.019.019.019.0

19.019.019.019.019.019.019.019.029.0

29.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.029.029.016.7

16.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.716.716.70.30.30.30.30.30.30.3

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.90.9

20.120.120.120.120.120.120.1

20.120.120.120.120.120.120.1

20.120.120.120.120.120.120.1

20.120.120.120.120.120.1

20.120.120.120.120.120.120.1

20.120.120.120.120.120.120.1

20.120.120.120.120.120.120.120.1

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.829.827.8

27.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.827.86.76.76.76.76.76.76.7

6.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.76.7

IFML

IFML

IFML

IFML

IFML

IFML

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IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

5802580258025802580258025802

5802580258025802580258025802

5802580258025802580258025802

580258025802580258025802

5802580258025802580258025802

5802580258025802580258025802

580258025802580258025802580258025803

580358035803580358035803

5803580358035803580358035803

5803580358035803580358035803

580358035803580358035803

5803580358035803580358035803

5803580358035803580358035803

580358035803580358035803580358035805

580558055805580558055805

5805580558055805580558055805

5805580558055805580558055805

580558055805580558055805

5805580558055805580558055805

5805580558055805580558055805

580558055805580558055805580558055806

580658065806580658065806

5806580658065806580658065806

5806580658065806580658065806

580658065806580658065806

5806580658065806580658065806

5806580658065806580658065806

58065806580658065806580658065806

5807580758075807580758075807

5807580758075807580758075807

5807580758075807580758075807

580758075807580758075807

5807580758075807580758075807

5807580758075807580758075807

58075807580758075807580758075807

5808580858085808580858085808

5808580858085808580858085808

5808580858085808580858085808

580858085808580858085808

5808580858085808580858085808

5808580858085808580858085808

58085808580858085808580858085808ARG

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m

50m E

lev

5,644,150mN

5,644,150mN

5,644,050mN

250m E

lev 150m

Elev

5,644,250mN

5,644,350mN

5,644,350mN

5,644,250mN 5,644,450mN 5,644,550mN

5,644,550mN

350

m E

lev

350m E

lev 4

50m

Ele

v 450m

Elev

5,644,450mN

50m

Ele

v 1

50m

Ele

v 2

50m

Ele

v

5,644,650mN

5,644,650mN

Scale 1:1,000Section Origin (top left)541,982.95 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

�

ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m189m ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010ES08-010

Raytec Metals Corp.

El Sol ProjectA Zone

Section E541982

0 25

metres

50

Scale: 1:1000

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

IFMJ

IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

Quartz Porphyry

Granitic Dyke

Biotite dyke

GD

QP

CASCasing

OVEROverburden

BD

Legend

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

24

ES56-0

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ES56-0

24

ES56-0

24

ES56-0

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ES56-0

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ES56-0

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ES56-0

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ES56-0

24

ES56-0

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ES56-0

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ES56-0

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ES56-0

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ES56-0

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ES56-0

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ES56-0

24

ES56-0

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ES56-0

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ES56-0

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ES56-0

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ES56-0

24

ES56-0

24

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

IFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFL

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

30.130.130.130.130.130.130.1

30.130.130.130.130.130.130.1

30.130.130.130.130.130.130.1

30.130.130.130.130.130.1

30.130.130.130.130.130.130.1

30.130.130.130.130.130.130.1

30.130.130.130.130.130.130.130.133.2

33.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.233.233.0

33.033.033.033.033.033.0

33.033.033.033.033.033.033.0

33.033.033.033.033.033.033.0

33.033.033.033.033.033.0

33.033.033.033.033.033.033.0

33.033.033.033.033.033.033.0

33.033.033.033.033.033.033.033.030.8

30.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.830.8

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.634.6

31.831.831.831.831.831.831.8

31.831.831.831.831.831.831.8

31.831.831.831.831.831.831.8

31.831.831.831.831.831.8

31.831.831.831.831.831.831.8

31.831.831.831.831.831.831.8

31.831.831.831.831.831.831.831.8

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.634.638.4

38.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.438.429.9

29.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.929.929.9

IFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFL

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

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ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

ES57-0

26

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26

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26

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26

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26

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26

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26

ES57-0

26

ES57-0

26

ES57-0

26

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26

ES57-0

26

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26

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26

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

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ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m

4.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.7

31.5

31.5

31.5

31.5

31.5

31.5

31.531.5

31.5

31.5

31.5

31.5

31.5

31.531.5

31.5

31.5

31.5

31.5

31.5

31.531.5

31.5

31.5

31.5

31.5

31.531.5

31.5

31.5

31.5

31.5

31.5

31.531.5

31.5

31.5

31.5

31.5

31.5

31.531.5

31.5

31.5

31.5

31.5

31.5

31.5

31.5

11.1

11.1

11.1

11.1

11.1

11.1

11.111.1

11.1

11.1

11.1

11.1

11.1

11.111.1

11.1

11.1

11.1

11.1

11.1

11.111.1

11.1

11.1

11.1

11.1

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11.1

11.1

11.1

11.1

11.1

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11.1

11.1

11.1

11.1

11.1

11.111.1

11.1

11.1

11.1

11.1

11.1

11.1

11.1

34.9

34.9

34.9

34.9

34.9

34.9

34.934.9

34.9

34.9

34.9

34.9

34.9

34.934.9

34.9

34.9

34.9

34.9

34.9

34.934.9

34.9

34.9

34.9

34.9

34.934.9

34.9

34.9

34.9

34.9

34.9

34.934.9

34.9

34.9

34.9

34.9

34.9

34.934.9

34.9

34.9

34.9

34.9

34.9

34.9

34.9

1.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.2

26.7

26.7

26.7

26.7

26.7

26.7

26.726.7

26.7

26.7

26.7

26.7

26.7

26.726.7

26.7

26.7

26.7

26.7

26.7

26.726.7

26.7

26.7

26.7

26.7

26.726.7

26.7

26.7

26.7

26.7

26.7

26.726.7

26.7

26.7

26.7

26.7

26.7

26.726.7

26.7

26.7

26.7

26.7

26.7

26.7

26.7

1.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.0

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

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ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m

33.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.633.6

28.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.028.0

8.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.68.6

15.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.115.1

1.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.1

GWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWK

36.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.2

37.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.8

38.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.038.037.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.4

47.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.7

50.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.850.835.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.331.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.631.6

48.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.3

45.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.345.3

48.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.6

51.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.551.533.4

33.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.4

33.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.4

34.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.6

34.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.634.6

51.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.451.4

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ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

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16435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435164351643516435

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16425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425164251642516425

16426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426164261642616426

16427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427164271642716427

16429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429164291642916429

16430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430164301643016430

16431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431164311643116431

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.634.633.8

33.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.833.833.8

31.7

31.7

31.7

31.7

31.7

31.7

31.731.7

31.7

31.7

31.7

31.7

31.7

31.731.7

31.7

31.7

31.7

31.7

31.7

31.731.7

31.7

31.7

31.7

31.7

31.731.7

31.7

31.7

31.7

31.7

31.7

31.731.7

31.7

31.7

31.7

31.7

31.7

31.731.7

31.7

31.7

31.7

31.7

31.7

31.7

31.7

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.034.0

1.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.92.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.1

13.9

13.9

13.9

13.9

13.9

13.9

13.913.9

13.9

13.9

13.9

13.9

13.9

13.913.9

13.9

13.9

13.9

13.9

13.9

13.913.9

13.9

13.9

13.9

13.9

13.913.9

13.9

13.9

13.9

13.9

13.9

13.913.9

13.9

13.9

13.9

13.9

13.9

13.913.9

13.9

13.9

13.9

13.9

13.9

13.9

13.9

25.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.4

25.4

37.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.4

37.4

35.5

35.5

35.5

35.5

35.5

35.5

35.535.5

35.5

35.5

35.5

35.5

35.5

35.535.5

35.5

35.5

35.5

35.5

35.5

35.535.5

35.5

35.5

35.5

35.5

35.535.5

35.5

35.5

35.5

35.5

35.5

35.535.5

35.5

35.5

35.5

35.5

35.5

35.535.5

35.5

35.5

35.5

35.5

35.5

35.5

35.5

16.8

16.8

16.8

16.8

16.8

16.8

16.816.8

16.8

16.8

16.8

16.8

16.8

16.816.8

16.8

16.8

16.8

16.8

16.8

16.816.8

16.8

16.8

16.8

16.8

16.816.8

16.8

16.8

16.8

16.8

16.8

16.816.8

16.8

16.8

16.8

16.8

16.8

16.816.8

16.8

16.8

16.8

16.8

16.8

16.8

16.8

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

3.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.9

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

2.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.2

12.0

12.0

12.0

12.0

12.0

12.0

12.012.0

12.0

12.0

12.0

12.0

12.0

12.012.0

12.0

12.0

12.0

12.0

12.0

12.012.0

12.0

12.0

12.0

12.0

12.012.0

12.0

12.0

12.0

12.0

12.0

12.012.0

12.0

12.0

12.0

12.0

12.0

12.012.0

12.0

12.0

12.0

12.0

12.0

12.0

12.0

0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.21.2

36.7

36.7

36.7

36.7

36.7

36.7

36.736.7

36.7

36.7

36.7

36.7

36.7

36.736.7

36.7

36.7

36.7

36.7

36.7

36.736.7

36.7

36.7

36.7

36.7

36.736.7

36.7

36.7

36.7

36.7

36.7

36.736.7

36.7

36.7

36.7

36.7

36.7

36.736.7

36.7

36.7

36.7

36.7

36.7

36.7

36.7

1636

4

1636

4

1636

4

1636

4

1636

4

1636

4

1636

416

364

1636

4

1636

4

1636

4

1636

4

1636

4

1636

416

364

1636

4

1636

4

1636

4

1636

4

1636

4

1636

416

364

1636

4

1636

4

1636

4

1636

4

1636

416

364

1636

4

1636

4

1636

4

1636

4

1636

4

1636

416

364

1636

4

1636

4

1636

4

1636

4

1636

4

1636

416

364

1636

4

1636

4

1636

4

1636

4

1636

4

1636

416

364

3.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.730

.7

2.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.3

1638

0

1638

0

1638

0

1638

0

1638

0

1638

0

1638

016

380

1638

0

1638

0

1638

0

1638

0

1638

0

1638

016

380

1638

0

1638

0

1638

0

1638

0

1638

0

1638

016

380

1638

0

1638

0

1638

0

1638

0

1638

016

380

1638

0

1638

0

1638

0

1638

0

1638

0

1638

016

380

1638

0

1638

0

1638

0

1638

0

1638

0

1638

016

380

1638

0

1638

0

1638

0

1638

0

1638

0

1638

016

380

1638

1

1638

1

1638

1

1638

1

1638

1

1638

1

1638

116

381

1638

1

1638

1

1638

1

1638

1

1638

1

1638

116

381

1638

1

1638

1

1638

1

1638

1

1638

1

1638

116

381

1638

1

1638

1

1638

1

1638

1

1638

116

381

1638

1

1638

1

1638

1

1638

1

1638

1

1638

116

381

1638

1

1638

1

1638

1

1638

1

1638

1

1638

116

381

1638

1

1638

1

1638

1

1638

1

1638

1

1638

116

381

35.7

35.7

35.7

35.7

35.7

35.7

35.735.7

35.7

35.7

35.7

35.7

35.7

35.735.7

35.7

35.7

35.7

35.7

35.7

35.735.7

35.7

35.7

35.7

35.7

35.735.7

35.7

35.7

35.7

35.7

35.7

35.735.7

35.7

35.7

35.7

35.7

35.7

35.735.7

35.7

35.7

35.7

35.7

35.7

35.7

35.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.725

.713

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.013

.0

39.5

39.5

39.5

39.5

39.5

39.5

39.539.5

39.5

39.5

39.5

39.5

39.5

39.539.5

39.5

39.5

39.5

39.5

39.5

39.539.5

39.5

39.5

39.5

39.5

39.539.5

39.5

39.5

39.5

39.5

39.5

39.539.5

39.5

39.5

39.5

39.5

39.5

39.539.5

39.5

39.5

39.5

39.5

39.5

39.5

39.5

1637

6

1637

6

1637

6

1637

6

1637

6

1637

6

1637

616

376

1637

6

1637

6

1637

6

1637

6

1637

6

1637

616

376

1637

6

1637

6

1637

6

1637

6

1637

6

1637

616

376

1637

6

1637

6

1637

6

1637

6

1637

616

376

1637

6

1637

6

1637

6

1637

6

1637

6

1637

616

376

1637

6

1637

6

1637

6

1637

6

1637

6

1637

616

376

1637

6

1637

6

1637

6

1637

6

1637

6

1637

616

376

1637

7

1637

7

1637

7

1637

7

1637

7

1637

7

1637

716

377

1637

7

1637

7

1637

7

1637

7

1637

7

1637

716

377

1637

7

1637

7

1637

7

1637

7

1637

7

1637

716

377

1637

7

1637

7

1637

7

1637

7

1637

716

377

1637

7

1637

7

1637

7

1637

7

1637

7

1637

716

377

1637

7

1637

7

1637

7

1637

7

1637

7

1637

716

377

1637

7

1637

7

1637

7

1637

7

1637

7

1637

716

377

1637

8

1637

8

1637

8

1637

8

1637

8

1637

8

1637

816

378

1637

8

1637

8

1637

8

1637

8

1637

8

1637

816

378

1637

8

1637

8

1637

8

1637

8

1637

8

1637

816

378

1637

8

1637

8

1637

8

1637

8

1637

816

378

1637

8

1637

8

1637

8

1637

8

1637

8

1637

816

378

1637

8

1637

8

1637

8

1637

8

1637

8

1637

816

378

1637

8

1637

8

1637

8

1637

8

1637

8

1637

816

378

1637

9

1637

9

1637

9

1637

9

1637

9

1637

9

1637

916

379

1637

9

1637

9

1637

9

1637

9

1637

9

1637

916

379

1637

9

1637

9

1637

9

1637

9

1637

9

1637

916

379

1637

9

1637

9

1637

9

1637

9

1637

916

379

1637

9

1637

9

1637

9

1637

9

1637

9

1637

916

379

1637

9

1637

9

1637

9

1637

9

1637

9

1637

916

379

1637

9

1637

9

1637

9

1637

9

1637

9

1637

916

379

1637

4

1637

4

1637

4

1637

4

1637

4

1637

4

1637

416

374

1637

4

1637

4

1637

4

1637

4

1637

4

1637

416

374

1637

4

1637

4

1637

4

1637

4

1637

4

1637

416

374

1637

4

1637

4

1637

4

1637

4

1637

416

374

1637

4

1637

4

1637

4

1637

4

1637

4

1637

416

374

1637

4

1637

4

1637

4

1637

4

1637

4

1637

416

374

1637

4

1637

4

1637

4

1637

4

1637

4

1637

416

374

1637

2

1637

2

1637

2

1637

2

1637

2

1637

2

1637

216

372

1637

2

1637

2

1637

2

1637

2

1637

2

1637

216

372

1637

2

1637

2

1637

2

1637

2

1637

2

1637

216

372

1637

2

1637

2

1637

2

1637

2

1637

216

372

1637

2

1637

2

1637

2

1637

2

1637

2

1637

216

372

1637

2

1637

2

1637

2

1637

2

1637

2

1637

216

372

1637

2

1637

2

1637

2

1637

2

1637

2

1637

216

372

1637

5

1637

5

1637

5

1637

5

1637

5

1637

5

1637

516

375

1637

5

1637

5

1637

5

1637

5

1637

5

1637

516

375

1637

5

1637

5

1637

5

1637

5

1637

5

1637

516

375

1637

5

1637

5

1637

5

1637

5

1637

516

375

1637

5

1637

5

1637

5

1637

5

1637

5

1637

516

375

1637

5

1637

5

1637

5

1637

5

1637

5

1637

516

375

1637

5

1637

5

1637

5

1637

5

1637

5

1637

516

375

1636

8

1636

8

1636

8

1636

8

1636

8

1636

8

1636

816

368

1636

8

1636

8

1636

8

1636

8

1636

8

1636

816

368

1636

8

1636

8

1636

8

1636

8

1636

8

1636

816

368

1636

8

1636

8

1636

8

1636

8

1636

816

368

1636

8

1636

8

1636

8

1636

8

1636

8

1636

816

368

1636

8

1636

8

1636

8

1636

8

1636

8

1636

816

368

1636

8

1636

8

1636

8

1636

8

1636

8

1636

816

368

1636

7

1636

7

1636

7

1636

7

1636

7

1636

7

1636

716

367

1636

7

1636

7

1636

7

1636

7

1636

7

1636

716

367

1636

7

1636

7

1636

7

1636

7

1636

7

1636

716

367

1636

7

1636

7

1636

7

1636

7

1636

716

367

1636

7

1636

7

1636

7

1636

7

1636

7

1636

716

367

1636

7

1636

7

1636

7

1636

7

1636

7

1636

716

367

1636

7

1636

7

1636

7

1636

7

1636

7

1636

716

367

1636

9

1636

9

1636

9

1636

9

1636

9

1636

9

1636

916

369

1636

9

1636

9

1636

9

1636

9

1636

9

1636

916

369

1636

9

1636

9

1636

9

1636

9

1636

9

1636

916

369

1636

9

1636

9

1636

9

1636

9

1636

916

369

1636

9

1636

9

1636

9

1636

9

1636

9

1636

916

369

1636

9

1636

9

1636

9

1636

9

1636

9

1636

916

369

1636

9

1636

9

1636

9

1636

9

1636

9

1636

916

369

1637

0

1637

0

1637

0

1637

0

1637

0

1637

0

1637

016

370

1637

0

1637

0

1637

0

1637

0

1637

0

1637

016

370

1637

0

1637

0

1637

0

1637

0

1637

0

1637

016

370

1637

0

1637

0

1637

0

1637

0

1637

016

370

1637

0

1637

0

1637

0

1637

0

1637

0

1637

016

370

1637

0

1637

0

1637

0

1637

0

1637

0

1637

016

370

1637

0

1637

0

1637

0

1637

0

1637

0

1637

016

370

1637

1

1637

1

1637

1

1637

1

1637

1

1637

1

1637

116

371

1637

1

1637

1

1637

1

1637

1

1637

1

1637

116

371

1637

1

1637

1

1637

1

1637

1

1637

1

1637

116

371

1637

1

1637

1

1637

1

1637

1

1637

116

371

1637

1

1637

1

1637

1

1637

1

1637

1

1637

116

371

1637

1

1637

1

1637

1

1637

1

1637

1

1637

116

371

1637

1

1637

1

1637

1

1637

1

1637

1

1637

116

371

1636

5

1636

5

1636

5

1636

5

1636

5

1636

5

1636

516

365

1636

5

1636

5

1636

5

1636

5

1636

5

1636

516

365

1636

5

1636

5

1636

5

1636

5

1636

5

1636

516

365

1636

5

1636

5

1636

5

1636

5

1636

516

365

1636

5

1636

5

1636

5

1636

5

1636

5

1636

516

365

1636

5

1636

5

1636

5

1636

5

1636

5

1636

516

365

1636

5

1636

5

1636

5

1636

5

1636

5

1636

516

365

1636

6

1636

6

1636

6

1636

6

1636

6

1636

6

1636

616

366

1636

6

1636

6

1636

6

1636

6

1636

6

1636

616

366

1636

6

1636

6

1636

6

1636

6

1636

6

1636

616

366

1636

6

1636

6

1636

6

1636

6

1636

616

366

1636

6

1636

6

1636

6

1636

6

1636

6

1636

616

366

1636

6

1636

6

1636

6

1636

6

1636

6

1636

616

366

1636

6

1636

6

1636

6

1636

6

1636

6

1636

616

366

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

15.7

15.7

15.7

15.7

15.7

15.7

15.715.7

15.7

15.7

15.7

15.7

15.7

15.715.7

15.7

15.7

15.7

15.7

15.7

15.715.7

15.7

15.7

15.7

15.7

15.715.7

15.7

15.7

15.7

15.7

15.7

15.715.7

15.7

15.7

15.7

15.7

15.7

15.715.7

15.7

15.7

15.7

15.7

15.7

15.7

15.7

54.5

54.5

54.5

54.5

54.5

54.5

54.554.5

54.5

54.5

54.5

54.5

54.5

54.554.5

54.5

54.5

54.5

54.5

54.5

54.554.5

54.5

54.5

54.5

54.5

54.554.5

54.5

54.5

54.5

54.5

54.5

54.554.5

54.5

54.5

54.5

54.5

54.5

54.554.5

54.5

54.5

54.5

54.5

54.5

54.5

54.5

35.2

35.2

35.2

35.2

35.2

35.2

35.235.2

35.2

35.2

35.2

35.2

35.2

35.235.2

35.2

35.2

35.2

35.2

35.2

35.235.2

35.2

35.2

35.2

35.2

35.235.2

35.2

35.2

35.2

35.2

35.2

35.235.2

35.2

35.2

35.2

35.2

35.2

35.235.2

35.2

35.2

35.2

35.2

35.2

35.2

35.2

44.8

44.8

44.8

44.8

44.8

44.8

44.844.8

44.8

44.8

44.8

44.8

44.8

44.844.8

44.8

44.8

44.8

44.8

44.8

44.844.8

44.8

44.8

44.8

44.8

44.844.8

44.8

44.8

44.8

44.8

44.8

44.844.8

44.8

44.8

44.8

44.8

44.8

44.844.8

44.8

44.8

44.8

44.8

44.8

44.8

44.8

52.6

52.6

52.6

52.6

52.6

52.6

52.652.6

52.6

52.6

52.6

52.6

52.6

52.652.6

52.6

52.6

52.6

52.6

52.6

52.652.6

52.6

52.6

52.6

52.6

52.652.6

52.6

52.6

52.6

52.6

52.6

52.652.6

52.6

52.6

52.6

52.6

52.6

52.652.6

52.6

52.6

52.6

52.6

52.6

52.6

52.6

52.0

52.0

52.0

52.0

52.0

52.0

52.052.0

52.0

52.0

52.0

52.0

52.0

52.052.0

52.0

52.0

52.0

52.0

52.0

52.052.0

52.0

52.0

52.0

52.0

52.052.0

52.0

52.0

52.0

52.0

52.0

52.052.0

52.0

52.0

52.0

52.0

52.0

52.052.0

52.0

52.0

52.0

52.0

52.0

52.0

52.0

25.0

25.0

25.0

25.0

25.0

25.0

25.025.0

25.0

25.0

25.0

25.0

25.0

25.025.0

25.0

25.0

25.0

25.0

25.0

25.025.0

25.0

25.0

25.0

25.0

25.025.0

25.0

25.0

25.0

25.0

25.0

25.025.0

25.0

25.0

25.0

25.0

25.0

25.025.0

25.0

25.0

25.0

25.0

25.0

25.0

25.0

46.2

46.2

46.2

46.2

46.2

46.2

46.246.2

46.2

46.2

46.2

46.2

46.2

46.246.2

46.2

46.2

46.2

46.2

46.2

46.246.2

46.2

46.2

46.2

46.2

46.246.2

46.2

46.2

46.2

46.2

46.2

46.246.2

46.2

46.2

46.2

46.2

46.2

46.246.2

46.2

46.2

46.2

46.2

46.2

46.2

46.2

44.4

44.4

44.4

44.4

44.4

44.4

44.444.4

44.4

44.4

44.4

44.4

44.4

44.444.4

44.4

44.4

44.4

44.4

44.4

44.444.4

44.4

44.4

44.4

44.4

44.444.4

44.4

44.4

44.4

44.4

44.4

44.444.4

44.4

44.4

44.4

44.4

44.4

44.444.4

44.4

44.4

44.4

44.4

44.4

44.4

44.4

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMQPQPQPQPQPQPQP

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

33.4

33.4

33.4

33.4

33.4

33.4

33.433.4

33.4

33.4

33.4

33.4

33.4

33.433.4

33.4

33.4

33.4

33.4

33.4

33.433.4

33.4

33.4

33.4

33.4

33.433.4

33.4

33.4

33.4

33.4

33.4

33.433.4

33.4

33.4

33.4

33.4

33.4

33.433.4

33.4

33.4

33.4

33.4

33.4

33.4

33.4

48.9

48.9

48.9

48.9

48.9

48.9

48.948.9

48.9

48.9

48.9

48.9

48.9

48.948.9

48.9

48.9

48.9

48.9

48.9

48.948.9

48.9

48.9

48.9

48.9

48.948.9

48.9

48.9

48.9

48.9

48.9

48.948.9

48.9

48.9

48.9

48.9

48.9

48.948.9

48.9

48.9

48.9

48.9

48.9

48.9

48.9

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

1636

3

1636

3

1636

3

1636

3

1636

3

1636

3

1636

316

363

1636

3

1636

3

1636

3

1636

3

1636

3

1636

316

363

1636

3

1636

3

1636

3

1636

3

1636

3

1636

316

363

1636

3

1636

3

1636

3

1636

3

1636

316

363

1636

3

1636

3

1636

3

1636

3

1636

3

1636

316

363

1636

3

1636

3

1636

3

1636

3

1636

3

1636

316

363

1636

3

1636

3

1636

3

1636

3

1636

3

1636

316

363

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

52.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.552.5

11.2

11.2

11.2

11.2

11.2

11.2

11.211.2

11.2

11.2

11.2

11.2

11.2

11.211.2

11.2

11.2

11.2

11.2

11.2

11.211.2

11.2

11.2

11.2

11.2

11.211.2

11.2

11.2

11.2

11.2

11.2

11.211.2

11.2

11.2

11.2

11.2

11.2

11.211.2

11.2

11.2

11.2

11.2

11.2

11.2

11.2

2.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.0

49.2

49.2

49.2

49.2

49.2

49.2

49.249.2

49.2

49.2

49.2

49.2

49.2

49.249.2

49.2

49.2

49.2

49.2

49.2

49.249.2

49.2

49.2

49.2

49.2

49.249.2

49.2

49.2

49.2

49.2

49.2

49.249.2

49.2

49.2

49.2

49.2

49.2

49.249.2

49.2

49.2

49.2

49.2

49.2

49.2

49.2

50.3

50.3

50.3

50.3

50.3

50.3

50.350.3

50.3

50.3

50.3

50.3

50.3

50.350.3

50.3

50.3

50.3

50.3

50.3

50.350.3

50.3

50.3

50.3

50.3

50.350.3

50.3

50.3

50.3

50.3

50.3

50.350.3

50.3

50.3

50.3

50.3

50.3

50.350.3

50.3

50.3

50.3

50.3

50.3

50.3

50.3

9.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.39.3

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

36.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.0

0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.240.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.840.8

47.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.5

50.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.1

51.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.251.2

51.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.651.6

34.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.734.7

53.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.353.3

36.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.2

36.2

39.0

39.0

39.0

39.0

39.0

39.0

39.039.0

39.0

39.0

39.0

39.0

39.0

39.039.0

39.0

39.0

39.0

39.0

39.0

39.039.0

39.0

39.0

39.0

39.0

39.039.0

39.0

39.0

39.0

39.0

39.0

39.039.0

39.0

39.0

39.0

39.0

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39.039.0

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36.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.4

27.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.8 50.5

50.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.550.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.547.546.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.1

34.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.234.237.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.4

36.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.4

35.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.235.2 39.1

39.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.139.1

48.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.848.8

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45.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.145.1

50.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.050.0

37.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.936.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.336.3

32.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.132.1

33.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.533.5

46.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.6

35.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.0

44.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.744.754.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.254.2

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44.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.8

56.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.856.8

55.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.555.5

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37.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.637.6

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37.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.937.9

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56.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.156.1

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3

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3

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3

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3

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3

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3

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3

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3

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3

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3

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3

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3

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3

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4

1635

4

1635

4

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4

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4

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354

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4

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4

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4

1635

4

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4

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354

38.5

38.5

38.5

38.5

38.5

38.5

38.538.5

38.5

38.5

38.5

38.5

38.5

38.538.5

38.5

38.5

38.5

38.5

38.5

38.538.5

38.5

38.5

38.5

38.5

38.538.5

38.5

38.5

38.5

38.5

38.5

38.538.5

38.5

38.5

38.5

38.5

38.5

38.538.5

38.5

38.5

38.5

38.5

38.5

38.5

38.5

2.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.1

IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

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IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

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QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

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2

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1636

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2

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2

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0

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0

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0

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0

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0

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0

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0

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0

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0

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0

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0

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0

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0

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361

36.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.0

36.0

37.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.0

37.0

37.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.437.4

37.4

37.4

37.4

37.4

37.4

37.4

37.4

8.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.98.9

49.8

49.8

49.8

49.8

49.8

49.8

49.849.8

49.8

49.8

49.8

49.8

49.8

49.849.8

49.8

49.8

49.8

49.8

49.8

49.849.8

49.8

49.8

49.8

49.8

49.849.8

49.8

49.8

49.8

49.8

49.8

49.849.8

49.8

49.8

49.8

49.8

49.8

49.849.8

49.8

49.8

49.8

49.8

49.8

49.8

49.833

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.533

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.533

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.533

.533

.533

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.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.533

.5

2.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.339

.239

.239

.239

.239

.239

.239

.239

.239

.239

.239

.239

.239

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.239

.239

.239

.239

.239

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.2

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.355

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.8

0.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.6

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

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2.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.62.6

32.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.232.2

1.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.0

45.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.445.4

2.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.1

20.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.720.7

0.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.4

26.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.626.6

34.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.4

32.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.7

16.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.634.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.0

2.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.42.4

46.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.4

40.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.940.9

15.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.215.2

16393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393163931639316393

25.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.5

17.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.517.5

16.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.316.3

11.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.111.1

2.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.82.8

9.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.69.6

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

0.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.6

1639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216392163921639216391

163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391163911639116391

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16386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386163861638616386

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IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM16390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390163901639016390

16384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384163841638416384

16382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382163821638216382

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QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

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36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.436.432.8

32.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.832.8

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2.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.229.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.829.8

33.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.133.1

16403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403164031640316403

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31.231.231.231.231.231.231.2

31.231.231.231.231.231.231.2

31.231.231.231.231.231.231.2

31.231.231.231.231.231.2

31.231.231.231.231.231.231.2

31.231.231.231.231.231.231.2

31.231.231.231.231.231.231.231.234.9

34.934.934.934.934.934.9

34.934.934.934.934.934.934.9

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34.934.934.934.934.934.9

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34.934.934.934.934.934.934.934.932.4

32.432.432.432.432.432.4

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32.432.432.432.432.432.432.432.438.3

38.338.338.338.338.338.3

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38.338.338.338.338.338.338.3

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38.338.338.338.338.338.338.3

38.338.338.338.338.338.338.338.3

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IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

16409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409164091640916409

16410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410164101641016410

16411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411164111641116411

16412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412164121641216412

16413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413164131641316413

5755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755575557555755

53.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.453.4

34.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.1

IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

38.038.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.038.038.0

35.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.835.837.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.4

38.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.9

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.334.3

IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.635.637.5

37.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.537.538.4

38.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.438.4

22.922.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.922.9

22.922.922.922.922.922.922.922.926.3

26.326.326.326.326.326.3

26.326.326.326.326.326.326.3

26.326.326.326.326.326.326.3

26.326.326.326.326.326.3

26.326.326.326.326.326.326.3

26.326.326.326.326.326.326.3

26.326.326.326.326.326.326.326.3RMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.151

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.751

.7

54.2

54.2

54.2

54.2

54.2

54.2

54.254.2

54.2

54.2

54.2

54.2

54.2

54.254.2

54.2

54.2

54.2

54.2

54.2

54.254.2

54.2

54.2

54.2

54.2

54.254.2

54.2

54.2

54.2

54.2

54.2

54.254.2

54.2

54.2

54.2

54.2

54.2

54.254.2

54.2

54.2

54.2

54.2

54.2

54.2

54.2

29.5

29.5

29.5

29.5

29.5

29.5

29.529.5

29.5

29.5

29.5

29.5

29.5

29.529.5

29.5

29.5

29.5

29.5

29.5

29.529.5

29.5

29.5

29.5

29.5

29.529.5

29.5

29.5

29.5

29.5

29.5

29.529.5

29.5

29.5

29.5

29.5

29.5

29.529.5

29.5

29.5

29.5

29.5

29.5

29.5

29.5

36.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.036.0

36.0

36.0

36.0

36.0

36.0

36.0

36.0

38.7

38.7

38.7

38.7

38.7

38.7

38.738.7

38.7

38.7

38.7

38.7

38.7

38.738.7

38.7

38.7

38.7

38.7

38.7

38.738.7

38.7

38.7

38.7

38.7

38.738.7

38.7

38.7

38.7

38.7

38.7

38.738.7

38.7

38.7

38.7

38.7

38.7

38.738.7

38.7

38.7

38.7

38.7

38.7

38.7

38.7

38.8

38.8

38.8

38.8

38.8

38.8

38.838.8

38.8

38.8

38.8

38.8

38.8

38.838.8

38.8

38.8

38.8

38.8

38.8

38.838.8

38.8

38.8

38.8

38.8

38.838.8

38.8

38.8

38.8

38.8

38.8

38.838.8

38.8

38.8

38.8

38.8

38.8

38.838.8

38.8

38.8

38.8

38.8

38.8

38.8

38.8

30.8

30.8

30.8

30.8

30.8

30.8

30.830.8

30.8

30.8

30.8

30.8

30.8

30.830.8

30.8

30.8

30.8

30.8

30.8

30.830.8

30.8

30.8

30.8

30.8

30.830.8

30.8

30.8

30.8

30.8

30.8

30.830.8

30.8

30.8

30.8

30.8

30.8

30.830.8

30.8

30.8

30.8

30.8

30.8

30.8

30.827

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.727

.76.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.86.8

14.3

14.3

14.3

14.3

14.3

14.3

14.314.3

14.3

14.3

14.3

14.3

14.3

14.314.3

14.3

14.3

14.3

14.3

14.3

14.314.3

14.3

14.3

14.3

14.3

14.314.3

14.3

14.3

14.3

14.3

14.3

14.314.3

14.3

14.3

14.3

14.3

14.3

14.314.3

14.3

14.3

14.3

14.3

14.3

14.3

14.3

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.8

10.7

10.7

10.7

10.7

10.7

10.7

10.710.7

10.7

10.7

10.7

10.7

10.7

10.710.7

10.7

10.7

10.7

10.7

10.7

10.710.7

10.7

10.7

10.7

10.7

10.710.7

10.7

10.7

10.7

10.7

10.7

10.710.7

10.7

10.7

10.7

10.7

10.7

10.710.7

10.7

10.7

10.7

10.7

10.7

10.7

10.7

30.2

30.2

30.2

30.2

30.2

30.2

30.230.2

30.2

30.2

30.2

30.2

30.2

30.230.2

30.2

30.2

30.2

30.2

30.2

30.230.2

30.2

30.2

30.2

30.2

30.230.2

30.2

30.2

30.2

30.2

30.2

30.230.2

30.2

30.2

30.2

30.2

30.2

30.230.2

30.2

30.2

30.2

30.2

30.2

30.2

30.2

12.6

12.6

12.6

12.6

12.6

12.6

12.612.6

12.6

12.6

12.6

12.6

12.6

12.612.6

12.6

12.6

12.6

12.6

12.6

12.612.6

12.6

12.6

12.6

12.6

12.612.6

12.6

12.6

12.6

12.6

12.6

12.612.6

12.6

12.6

12.6

12.6

12.6

12.612.6

12.6

12.6

12.6

12.6

12.6

12.6

12.6

0.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.12.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.32.3

0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.21.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.01.0

18.4

18.4

18.4

18.4

18.4

18.4

18.418.4

18.4

18.4

18.4

18.4

18.4

18.418.4

18.4

18.4

18.4

18.4

18.4

18.418.4

18.4

18.4

18.4

18.4

18.418.4

18.4

18.4

18.4

18.4

18.4

18.418.4

18.4

18.4

18.4

18.4

18.4

18.418.4

18.4

18.4

18.4

18.4

18.4

18.4

18.4

9.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.715.2

15.2

15.2

15.2

15.2

15.2

15.215.2

15.2

15.2

15.2

15.2

15.2

15.215.2

15.2

15.2

15.2

15.2

15.2

15.215.2

15.2

15.2

15.2

15.2

15.215.2

15.2

15.2

15.2

15.2

15.2

15.215.2

15.2

15.2

15.2

15.2

15.2

15.215.2

15.2

15.2

15.2

15.2

15.2

15.2

15.2

4.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.614

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.114

.1

1633

5

1633

5

1633

5

1633

5

1633

5

1633

5

1633

516

335

1633

5

1633

5

1633

5

1633

5

1633

5

1633

516

335

1633

5

1633

5

1633

5

1633

5

1633

5

1633

516

335

1633

5

1633

5

1633

5

1633

5

1633

516

335

1633

5

1633

5

1633

5

1633

5

1633

5

1633

516

335

1633

5

1633

5

1633

5

1633

5

1633

5

1633

516

335

1633

5

1633

5

1633

5

1633

5

1633

5

1633

516

33516

334

1633

4

1633

4

1633

4

1633

4

1633

4

1633

416

334

1633

4

1633

4

1633

4

1633

4

1633

4

1633

416

334

1633

4

1633

4

1633

4

1633

4

1633

4

1633

416

334

1633

4

1633

4

1633

4

1633

4

1633

416

334

1633

4

1633

4

1633

4

1633

4

1633

4

1633

416

334

1633

4

1633

4

1633

4

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250m E

lev 350m

Elev

150m E

lev

5,644,150mN

5,644,150mN

5,644,050mN

50m E

lev

5,644,350mN

5,644,350mN

450

m E

lev

50m

Ele

v 1

50m

Ele

v 2

50m

Ele

v 3

50m

Ele

v 450m

Elev

5,644,250mN

5,644,250mN

5,644,650mN

5,644,650mN 5,644,550mN

5,644,550mN

5,644,450mN

5,644,450mN

Scale 1:1,000Section Origin (top left)542,799.96 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

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ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024

ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024ES56-024137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m137.16m

ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026

ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026ES57-026185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m185.93m

ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228m228mES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168m168mES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-008ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007ES08-007

Raytec Metals Corp.

El Sol ProjectA Zone

Section E542799

0 25

metres

50

Scale: 1:1000

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

IFMJ

IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

Quartz Porphyry

Granitic Dyke

Biotite dyke

GD

QP

CASCasing

OVEROverburden

BD

Legend

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29.029.029.029.029.029.029.0

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29.029.029.029.029.029.029.029.024.1

24.124.124.124.124.124.1

24.124.124.124.124.124.124.1

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32.832.832.832.832.832.8

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32.832.832.832.832.832.832.8

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32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

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30.730.730.730.730.730.730.7

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34.034.034.034.034.034.0

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39.239.239.239.239.239.2

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33.133.133.133.133.133.133.1

33.133.133.133.133.133.133.1

33.133.133.133.133.133.133.1

33.133.133.133.133.133.1

33.133.133.133.133.133.133.1

33.133.133.133.133.133.133.1

33.133.133.133.133.133.133.133.1

26.026.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.026.026.027.5

27.527.527.527.527.527.5

27.527.527.527.527.527.527.5

27.527.527.527.527.527.527.5

27.527.527.527.527.527.5

27.527.527.527.527.527.527.5

27.527.527.527.527.527.527.5

27.527.527.527.527.527.527.527.527.3

27.327.327.327.327.327.3

27.327.327.327.327.327.327.3

27.327.327.327.327.327.327.3

27.327.327.327.327.327.3

27.327.327.327.327.327.327.3

27.327.327.327.327.327.327.3

27.327.327.327.327.327.327.327.327.8

27.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.827.8

11.611.611.611.611.611.611.6

11.611.611.611.611.611.611.6

11.611.611.611.611.611.611.6

11.611.611.611.611.611.6

11.611.611.611.611.611.611.6

11.611.611.611.611.611.611.6

11.611.611.611.611.611.611.611.63.13.13.13.13.13.13.1

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0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

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34.134.134.134.134.134.134.134.130.0

30.030.030.030.030.030.0

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30.030.030.030.030.030.030.030.019.8

19.819.819.819.819.819.8

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40.940.940.940.940.940.940.9

40.940.940.940.940.940.940.9

40.940.940.940.940.940.940.9

40.940.940.940.940.940.9

40.940.940.940.940.940.940.9

40.940.940.940.940.940.940.9

40.940.940.940.940.940.940.940.942.7

42.742.742.742.742.742.7

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42.742.742.742.742.742.7

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42.742.742.742.742.742.742.7

42.742.742.742.742.742.742.742.71.81.81.81.81.81.81.8

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33.533.533.533.533.533.533.5

33.533.533.533.533.533.533.5

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33.533.533.533.533.533.533.533.5

16.816.816.816.816.816.816.8

16.816.816.816.816.816.816.8

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16.816.816.816.816.816.816.816.834.8

34.834.834.834.834.834.8

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16.716.716.716.716.716.7

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16.716.716.716.716.716.716.716.7

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31.131.131.131.131.131.131.1

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0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

13.513.513.513.513.513.513.5

13.513.513.513.513.513.513.5

13.513.513.513.513.513.513.5

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17.817.817.817.817.817.817.8

17.817.817.817.817.817.817.8

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17.817.817.817.817.817.817.8

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12.112.112.112.112.112.1

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12.112.112.112.112.112.112.1

12.112.112.112.112.112.112.1

12.112.112.112.112.112.112.112.1ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035ES57-035

247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m247.8m

4.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.9

22.222.222.222.222.222.222.2

22.222.222.222.222.222.222.2

22.222.222.222.222.222.222.2

22.222.222.222.222.222.2

22.222.222.222.222.222.222.2

22.222.222.222.222.222.222.2

22.222.222.222.222.222.222.222.2

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34.434.434.434.434.434.4

34.434.434.434.434.434.434.4

34.434.434.434.434.434.434.4

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34.434.434.434.434.434.434.434.4

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33.833.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.833.8

33.833.833.833.833.833.833.833.829.0

29.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.029.0

29.029.029.029.029.029.029.029.023.8

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23.823.823.823.823.823.823.8

23.823.823.823.823.823.823.8

23.823.823.823.823.823.8

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23.823.823.823.823.823.823.8

23.823.823.823.823.823.823.823.8

37.537.537.537.537.537.537.5

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37.537.537.537.537.537.537.537.5

31.131.131.131.131.131.131.1

31.131.131.131.131.131.131.1

31.131.131.131.131.131.131.1

31.131.131.131.131.131.1

31.131.131.131.131.131.131.1

31.131.131.131.131.131.131.1

31.131.131.131.131.131.131.131.132.7

32.732.732.732.732.732.7

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32.732.732.732.732.732.732.7

32.732.732.732.732.732.732.7

32.732.732.732.732.732.732.732.735.6

35.635.635.635.635.635.6

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33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.3

33.333.333.333.333.333.333.333.332.9

32.932.932.932.932.932.9

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32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.932.935.4

35.435.435.435.435.435.4

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35.435.435.435.435.435.435.4

35.435.435.435.435.435.4

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31.431.431.431.431.431.4

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25.825.825.825.825.825.825.825.8

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37.837.837.837.837.837.837.8

37.837.837.837.837.837.837.8

37.837.837.837.837.837.8

37.837.837.837.837.837.837.8

37.837.837.837.837.837.837.8

37.837.837.837.837.837.837.837.840.3

40.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.340.340.341.9

41.941.941.941.941.941.9

41.941.941.941.941.941.941.9

41.941.941.941.941.941.941.9

41.941.941.941.941.941.9

41.941.941.941.941.941.941.9

41.941.941.941.941.941.941.9

41.941.941.941.941.941.941.941.946.1

46.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.146.147.7

47.747.747.747.747.747.7

47.747.747.747.747.747.747.7

47.747.747.747.747.747.747.7

47.747.747.747.747.747.7

47.747.747.747.747.747.747.7

47.747.747.747.747.747.747.7

47.747.747.747.747.747.747.747.748.2

48.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.248.2

16288162881628816288162881628816288

16288162881628816288162881628816288

16288162881628816288162881628816288

162881628816288162881628816288

16288162881628816288162881628816288

16288162881628816288162881628816288

16288162881628816288162881628816288

1628816290162901629016290162901629016290

16290162901629016290162901629016290

16290162901629016290162901629016290

162901629016290162901629016290

16290162901629016290162901629016290

16290162901629016290162901629016290

16290162901629016290162901629016290

16290

16291162911629116291162911629116291

16291162911629116291162911629116291

16291162911629116291162911629116291

162911629116291162911629116291

16291162911629116291162911629116291

16291162911629116291162911629116291

16291162911629116291162911629116291

16291

16292162921629216292162921629216292

16292162921629216292162921629216292

16292162921629216292162921629216292

162921629216292162921629216292

16292162921629216292162921629216292

16292162921629216292162921629216292

16292162921629216292162921629216292

16292

16293162931629316293162931629316293

16293162931629316293162931629316293

16293162931629316293162931629316293

162931629316293162931629316293

16293162931629316293162931629316293

16293162931629316293162931629316293

16293162931629316293162931629316293

16293

5754575457545754575457545754

5754575457545754575457545754

5754575457545754575457545754

575457545754575457545754

5754575457545754575457545754

5754575457545754575457545754

5754575457545754575457545754575416294

162941629416294162941629416294

16294162941629416294162941629416294

16294162941629416294162941629416294

162941629416294162941629416294

16294162941629416294162941629416294

16294162941629416294162941629416294

16294162941629416294162941629416294

16294

42.742.742.742.742.742.742.7

42.742.742.742.742.742.742.7

42.742.742.742.742.742.742.7

42.742.742.742.742.742.7

42.742.742.742.742.742.742.7

42.742.742.742.742.742.742.7

42.742.742.742.742.742.742.742.7

40.740.740.740.740.740.740.7

40.740.740.740.740.740.740.7

40.740.740.740.740.740.740.7

40.740.740.740.740.740.7

40.740.740.740.740.740.740.7

40.740.740.740.740.740.740.7

40.740.740.740.740.740.740.740.7

0.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.739.5

39.539.539.539.539.539.5

39.539.539.539.539.539.539.5

39.539.539.539.539.539.539.5

39.539.539.539.539.539.5

39.539.539.539.539.539.539.5

39.539.539.539.539.539.539.5

39.539.539.539.539.539.539.539.50.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.353.0

53.053.053.053.053.053.0

53.053.053.053.053.053.053.0

53.053.053.053.053.053.053.0

53.053.053.053.053.053.0

53.053.053.053.053.053.053.0

53.053.053.053.053.053.053.0

53.053.053.053.053.053.053.053.048.1

48.148.148.148.148.148.1

48.148.148.148.148.148.148.1

48.148.148.148.148.148.148.1

48.148.148.148.148.148.1

48.148.148.148.148.148.148.1

48.148.148.148.148.148.148.1

48.148.148.148.148.148.148.148.146.9

46.946.946.946.946.946.9

46.946.946.946.946.946.946.9

46.946.946.946.946.946.946.9

46.946.946.946.946.946.9

46.946.946.946.946.946.946.9

46.946.946.946.946.946.946.9

46.946.946.946.946.946.946.946.9

16295162951629516295162951629516295

16295162951629516295162951629516295

16295162951629516295162951629516295

162951629516295162951629516295

16295162951629516295162951629516295

16295162951629516295162951629516295

16295162951629516295162951629516295

1629516296162961629616296162961629616296

16296162961629616296162961629616296

16296162961629616296162961629616296

162961629616296162961629616296

16296162961629616296162961629616296

16296162961629616296162961629616296

16296162961629616296162961629616296

1629616297162971629716297162971629716297

16297162971629716297162971629716297

16297162971629716297162971629716297

162971629716297162971629716297

16297162971629716297162971629716297

16297162971629716297162971629716297

16297162971629716297162971629716297

16297

16299162991629916299162991629916299

16299162991629916299162991629916299

16299162991629916299162991629916299

162991629916299162991629916299

16299162991629916299162991629916299

16299162991629916299162991629916299

16299162991629916299162991629916299

16299

16300163001630016300163001630016300

16300163001630016300163001630016300

16300163001630016300163001630016300

163001630016300163001630016300

16300163001630016300163001630016300

16300163001630016300163001630016300

16300163001630016300163001630016300

16300

44.744.744.744.744.744.744.7

44.744.744.744.744.744.744.7

44.744.744.744.744.744.744.7

44.744.744.744.744.744.7

44.744.744.744.744.744.744.7

44.744.744.744.744.744.744.7

44.744.744.744.744.744.744.744.7

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.637.645.2

45.245.245.245.245.245.2

45.245.245.245.245.245.245.2

45.245.245.245.245.245.245.2

45.245.245.245.245.245.2

45.245.245.245.245.245.245.2

45.245.245.245.245.245.245.2

45.245.245.245.245.245.245.245.2

44.144.144.144.144.144.144.1

44.144.144.144.144.144.144.1

44.144.144.144.144.144.144.1

44.144.144.144.144.144.1

44.144.144.144.144.144.144.1

44.144.144.144.144.144.144.1

44.144.144.144.144.144.144.144.139.839.839.839.839.839.839.8

39.839.839.839.839.839.839.8

39.839.839.839.839.839.839.8

39.839.839.839.839.839.8

39.839.839.839.839.839.839.8

39.839.839.839.839.839.839.8

39.839.839.839.839.839.839.839.821.7

21.721.721.721.721.721.7

21.721.721.721.721.721.721.7

21.721.721.721.721.721.721.7

21.721.721.721.721.721.7

21.721.721.721.721.721.721.7

21.721.721.721.721.721.721.7

21.721.721.721.721.721.721.721.7

16305163051630516305163051630516305

16305163051630516305163051630516305

16305163051630516305163051630516305

163051630516305163051630516305

16305163051630516305163051630516305

16305163051630516305163051630516305

16305163051630516305163051630516305

1630516303163031630316303163031630316303

16303163031630316303163031630316303

16303163031630316303163031630316303

163031630316303163031630316303

16303163031630316303163031630316303

16303163031630316303163031630316303

16303163031630316303163031630316303

1630316301163011630116301163011630116301

16301163011630116301163011630116301

16301163011630116301163011630116301

163011630116301163011630116301

16301163011630116301163011630116301

16301163011630116301163011630116301

16301163011630116301163011630116301

16301

16302163021630216302163021630216302

16302163021630216302163021630216302

16302163021630216302163021630216302

163021630216302163021630216302

16302163021630216302163021630216302

16302163021630216302163021630216302

16302163021630216302163021630216302

1630216304163041630416304163041630416304

16304163041630416304163041630416304

16304163041630416304163041630416304

163041630416304163041630416304

16304163041630416304163041630416304

16304163041630416304163041630416304

16304163041630416304163041630416304

16304

12.512.512.512.512.512.512.5

12.512.512.512.512.512.512.5

12.512.512.512.512.512.512.5

12.512.512.512.512.512.5

12.512.512.512.512.512.512.5

12.512.512.512.512.512.512.5

12.512.512.512.512.512.512.512.5

16306163061630616306163061630616306

16306163061630616306163061630616306

16306163061630616306163061630616306

163061630616306163061630616306

16306163061630616306163061630616306

16306163061630616306163061630616306

16306163061630616306163061630616306

16306

16307163071630716307163071630716307

16307163071630716307163071630716307

16307163071630716307163071630716307

163071630716307163071630716307

16307163071630716307163071630716307

16307163071630716307163071630716307

16307163071630716307163071630716307

16307

16309163091630916309163091630916309

16309163091630916309163091630916309

16309163091630916309163091630916309

163091630916309163091630916309

16309163091630916309163091630916309

16309163091630916309163091630916309

16309163091630916309163091630916309

16309

16310163101631016310163101631016310

16310163101631016310163101631016310

16310163101631016310163101631016310

163101631016310163101631016310

16310163101631016310163101631016310

16310163101631016310163101631016310

16310163101631016310163101631016310

16310

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.035.0

37.337.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.337.337.340.3

40.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.340.3

40.340.340.340.340.340.340.340.336.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.036.0

52.152.152.152.152.152.152.1

52.152.152.152.152.152.152.1

52.152.152.152.152.152.152.1

52.152.152.152.152.152.1

52.152.152.152.152.152.152.1

52.152.152.152.152.152.152.1

52.152.152.152.152.152.152.152.139.6

39.639.639.639.639.639.6

39.639.639.639.639.639.639.6

39.639.639.639.639.639.639.6

39.639.639.639.639.639.6

39.639.639.639.639.639.639.6

39.639.639.639.639.639.639.6

39.639.639.639.639.639.639.639.6

25.025.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.025.025.017.9

17.917.917.917.917.917.9

17.917.917.917.917.917.917.9

17.917.917.917.917.917.917.9

17.917.917.917.917.917.9

17.917.917.917.917.917.917.9

17.917.917.917.917.917.917.9

17.917.917.917.917.917.917.917.9

16311163111631116311163111631116311

16311163111631116311163111631116311

16311163111631116311163111631116311

163111631116311163111631116311

16311163111631116311163111631116311

16311163111631116311163111631116311

16311163111631116311163111631116311

1631116312163121631216312163121631216312

16312163121631216312163121631216312

16312163121631216312163121631216312

163121631216312163121631216312

16312163121631216312163121631216312

16312163121631216312163121631216312

16312163121631216312163121631216312

16312

16313163131631316313163131631316313

16313163131631316313163131631316313

16313163131631316313163131631316313

163131631316313163131631316313

16313163131631316313163131631316313

16313163131631316313163131631316313

16313163131631316313163131631316313

16313

6.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.06.0

16314163141631416314163141631416314

16314163141631416314163141631416314

16314163141631416314163141631416314

163141631416314163141631416314

16314163141631416314163141631416314

16314163141631416314163141631416314

16314163141631416314163141631416314

16314

16315163151631516315163151631516315

16315163151631516315163151631516315

16315163151631516315163151631516315

163151631516315163151631516315

16315163151631516315163151631516315

16315163151631516315163151631516315

16315163151631516315163151631516315

16315

16316163161631616316163161631616316

16316163161631616316163161631616316

16316163161631616316163161631616316

163161631616316163161631616316

16316163161631616316163161631616316

16316163161631616316163161631616316

16316163161631616316163161631616316

16316IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

16317163171631716317163171631716317

16317163171631716317163171631716317

16317163171631716317163171631716317

163171631716317163171631716317

16317163171631716317163171631716317

16317163171631716317163171631716317

16317163171631716317163171631716317

16317

16319163191631916319163191631916319

16319163191631916319163191631916319

16319163191631916319163191631916319

163191631916319163191631916319

16319163191631916319163191631916319

16319163191631916319163191631916319

16319163191631916319163191631916319

16319

IFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFL

QBS

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QBS

QBS

QBS

QBS

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QBS

QBS

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QBS

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QBS

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QBS

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QBS

QBS

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QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

16322163221632216322163221632216322

16322163221632216322163221632216322

16322163221632216322163221632216322

163221632216322163221632216322

16322163221632216322163221632216322

16322163221632216322163221632216322

16322163221632216322163221632216322

1632216320163201632016320163201632016320

16320163201632016320163201632016320

16320163201632016320163201632016320

163201632016320163201632016320

16320163201632016320163201632016320

16320163201632016320163201632016320

16320163201632016320163201632016320

16320

16321163211632116321163211632116321

16321163211632116321163211632116321

16321163211632116321163211632116321

163211632116321163211632116321

16321163211632116321163211632116321

16321163211632116321163211632116321

16321163211632116321163211632116321

1632116323163231632316323163231632316323

16323163231632316323163231632316323

16323163231632316323163231632316323

163231632316323163231632316323

16323163231632316323163231632316323

16323163231632316323163231632316323

16323163231632316323163231632316323

16323

16324163241632416324163241632416324

16324163241632416324163241632416324

16324163241632416324163241632416324

163241632416324163241632416324

16324163241632416324163241632416324

16324163241632416324163241632416324

16324163241632416324163241632416324

16324

16329163291632916329163291632916329

16329163291632916329163291632916329

16329163291632916329163291632916329

163291632916329163291632916329

16329163291632916329163291632916329

16329163291632916329163291632916329

16329163291632916329163291632916329

1632916325163251632516325163251632516325

16325163251632516325163251632516325

16325163251632516325163251632516325

163251632516325163251632516325

16325163251632516325163251632516325

16325163251632516325163251632516325

16325163251632516325163251632516325

16325

16326163261632616326163261632616326

16326163261632616326163261632616326

16326163261632616326163261632616326

163261632616326163261632616326

16326163261632616326163261632616326

16326163261632616326163261632616326

16326163261632616326163261632616326

16326

16328163281632816328163281632816328

16328163281632816328163281632816328

16328163281632816328163281632816328

163281632816328163281632816328

16328163281632816328163281632816328

16328163281632816328163281632816328

16328163281632816328163281632816328

1632816330163301633016330163301633016330

16330163301633016330163301633016330

16330163301633016330163301633016330

163301633016330163301633016330

16330163301633016330163301633016330

16330163301633016330163301633016330

16330163301633016330163301633016330

16330

16331163311633116331163311633116331

16331163311633116331163311633116331

16331163311633116331163311633116331

163311633116331163311633116331

16331163311633116331163311633116331

16331163311633116331163311633116331

16331163311633116331163311633116331

16331

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFML

IFMLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFL

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFL

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.032.035.5

35.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.535.535.9

35.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.935.934.7

34.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.734.737.337.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.337.3

37.337.337.337.337.337.337.337.335.8

35.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.835.8

35.835.835.835.835.835.835.835.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.835.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.635.631.0

31.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.031.0

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.136.1

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.82.12.12.12.12.12.12.1

2.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.131.9

31.931.931.931.931.931.9

31.931.931.931.931.931.931.9

31.931.931.931.931.931.931.9

31.931.931.931.931.931.9

31.931.931.931.931.931.931.9

31.931.931.931.931.931.931.9

31.931.931.931.931.931.931.931.92.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.138.0

38.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.038.0

38.038.038.038.038.038.038.038.0

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.537.5

38.538.538.538.538.538.538.5

38.538.538.538.538.538.538.5

38.538.538.538.538.538.538.5

38.538.538.538.538.538.5

38.538.538.538.538.538.538.5

38.538.538.538.538.538.538.5

38.538.538.538.538.538.538.538.532.9

32.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.932.937.4

37.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.437.4

35.235.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.235.235.2

29.429.429.429.429.429.429.4

29.429.429.429.429.429.429.4

29.429.429.429.429.429.429.4

29.429.429.429.429.429.4

29.429.429.429.429.429.429.4

29.429.429.429.429.429.429.4

29.429.429.429.429.429.429.429.4

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.230.223.2

23.223.223.223.223.223.2

23.223.223.223.223.223.223.2

23.223.223.223.223.223.223.2

23.223.223.223.223.223.2

23.223.223.223.223.223.223.2

23.223.223.223.223.223.223.2

23.223.223.223.223.223.223.223.216.7

16.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.716.7

16.716.716.716.716.716.716.716.714.7

14.714.714.714.714.714.7

14.714.714.714.714.714.714.7

14.714.714.714.714.714.714.7

14.714.714.714.714.714.7

14.714.714.714.714.714.714.7

14.714.714.714.714.714.714.7

14.714.714.714.714.714.714.714.7

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.433.4 36.3

36.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.336.345.6

45.645.645.645.645.645.6

45.645.645.645.645.645.645.6

45.645.645.645.645.645.645.6

45.645.645.645.645.645.6

45.645.645.645.645.645.645.6

45.645.645.645.645.645.645.6

45.645.645.645.645.645.645.645.646.1

46.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.146.1

36.736.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.736.736.7

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.433.4

37.037.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.037.037.045.3

45.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.345.345.352.4

52.452.452.452.452.452.4

52.452.452.452.452.452.452.4

52.452.452.452.452.452.452.4

52.452.452.452.452.452.4

52.452.452.452.452.452.452.4

52.452.452.452.452.452.452.4

52.452.452.452.452.452.452.452.4

30.330.330.330.330.330.330.3

30.330.330.330.330.330.330.3

30.330.330.330.330.330.330.3

30.330.330.330.330.330.3

30.330.330.330.330.330.330.3

30.330.330.330.330.330.330.3

30.330.330.330.330.330.330.330.336.6

36.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.636.636.3

36.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.336.324.1

24.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.124.124.1

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

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GWK

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GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

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GWK

GWK

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GWK

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

GWK

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GWK

GWK

GWK

GWK

GWK

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GWK

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GWK

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GWK

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GWK

GWK

GWK

GWK

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GWK

GWK

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GWK

GWK

GW

KG

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GW

KG

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GW

KG

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GW

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WK

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GW

KG

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KG

WK

GW

K

ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030ES57-030181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m181.36m

GW

KG

WK

GW

KG

WK

GW

KG

WK

GW

KG

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GW

KG

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GW

KG

WK

GW

KG

WK

GW

KG

WK

GW

KG

WK

GW

KG

WK

GW

K

250m E

lev 350m

Elev

150m E

lev

5,644,150mN

5,644,150mN

5,644,050mN

50m E

lev

5,644,350mN

5,644,350mN

450

m E

lev

50m

Ele

v 1

50m

Ele

v 2

50m

Ele

v 3

50m

Ele

v 450m

Elev

5,644,250mN

5,644,250mN

5,644,650mN

5,644,650mN 5,644,550mN

5,644,550mN

5,644,450mN

5,644,450mN

Scale 1:1,000Section Origin (top left)543,008.72 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

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ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055ES57-055512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m512.37m

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Raytec Metals Corp.

El Sol ProjectA Zone

Section E543008

Scale: 1:1000

0 25

metres

50

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

IFMJ

IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

Quartz Porphyry

Granitic Dyke

Biotite dyke

GD

QP

CASCasing

OVEROverburden

BD

Legend

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IFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLMIFLM

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3.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.7

3.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.6

3.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.93.9

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4.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.1

32.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.7

4.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.1

9.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.2

31.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.931.935.335.335.335.335.335.335.3

35.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.334.134.134.134.134.134.134.1

34.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.1

36.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.836.8

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3.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.48.38.38.38.38.38.38.3

8.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.330.2

30.230.230.230.230.230.2

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35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.035.0

24.624.624.624.624.624.624.6

24.624.624.624.624.624.624.6

24.624.624.624.624.624.624.6

24.624.624.624.624.624.6

24.624.624.624.624.624.624.6

24.624.624.624.624.624.624.6

24.624.624.624.624.624.624.624.628.1

28.128.128.128.128.128.1

28.128.128.128.128.128.128.1

28.128.128.128.128.128.128.1

28.128.128.128.128.128.1

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28.128.128.128.128.128.128.1

28.128.128.128.128.128.128.128.129.5

29.529.529.529.529.529.5

29.529.529.529.529.529.529.5

29.529.529.529.529.529.529.5

29.529.529.529.529.529.5

29.529.529.529.529.529.529.5

29.529.529.529.529.529.529.5

29.529.529.529.529.529.529.529.533.5

33.533.533.533.533.533.5

33.533.533.533.533.533.533.5

33.533.533.533.533.533.533.5

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33.533.533.533.533.533.533.5

33.533.533.533.533.533.533.533.532.0

32.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.032.0

33.233.233.233.233.233.233.2

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33.233.233.233.233.233.233.2

33.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.233.2

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34.534.534.534.534.534.5

34.534.534.534.534.534.534.5

34.534.534.534.534.534.534.5

34.534.534.534.534.534.534.534.525.4

25.425.425.425.425.425.4

25.425.425.425.425.425.425.4

25.425.425.425.425.425.425.4

25.425.425.425.425.425.4

25.425.425.425.425.425.425.4

25.425.425.425.425.425.425.4

25.425.425.425.425.425.425.425.43.23.23.23.23.23.23.2

3.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.23.2

0.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.5

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

0.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.4

0.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.5

0.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.60.6

0.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.5

1.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.6

59.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.959.9

38.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.938.943.143.143.143.143.143.143.1

43.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.143.146.946.946.946.946.946.946.9

46.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.946.846.846.846.846.846.846.8

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46.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.4

38.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.439.639.639.639.639.639.639.6

39.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.639.646.546.546.546.546.546.546.5

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0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.70.70.70.70.70.70.7

0.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.739.9

39.939.939.939.939.939.9

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39.939.939.939.939.939.939.9

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39.939.939.939.939.939.939.9

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48.748.748.748.748.748.748.748.750.5

50.550.550.550.550.550.5

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46.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.446.4

48.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.348.3

55.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.455.4

36.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.2

35.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.5

33.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.733.735.635.635.635.635.635.635.6

35.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.6

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36.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.436.4

31.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.539.839.839.839.839.839.839.8

39.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.839.8

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.146.146.146.146.146.146.146.1

46.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.146.746.746.746.746.746.746.7

46.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.746.7

51.751.751.751.751.751.751.7

51.751.751.751.751.751.751.7

51.751.751.751.751.751.751.7

51.751.751.751.751.751.7

51.751.751.751.751.751.751.7

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51.751.751.751.751.751.751.751.7

47.847.847.847.847.847.847.8

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47.847.847.847.847.847.847.847.842.6

42.642.642.642.642.642.6

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42.642.642.642.642.642.642.642.642.3

42.342.342.342.342.342.3

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42.342.342.342.342.342.342.342.3

49.549.549.549.549.549.549.5

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49.549.549.549.549.549.549.549.5

2.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.2

2.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.034.334.334.334.334.334.334.3

34.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.334.333.833.833.833.833.833.833.8

33.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.833.8

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50.950.950.950.950.950.950.9

50.950.950.950.950.950.950.9

50.950.950.950.950.950.950.9

50.950.950.950.950.950.9

50.950.950.950.950.950.950.9

50.950.950.950.950.950.950.9

50.950.950.950.950.950.950.950.9

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.348.347.6

47.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.647.647.6

47.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.647.643.343.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.343.343.3

36.836.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.836.836.8

16263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263162631626316263

25.625.625.625.625.625.625.6

25.625.625.625.625.625.625.6

25.625.625.625.625.625.625.6

25.625.625.625.625.625.6

25.625.625.625.625.625.625.6

25.625.625.625.625.625.625.6

25.625.625.625.625.625.625.625.6

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.3

48.348.348.348.348.348.348.348.316.9

16.916.916.916.916.916.9

16.916.916.916.916.916.916.9

16.916.916.916.916.916.916.9

16.916.916.916.916.916.9

16.916.916.916.916.916.916.9

16.916.916.916.916.916.916.9

16.916.916.916.916.916.916.916.91.41.41.41.41.41.41.4

1.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.4

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.334.3

41.441.441.441.441.441.441.4

41.441.441.441.441.441.441.4

41.441.441.441.441.441.441.4

41.441.441.441.441.441.4

41.441.441.441.441.441.441.4

41.441.441.441.441.441.441.4

41.441.441.441.441.441.441.441.4

32.232.232.232.232.232.232.2

32.232.232.232.232.232.232.2

32.232.232.232.232.232.232.2

32.232.232.232.232.232.2

32.232.232.232.232.232.232.2

32.232.232.232.232.232.232.2

32.232.232.232.232.232.232.232.233.7

33.733.733.733.733.733.7

33.733.733.733.733.733.733.7

33.733.733.733.733.733.733.7

33.733.733.733.733.733.7

33.733.733.733.733.733.733.7

33.733.733.733.733.733.733.7

33.733.733.733.733.733.733.733.739.1

39.139.139.139.139.139.1

39.139.139.139.139.139.139.1

39.139.139.139.139.139.139.1

39.139.139.139.139.139.1

39.139.139.139.139.139.139.1

39.139.139.139.139.139.139.1

39.139.139.139.139.139.139.139.145.0

45.045.045.045.045.045.0

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45.045.045.045.045.045.045.0

45.045.045.045.045.045.0

45.045.045.045.045.045.045.0

45.045.045.045.045.045.045.0

45.045.045.045.045.045.045.045.0

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.4

38.438.438.438.438.438.438.438.421.3

21.321.321.321.321.321.3

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21.321.321.321.321.321.3

21.321.321.321.321.321.321.3

21.321.321.321.321.321.321.3

21.321.321.321.321.321.321.321.30.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

43.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.943.9

35.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.7

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

49.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.2

51.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.051.025.525.525.525.525.525.525.5

25.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.525.512.712.712.712.712.712.712.7

12.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.712.7

2.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.92.9

2.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.0

0.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.8

37.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.4

37.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.437.423.223.223.223.223.223.223.2

23.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.223.218.818.818.818.818.818.818.8

18.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.818.8

10.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.710.7

17.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.617.6

15.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.415.4 7.37.37.37.37.37.37.3

7.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.3

21.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.321.3

46.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.6

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23.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.923.9

33.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.433.4

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0.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.7

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

49.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.949.9

17.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.117.1

14.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.8

2.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.0

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

38.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.438.4

33.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.033.0

36.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.036.0

2.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.2

33.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.220.920.920.920.920.920.920.9

20.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.920.9

4.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.84.8

16.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.416.4

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

2.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.0

2.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.12.1

1628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016280162801628016281

162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281162811628116281

ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m

16282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282162821628216282

IFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFML

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

GWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWK

PGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPG

1628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416284162841628416285

162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285162851628516285

150m E

lev 50m

Elev

5,644,150mN

5,644,150mN

5,644,050mN

5,644,250mN

5,644,350mN

5,644,350mN

5,644,250mN

250m E

lev

5,644,550mN 5,644,650mN

5,644,650mN

350

m E

lev

350m E

lev 4

50m

Ele

v 450m

Elev

50m

Ele

v

5,644,550mN

5,644,450mN

5,644,450mN

150

m E

lev

250

m E

lev

Scale 1:1,000Section Origin (top left)543,317.76 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

��

ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m222m

ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m171m ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-005ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004ES08-004

Raytec Metals Corp.

El Sol ProjectA Zone

Section E543317

Scale: 1:1000

0 25

metres

50

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

IFMJ

IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

Quartz Porphyry

Granitic Dyke

Biotite dyke

GD

QP

CASCasing

OVEROverburden

BD

Legend

QVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQVQV

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

0.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.50.5

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.20.20.20.20.20.20.2

0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.2

16289

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16289

16289

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1628916289

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1628916308

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1630816308

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1630816308

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1630816308

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16308

16308

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16308

1630816327

16327

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1632716327

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1632716327

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16327

16327

1632716327

16327

16327

16327

16327

16327

1632716327

16327

16327

16327

16327

16327

16327

163270.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.4

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

5.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.55.525.0

25.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.025.0

25.025.025.025.025.025.025.025.032.5

32.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.532.532.546.446.446.446.446.446.446.4

46.446.446.446.446.446.446.4

46.446.446.446.446.446.446.4

46.446.446.446.446.446.4

46.446.446.446.446.446.446.4

46.446.446.446.446.446.446.4

46.446.446.446.446.446.446.446.448.2

48.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.248.2

16579

16579

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1657916579

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1658016580

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1658016580

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1658016580

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1658016580

16580

16580

16580

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16580

1658016580

16580

16580

16580

16580

16580

16580

16580

49.249.249.249.249.249.249.2

49.249.249.249.249.249.249.2

49.249.249.249.249.249.249.2

49.249.249.249.249.249.2

49.249.249.249.249.249.249.2

49.249.249.249.249.249.249.2

49.249.249.249.249.249.249.249.2

41.341.341.341.341.341.341.3

41.341.341.341.341.341.341.3

41.341.341.341.341.341.341.3

41.341.341.341.341.341.3

41.341.341.341.341.341.341.3

41.341.341.341.341.341.341.3

41.341.341.341.341.341.341.341.3

24.724.724.724.724.724.724.7

24.724.724.724.724.724.724.7

24.724.724.724.724.724.724.7

24.724.724.724.724.724.7

24.724.724.724.724.724.724.7

24.724.724.724.724.724.724.7

24.724.724.724.724.724.724.724.743.9

43.943.943.943.943.943.9

43.943.943.943.943.943.943.9

43.943.943.943.943.943.943.9

43.943.943.943.943.943.9

43.943.943.943.943.943.943.9

43.943.943.943.943.943.943.9

43.943.943.943.943.943.943.943.9

16582

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1658116584165841658416584165841658416584

16584165841658416584165841658416584

16584165841658416584165841658416584

165841658416584165841658416584

16584165841658416584165841658416584

16584165841658416584165841658416584

16584165841658416584165841658416584

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16585165851658516585165851658516585

16585165851658516585165851658516585

16585165851658516585165851658516585

165851658516585165851658516585

16585165851658516585165851658516585

16585165851658516585165851658516585

16585165851658516585165851658516585

16585

16586165861658616586165861658616586

16586165861658616586165861658616586

16586165861658616586165861658616586

165861658616586165861658616586

16586165861658616586165861658616586

16586165861658616586165861658616586

16586165861658616586165861658616586

16586

4.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.3

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.2

48.248.248.248.248.248.248.248.28.88.88.88.88.88.88.8

8.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.88.8

16420

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1642016420

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16420

16420

16420

16420

16420

1642016344

16344

16344

16344

16344

16344

1634416344

16344

16344

16344

16344

16344

1634416344

16344

16344

16344

16344

16344

1634416344

16344

16344

16344

16344

1634416344

16344

16344

16344

16344

16344

1634416344

16344

16344

16344

16344

16344

1634416344

16344

16344

16344

16344

16344

16344

1634416402

16402

16402

16402

16402

16402

1640216402

16402

16402

16402

16402

16402

1640216402

16402

16402

16402

16402

16402

1640216402

16402

16402

16402

16402

1640216402

16402

16402

16402

16402

16402

1640216402

16402

16402

16402

16402

16402

1640216402

16402

16402

16402

16402

16402

16402

16402

16587165871658716587165871658716587

16587165871658716587165871658716587

16587165871658716587165871658716587

165871658716587165871658716587

16587165871658716587165871658716587

16587165871658716587165871658716587

16587165871658716587165871658716587

16587

16588165881658816588165881658816588

16588165881658816588165881658816588

16588165881658816588165881658816588

165881658816588165881658816588

16588165881658816588165881658816588

16588165881658816588165881658816588

16588165881658816588165881658816588

16588

16589165891658916589165891658916589

16589165891658916589165891658916589

16589165891658916589165891658916589

165891658916589165891658916589

16589165891658916589165891658916589

16589165891658916589165891658916589

16589165891658916589165891658916589

16589

16591165911659116591165911659116591

16591165911659116591165911659116591

16591165911659116591165911659116591

165911659116591165911659116591

16591165911659116591165911659116591

16591165911659116591165911659116591

16591165911659116591165911659116591

16591

16592165921659216592165921659216592

16592165921659216592165921659216592

16592165921659216592165921659216592

165921659216592165921659216592

16592165921659216592165921659216592

16592165921659216592165921659216592

16592165921659216592165921659216592

16592

16593165931659316593165931659316593

16593165931659316593165931659316593

16593165931659316593165931659316593

165931659316593165931659316593

16593165931659316593165931659316593

16593165931659316593165931659316593

16593165931659316593165931659316593

16593

16594165941659416594165941659416594

16594165941659416594165941659416594

16594165941659416594165941659416594

165941659416594165941659416594

16594165941659416594165941659416594

16594165941659416594165941659416594

16594165941659416594165941659416594

16594

16598165981659816598165981659816598

16598165981659816598165981659816598

16598165981659816598165981659816598

165981659816598165981659816598

16598165981659816598165981659816598

16598165981659816598165981659816598

16598165981659816598165981659816598

1659816595165951659516595165951659516595

16595165951659516595165951659516595

16595165951659516595165951659516595

165951659516595165951659516595

16595165951659516595165951659516595

16595165951659516595165951659516595

16595165951659516595165951659516595

16595

16596165961659616596165961659616596

16596165961659616596165961659616596

16596165961659616596165961659616596

165961659616596165961659616596

16596165961659616596165961659616596

16596165961659616596165961659616596

16596165961659616596165961659616596

16596

16597165971659716597165971659716597

16597165971659716597165971659716597

16597165971659716597165971659716597

165971659716597165971659716597

16597165971659716597165971659716597

16597165971659716597165971659716597

16597165971659716597165971659716597

1659716600166001660016600166001660016600

16600166001660016600166001660016600

16600166001660016600166001660016600

166001660016600166001660016600

16600166001660016600166001660016600

16600166001660016600166001660016600

16600166001660016600166001660016600

16600

16201162011620116201162011620116201

16201162011620116201162011620116201

16201162011620116201162011620116201

162011620116201162011620116201

16201162011620116201162011620116201

16201162011620116201162011620116201

16201162011620116201162011620116201

16201ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054ES57-054149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m149.05m

CON

GCO

NG

CON

GCO

NG

CON

GCO

NG

CON

GCO

NG

CON

GCO

NG

CON

GCO

NG

CON

GCO

NG

CON

GCO

NG

CON

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NG

CON

GCO

NG

CON

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NG

CON

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CON

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NG

CON

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NG

CON

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NG

CON

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NG

CON

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NG

CON

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NG

CON

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NG

CON

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NG

CON

GCO

NG

CON

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NG

CON

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NG

CON

GCO

NG

CON

G

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVEROVEROVEROVEROVEROVEROVER

OVER

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES08-0

03

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

ES57-0

54

CASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCAS

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

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GWK

GWK

GWK

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GWK

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GWK

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GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

4.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.04.54.54.54.54.54.54.5

4.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.94.94.94.94.94.94.9

4.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.94.93.73.73.73.73.73.73.7

3.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.74.24.24.24.24.24.24.2

4.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.14.14.14.14.14.14.1

4.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.14.1

4.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.7

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.4

33.433.433.433.433.433.433.433.4

16.016.016.016.016.016.016.0

16.016.016.016.016.016.016.0

16.016.016.016.016.016.016.0

16.016.016.016.016.016.0

16.016.016.016.016.016.016.0

16.016.016.016.016.016.016.0

16.016.016.016.016.016.016.016.025.7

25.725.725.725.725.725.7

25.725.725.725.725.725.725.7

25.725.725.725.725.725.725.7

25.725.725.725.725.725.7

25.725.725.725.725.725.725.7

25.725.725.725.725.725.725.7

25.725.725.725.725.725.725.725.734.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.835.1

35.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.135.1

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.932.936.2

36.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.236.2

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

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IFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFMLIFML

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20.720.720.720.720.720.720.7

20.720.720.720.720.720.720.7

20.720.720.720.720.720.720.7

20.720.720.720.720.720.7

20.720.720.720.720.720.720.7

20.720.720.720.720.720.720.7

20.720.720.720.720.720.720.720.732.4

32.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.432.432.436.4

36.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.436.4

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

17.517.517.517.517.517.517.5

17.517.517.517.517.517.517.5

17.517.517.517.517.517.517.5

17.517.517.517.517.517.5

17.517.517.517.517.517.517.5

17.517.517.517.517.517.517.5

17.517.517.517.517.517.517.517.515.3

15.315.315.315.315.315.3

15.315.315.315.315.315.315.3

15.315.315.315.315.315.315.3

15.315.315.315.315.315.3

15.315.315.315.315.315.315.3

15.315.315.315.315.315.315.3

15.315.315.315.315.315.315.315.3

47.447.447.447.447.447.447.4

47.447.447.447.447.447.447.4

47.447.447.447.447.447.447.4

47.447.447.447.447.447.4

47.447.447.447.447.447.447.4

47.447.447.447.447.447.447.4

47.447.447.447.447.447.447.447.4

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.934.936.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.036.0 45.5

45.545.545.545.545.545.5

45.545.545.545.545.545.545.5

45.545.545.545.545.545.545.5

45.545.545.545.545.545.5

45.545.545.545.545.545.545.5

45.545.545.545.545.545.545.5

45.545.545.545.545.545.545.545.5

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.4

49.449.449.449.449.449.449.449.442.242.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.242.242.244.4

44.444.444.444.444.444.4

44.444.444.444.444.444.444.4

44.444.444.444.444.444.444.4

44.444.444.444.444.444.4

44.444.444.444.444.444.444.4

44.444.444.444.444.444.444.4

44.444.444.444.444.444.444.444.4

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

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32.232.232.232.232.232.232.2

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32.232.232.232.232.232.232.2

32.232.232.232.232.232.232.2

32.232.232.232.232.232.232.232.2

39.539.539.539.539.539.539.5

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33.733.733.733.733.733.733.7

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0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.313.5

13.513.513.513.513.513.5

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21.421.421.421.421.421.4

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21.421.421.421.421.421.421.421.4

40.140.140.140.140.140.140.1

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16.216.216.216.216.216.216.2

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16.216.216.216.216.216.216.2

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16.216.216.216.216.216.216.216.231.8

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31.731.731.731.731.731.7

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3.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.43.4

39.539.539.539.539.539.539.5

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39.539.539.539.539.539.539.539.520.1

20.120.120.120.120.120.1

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20.120.120.120.120.120.120.120.131.1

31.131.131.131.131.131.1

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1.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

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250m E

lev 350m

Elev

150m E

lev

5,644,150mN

5,644,150mN

5,644,050mN

50m E

lev

5,644,350mN

5,644,350mN

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5,644,250mN

5,644,650mN

5,644,650mN 5,644,550mN

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5,644,450mN

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Scale 1:1,000Section Origin (top left)543,624.33 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

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Raytec Metals Corp.

El Sol ProjectA Zone

Section E543624

0 25

metres

50

Scale: 1:1000

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

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IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

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Biotite dyke

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01

ES08-0

01

ES08-0

01

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01

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01

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01

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01

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01

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01

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01

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01

ES08-0

01

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01

ES08-0

01

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01

ES08-0

01

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01

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01

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01

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01

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01

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01

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01

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01

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01

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01

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01

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01

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01

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01

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

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02

ES08-0

02

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02

ES08-0

02

ES08-0

02

ES08-0

02

ES08-0

02

ES08-0

02

ES08-0

02

ES08-0

02

CASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASOVER

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

CASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCAS

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

PGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPG

GWK

GWK

GWK

GWK

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GWK

GWK

GWK

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GWK

GWK

GWK

GWK

GWK

GWK

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GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

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GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

PGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPG

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

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53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

ES57-0

53

0.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.4

GWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWKGWK

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.40.40.40.40.40.40.4

0.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.4

0.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.4

4.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.44.43.63.63.63.63.63.63.6

3.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.6 0.80.80.80.80.80.80.8

0.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.8

3.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.63.63.63.63.63.63.6

3.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.63.6

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.9

23.923.923.923.923.923.923.923.9

13.713.713.713.713.713.713.7

13.713.713.713.713.713.713.7

13.713.713.713.713.713.713.7

13.713.713.713.713.713.7

13.713.713.713.713.713.713.7

13.713.713.713.713.713.713.7

13.713.713.713.713.713.713.713.7

4.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.24.26.96.96.96.96.96.96.9

6.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.96.9

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.03.73.73.73.73.73.73.7

3.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.73.7

43.343.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.343.3

43.343.343.343.343.343.343.343.3

16551165511655116551165511655116551

16551165511655116551165511655116551

16551165511655116551165511655116551

165511655116551165511655116551

16551165511655116551165511655116551

16551165511655116551165511655116551

16551165511655116551165511655116551

1655116512165121651216512165121651216512

16512165121651216512165121651216512

16512165121651216512165121651216512

165121651216512165121651216512

16512165121651216512165121651216512

16512165121651216512165121651216512

16512165121651216512165121651216512

16512

16537165371653716537165371653716537

16537165371653716537165371653716537

16537165371653716537165371653716537

165371653716537165371653716537

16537165371653716537165371653716537

16537165371653716537165371653716537

16537165371653716537165371653716537

1653716573165731657316573165731657316573

16573165731657316573165731657316573

16573165731657316573165731657316573

165731657316573165731657316573

16573165731657316573165731657316573

16573165731657316573165731657316573

16573165731657316573165731657316573

1657323.423.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.423.423.432.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.0

32.032.032.032.032.032.032.032.034.6

34.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.6

34.634.634.634.634.634.634.634.6

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.1

46.146.146.146.146.146.146.146.1

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1650316502165021650216502165021650216502

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165021650216502165021650216502

16502165021650216502165021650216502

16502165021650216502165021650216502

16502165021650216502165021650216502

16502

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

16590165901659016590165901659016590

16590165901659016590165901659016590

16590165901659016590165901659016590

165901659016590165901659016590

16590165901659016590165901659016590

16590165901659016590165901659016590

16590165901659016590165901659016590

16590

16501165011650116501165011650116501

16501165011650116501165011650116501

16501165011650116501165011650116501

165011650116501165011650116501

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16501165011650116501165011650116501

16501165011650116501165011650116501

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35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.635.6

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.2

33.233.233.233.233.233.233.233.2

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16506165061650616506165061650616506

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16504

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16507165071650716507165071650716507

16507165071650716507165071650716507

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RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

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16508165081650816508165081650816508

16508165081650816508165081650816508

16508

16509165091650916509165091650916509

16509165091650916509165091650916509

16509165091650916509165091650916509

165091650916509165091650916509

16509165091650916509165091650916509

16509165091650916509165091650916509

16509165091650916509165091650916509

16509

16510165101651016510165101651016510

16510165101651016510165101651016510

16510165101651016510165101651016510

165101651016510165101651016510

16510165101651016510165101651016510

16510165101651016510165101651016510

16510165101651016510165101651016510

16510

16511165111651116511165111651116511

16511165111651116511165111651116511

16511165111651116511165111651116511

165111651116511165111651116511

16511165111651116511165111651116511

16511165111651116511165111651116511

16511165111651116511165111651116511

16511RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

4.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.34.3

0.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.8

1.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.11.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

4.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.64.6

3.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.5

3.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.83.8

13.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.513.510.0

10.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.010.025.2

25.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.225.229.5

29.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.529.5

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.122.2

22.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.222.227.2

27.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.227.2

29.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.729.7

1.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.41.4

41.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.941.9

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162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271162711627116271

32.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.432.4

9.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.79.7

24.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.524.5

49.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.249.2

34.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.434.4

45.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.645.6

2.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.72.748.1

48.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.148.6

48.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.648.6

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35.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.79.29.29.29.29.29.29.2

9.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.29.2

35.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.7

37.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.337.336.6

36.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.636.6

47.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.3

38.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.538.534.1

34.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.134.131.5

31.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.531.5

52.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.752.746.6

46.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.646.640.6

40.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.640.626.4

26.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.426.4

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35.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.335.3

26.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.026.0

37.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.837.8

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50.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.150.142.7

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16552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216552165521655216553

16553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316553165531655316554

165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554165541655416554

38.938.938.938.938.938.938.9

38.938.938.938.938.938.938.9

38.938.938.938.938.938.938.9

38.938.938.938.938.938.9

38.938.938.938.938.938.938.9

38.938.938.938.938.938.938.9

38.938.938.938.938.938.938.938.9

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.435.4

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.036.036.5

36.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.536.536.5

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.8

45.345.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.345.3

45.345.345.345.345.345.345.345.343.1

43.143.143.143.143.143.1

43.143.143.143.143.143.143.1

43.143.143.143.143.143.143.1

43.143.143.143.143.143.1

43.143.143.143.143.143.143.1

43.143.143.143.143.143.143.1

43.143.143.143.143.143.143.143.147.6

47.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.6

47.647.647.647.647.647.647.647.6

47.147.147.147.147.147.147.1

47.147.147.147.147.147.147.1

47.147.147.147.147.147.147.1

47.147.147.147.147.147.1

47.147.147.147.147.147.147.1

47.147.147.147.147.147.147.1

47.147.147.147.147.147.147.147.140.4

40.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.440.440.4

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.3

47.347.347.347.347.347.347.347.3

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.034.035.3

35.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.335.33.53.53.53.53.53.53.5

3.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.53.52.02.02.02.02.02.02.0

2.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.0 2.02.02.02.02.02.02.0

2.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.02.00.20.20.20.20.20.20.2

0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.00.00.00.00.00.00.0

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.0

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

16513165131651316513165131651316513

16513165131651316513165131651316513

16513165131651316513165131651316513

165131651316513165131651316513

16513165131651316513165131651316513

16513165131651316513165131651316513

16513165131651316513165131651316513

16513

16514165141651416514165141651416514

16514165141651416514165141651416514

16514165141651416514165141651416514

165141651416514165141651416514

16514165141651416514165141651416514

16514165141651416514165141651416514

16514165141651416514165141651416514

16514

16515165151651516515165151651516515

16515165151651516515165151651516515

16515165151651516515165151651516515

165151651516515165151651516515

16515165151651516515165151651516515

16515165151651516515165151651516515

16515165151651516515165151651516515

16515

16516165161651616516165161651616516

16516165161651616516165161651616516

16516165161651616516165161651616516

165161651616516165161651616516

16516165161651616516165161651616516

16516165161651616516165161651616516

16516165161651616516165161651616516

16516

16517165171651716517165171651716517

16517165171651716517165171651716517

16517165171651716517165171651716517

165171651716517165171651716517

16517165171651716517165171651716517

16517165171651716517165171651716517

16517165171651716517165171651716517

16517

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.0

14.514.514.514.514.514.514.5

14.514.514.514.514.514.514.5

14.514.514.514.514.514.514.5

14.514.514.514.514.514.5

14.514.514.514.514.514.514.5

14.514.514.514.514.514.514.5

14.514.514.514.514.514.514.514.5

1.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.91.92.22.22.22.22.22.22.2

2.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.22.2

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.01.61.61.61.61.61.61.6

1.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.61.6

23.023.023.023.023.023.023.0

23.023.023.023.023.023.023.0

23.023.023.023.023.023.023.0

23.023.023.023.023.023.0

23.023.023.023.023.023.023.0

23.023.023.023.023.023.023.0

23.023.023.023.023.023.023.023.0

16522165221652216522165221652216522

16522165221652216522165221652216522

16522165221652216522165221652216522

165221652216522165221652216522

16522165221652216522165221652216522

16522165221652216522165221652216522

16522165221652216522165221652216522

16522

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

16519165191651916519165191651916519

16519165191651916519165191651916519

16519165191651916519165191651916519

165191651916519165191651916519

16519165191651916519165191651916519

16519165191651916519165191651916519

16519165191651916519165191651916519

16519

16520165201652016520165201652016520

16520165201652016520165201652016520

16520165201652016520165201652016520

165201652016520165201652016520

16520165201652016520165201652016520

16520165201652016520165201652016520

16520165201652016520165201652016520

16520

16521165211652116521165211652116521

16521165211652116521165211652116521

16521165211652116521165211652116521

165211652116521165211652116521

16521165211652116521165211652116521

16521165211652116521165211652116521

16521165211652116521165211652116521

16521

5.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.024.1

24.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.124.1

24.124.124.124.124.124.124.124.129.7

29.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.729.727.1

27.127.127.127.127.127.1

27.127.127.127.127.127.127.1

27.127.127.127.127.127.127.1

27.127.127.127.127.127.1

27.127.127.127.127.127.127.1

27.127.127.127.127.127.127.1

27.127.127.127.127.127.127.127.1 32.3

32.332.332.332.332.332.3

32.332.332.332.332.332.332.3

32.332.332.332.332.332.332.3

32.332.332.332.332.332.3

32.332.332.332.332.332.332.3

32.332.332.332.332.332.332.3

32.332.332.332.332.332.332.332.332.9

32.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.9

32.932.932.932.932.932.932.932.942.6

42.642.642.642.642.642.6

42.642.642.642.642.642.642.6

42.642.642.642.642.642.642.6

42.642.642.642.642.642.6

42.642.642.642.642.642.642.6

42.642.642.642.642.642.642.6

42.642.642.642.642.642.642.642.60.20.20.20.20.20.20.2

0.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.20.2

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

16523165231652316523165231652316523

16523165231652316523165231652316523

16523165231652316523165231652316523

165231652316523165231652316523

16523165231652316523165231652316523

16523165231652316523165231652316523

16523165231652316523165231652316523

16523

16524165241652416524165241652416524

16524165241652416524165241652416524

16524165241652416524165241652416524

165241652416524165241652416524

16524165241652416524165241652416524

16524165241652416524165241652416524

16524165241652416524165241652416524

16524

16525165251652516525165251652516525

16525165251652516525165251652516525

16525165251652516525165251652516525

165251652516525165251652516525

16525165251652516525165251652516525

16525165251652516525165251652516525

16525165251652516525165251652516525

16525

4.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.74.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.734.75.35.35.35.35.35.35.3

5.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.35.3

0.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.30.3

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

PGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPG

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

GW

KG

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GW

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30.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.130.1

35.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.735.5

35.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.9

35.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.9

43.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.743.7

36.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.236.2 38.1

38.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.138.144.8

44.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.844.8

47.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.747.9

47.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.947.3

47.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.347.344.3

44.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.344.3

35.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.535.9

35.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.935.936.1

36.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.1

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3.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.33.3

16.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.616.614.8

14.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.814.8

36.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.136.17.27.27.27.27.27.27.2

7.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.27.2

34.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.034.033.2

33.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.233.229.0

29.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.029.0

40.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.340.3

27.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.927.9

28.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.928.9

42.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.842.845.2

45.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.245.2

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32.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.732.7

31.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.331.3

27.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.827.8

35.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.035.030.4

30.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.4

35.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.635.631.8

31.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.831.84.54.54.54.54.54.54.5

4.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.54.5

30.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.430.440.5

40.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.540.50.10.10.10.10.10.10.1

0.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.10.1

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16530165301653016530165301653016530

16530165301653016530165301653016530

16530165301653016530165301653016530

1653016529165291652916529165291652916529

16529165291652916529165291652916529

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16529165291652916529165291652916529

16529165291652916529165291652916529

1652916531165311653116531165311653116531

16531165311653116531165311653116531

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16531165311653116531165311653116531

16531165311653116531165311653116531

16531165311653116531165311653116531

16531

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

CONG

ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m

50m E

lev 150m

Elev

5,644,250mN 5,644,350mN

5,644,350mN

250m E

lev

5,644,050mN

5,644,250mN

5,644,150mN

5,644,150mN 5,644,550mN

5,644,450mN

5,644,450mN

350m E

lev 4

50m

Ele

v 450m

Elev

250

m E

lev

5,644,650mN

50m

Ele

v 1

50m

Ele

v 3

50m

Ele

v

5,644,550mN 5,644,650mN

Scale 1:1,000Section Origin (top left)543,883.2 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

��

�

ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m291m

ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m234m

ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m188.98m

ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-002ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001ES08-001

ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053ES57-053

Raytec Metals Corp.

El Sol ProjectA Zone

Section E543883

0 25

metres

50

Scale: 1:1000

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

IFMJ

IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

Quartz Porphyry

Granitic Dyke

Biotite dyke

GD

QP

CASCasing

OVEROverburden

BD

Legend

ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

1.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.51.5

45.5

45.5

45.5

45.5

45.5

45.5

45.545.5

45.5

45.5

45.5

45.5

45.5

45.545.5

45.5

45.5

45.5

45.5

45.5

45.545.5

45.5

45.5

45.5

45.5

45.545.5

45.5

45.5

45.5

45.5

45.5

45.545.5

45.5

45.5

45.5

45.5

45.5

45.545.5

45.5

45.5

45.5

45.5

45.5

45.5

45.5

43.4

43.4

43.4

43.4

43.4

43.4

43.443.4

43.4

43.4

43.4

43.4

43.4

43.443.4

43.4

43.4

43.4

43.4

43.4

43.443.4

43.4

43.4

43.4

43.4

43.443.4

43.4

43.4

43.4

43.4

43.4

43.443.4

43.4

43.4

43.4

43.4

43.4

43.443.4

43.4

43.4

43.4

43.4

43.4

43.4

43.4

11.8

11.8

11.8

11.8

11.8

11.8

11.811.8

11.8

11.8

11.8

11.8

11.8

11.811.8

11.8

11.8

11.8

11.8

11.8

11.811.8

11.8

11.8

11.8

11.8

11.811.8

11.8

11.8

11.8

11.8

11.8

11.811.8

11.8

11.8

11.8

11.8

11.8

11.811.8

11.8

11.8

11.8

11.8

11.8

11.8

11.8

5825

5825

5825

5825

5825

5825

58255825

5825

5825

5825

5825

5825

58255825

5825

5825

5825

5825

5825

58255825

5825

5825

5825

5825

58255825

5825

5825

5825

5825

5825

58255825

5825

5825

5825

5825

5825

58255825

5825

5825

5825

5825

5825

5825

5825

42.0

42.0

42.0

42.0

42.0

42.0

42.042.0

42.0

42.0

42.0

42.0

42.0

42.042.0

42.0

42.0

42.0

42.0

42.0

42.042.0

42.0

42.0

42.0

42.0

42.042.0

42.0

42.0

42.0

42.0

42.0

42.042.0

42.0

42.0

42.0

42.0

42.0

42.042.0

42.0

42.0

42.0

42.0

42.0

42.0

42.0

47.3

47.3

47.3

47.3

47.3

47.3

47.347.3

47.3

47.3

47.3

47.3

47.3

47.347.3

47.3

47.3

47.3

47.3

47.3

47.347.3

47.3

47.3

47.3

47.3

47.347.3

47.3

47.3

47.3

47.3

47.3

47.347.3

47.3

47.3

47.3

47.3

47.3

47.347.3

47.3

47.3

47.3

47.3

47.3

47.3

47.3

0.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.734.2

34.2

34.2

34.2

34.2

34.2

34.234.2

34.2

34.2

34.2

34.2

34.2

34.234.2

34.2

34.2

34.2

34.2

34.2

34.234.2

34.2

34.2

34.2

34.2

34.234.2

34.2

34.2

34.2

34.2

34.2

34.234.2

34.2

34.2

34.2

34.2

34.2

34.234.2

34.2

34.2

34.2

34.2

34.2

34.2

34.2

52.2

52.2

52.2

52.2

52.2

52.2

52.252.2

52.2

52.2

52.2

52.2

52.2

52.252.2

52.2

52.2

52.2

52.2

52.2

52.252.2

52.2

52.2

52.2

52.2

52.252.2

52.2

52.2

52.2

52.2

52.2

52.252.2

52.2

52.2

52.2

52.2

52.2

52.252.2

52.2

52.2

52.2

52.2

52.2

52.2

52.2

18.3

18.3

18.3

18.3

18.3

18.3

18.318.3

18.3

18.3

18.3

18.3

18.3

18.318.3

18.3

18.3

18.3

18.3

18.3

18.318.3

18.3

18.3

18.3

18.3

18.318.3

18.3

18.3

18.3

18.3

18.3

18.318.3

18.3

18.3

18.3

18.3

18.3

18.318.3

18.3

18.3

18.3

18.3

18.3

18.3

18.3

5823

5823

5823

5823

5823

5823

58235823

5823

5823

5823

5823

5823

58235823

5823

5823

5823

5823

5823

58235823

5823

5823

5823

5823

58235823

5823

5823

5823

5823

5823

58235823

5823

5823

5823

5823

5823

58235823

5823

5823

5823

5823

5823

5823

582358

2258

2258

2258

2258

2258

2258

225822

5822

5822

5822

5822

5822

58225822

5822

5822

5822

5822

5822

58225822

5822

5822

5822

5822

58225822

5822

5822

5822

5822

5822

58225822

5822

5822

5822

5822

5822

58225822

5822

5822

5822

5822

5822

5822

5822

5824

5824

5824

5824

5824

5824

58245824

5824

5824

5824

5824

5824

58245824

5824

5824

5824

5824

5824

58245824

5824

5824

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58245824

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5824

5824

5824

58245824

5824

5824

5824

5824

5824

58245824

5824

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5824

5824

5824

5824

5824

5820

5820

5820

5820

5820

5820

58205820

5820

5820

5820

5820

5820

58205820

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5820

5820

5820

5820

58205820

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58205820

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5820

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58205820

5820

5820

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58205820

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5820

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5820

5820

5820

5817

5817

5817

5817

5817

5817

58175817

5817

5817

5817

5817

5817

58175817

5817

5817

5817

5817

5817

58175817

5817

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5817

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58175817

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5817

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58175817

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5817

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58175817

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5819

5819

5819

5819

5819

5819

58195819

5819

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5819

5819

58195819

5819

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5819

5819

5819

58195819

5819

5819

5819

5819

58195819

5819

5819

5819

5819

5819

58195819

5819

5819

5819

5819

5819

58195819

5819

5819

5819

5819

5819

5819

5819

5821

5821

5821

5821

5821

5821

58215821

5821

5821

5821

5821

5821

58215821

5821

5821

5821

5821

5821

58215821

5821

5821

5821

5821

58215821

5821

5821

5821

5821

5821

58215821

5821

5821

5821

5821

5821

58215821

5821

5821

5821

5821

5821

5821

5821

5815

5815

5815

5815

5815

5815

58155815

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5815

58155815

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58155815

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58155815

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58155815

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58165816

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58165816

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5816

5816

0.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.7

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

08

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

06

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07

ES56-0

07OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVERQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.934.9

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.134.144.0

44.044.044.044.044.044.0

44.044.044.044.044.044.044.0

44.044.044.044.044.044.044.0

44.044.044.044.044.044.0

44.044.044.044.044.044.044.0

44.044.044.044.044.044.044.0

44.044.044.044.044.044.044.044.0

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.436.4QBS

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.7

29.729.729.729.729.729.729.729.737.0

37.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.037.0

37.037.037.037.037.037.037.037.034.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.833.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.933.934.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.836.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.636.637.737.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.737.7

37.737.737.737.737.737.737.737.7

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

PGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPG

20.6

20.6

20.6

20.6

20.6

20.6

20.620.6

20.6

20.6

20.6

20.6

20.6

20.620.6

20.6

20.6

20.6

20.6

20.6

20.620.6

20.6

20.6

20.6

20.6

20.620.6

20.6

20.6

20.6

20.6

20.6

20.620.6

20.6

20.6

20.6

20.6

20.6

20.620.6

20.6

20.6

20.6

20.6

20.6

20.6

20.6

14.6

14.6

14.6

14.6

14.6

14.6

14.614.6

14.6

14.6

14.6

14.6

14.6

14.614.6

14.6

14.6

14.6

14.6

14.6

14.614.6

14.6

14.6

14.6

14.6

14.614.6

14.6

14.6

14.6

14.6

14.6

14.614.6

14.6

14.6

14.6

14.6

14.6

14.614.6

14.6

14.6

14.6

14.6

14.6

14.6

14.6

37.2

37.2

37.2

37.2

37.2

37.2

37.237.2

37.2

37.2

37.2

37.2

37.2

37.237.2

37.2

37.2

37.2

37.2

37.2

37.237.2

37.2

37.2

37.2

37.2

37.237.2

37.2

37.2

37.2

37.2

37.2

37.237.2

37.2

37.2

37.2

37.2

37.2

37.237.2

37.2

37.2

37.2

37.2

37.2

37.2

37.2

36.3

36.3

36.3

36.3

36.3

36.3

36.336.3

36.3

36.3

36.3

36.3

36.3

36.336.3

36.3

36.3

36.3

36.3

36.3

36.336.3

36.3

36.3

36.3

36.3

36.336.3

36.3

36.3

36.3

36.3

36.3

36.336.3

36.3

36.3

36.3

36.3

36.3

36.336.3

36.3

36.3

36.3

36.3

36.3

36.3

36.3

5.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.05.0

37.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.037.0

37.0

37.0

37.0

37.0

37.0

37.0

37.0

39.2

39.2

39.2

39.2

39.2

39.2

39.239.2

39.2

39.2

39.2

39.2

39.2

39.239.2

39.2

39.2

39.2

39.2

39.2

39.239.2

39.2

39.2

39.2

39.2

39.239.2

39.2

39.2

39.2

39.2

39.2

39.239.2

39.2

39.2

39.2

39.2

39.2

39.239.2

39.2

39.2

39.2

39.2

39.2

39.2

39.2

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

IFLM

IFLM

IFLM

IFLM

IFLM

IFLM

IFLMIFLM

IFLM

IFLM

IFLM

IFLM

IFLM

IFLMIFLM

IFLM

IFLM

IFLM

IFLM

IFLM

IFLMIFLM

IFLM

IFLM

IFLM

IFLM

IFLMIFLM

IFLM

IFLM

IFLM

IFLM

IFLM

IFLMIFLM

IFLM

IFLM

IFLM

IFLM

IFLM

IFLMIFLM

IFLM

IFLM

IFLM

IFLM

IFLM

IFLMIFLM

QPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQPQP

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

IFMJ

8.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.78.735.3

35.3

35.3

35.3

35.3

35.3

35.335.3

35.3

35.3

35.3

35.3

35.3

35.335.3

35.3

35.3

35.3

35.3

35.3

35.335.3

35.3

35.3

35.3

35.3

35.335.3

35.3

35.3

35.3

35.3

35.3

35.335.3

35.3

35.3

35.3

35.3

35.3

35.335.3

35.3

35.3

35.3

35.3

35.3

35.3

35.3

36.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.236.2

36.2

36.2

36.2

36.2

36.2

36.2

36.2

IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

27.0

27.0

27.0

27.0

27.0

27.0

27.027.0

27.0

27.0

27.0

27.0

27.0

27.027.0

27.0

27.0

27.0

27.0

27.0

27.027.0

27.0

27.0

27.0

27.0

27.027.0

27.0

27.0

27.0

27.0

27.0

27.027.0

27.0

27.0

27.0

27.0

27.0

27.027.0

27.0

27.0

27.0

27.0

27.0

27.0

27.0

24.7

24.7

24.7

24.7

24.7

24.7

24.724.7

24.7

24.7

24.7

24.7

24.7

24.724.7

24.7

24.7

24.7

24.7

24.7

24.724.7

24.7

24.7

24.7

24.7

24.724.7

24.7

24.7

24.7

24.7

24.7

24.724.7

24.7

24.7

24.7

24.7

24.7

24.724.7

24.7

24.7

24.7

24.7

24.7

24.7

24.7

7.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.67.6

23.1

23.1

23.1

23.1

23.1

23.1

23.123.1

23.1

23.1

23.1

23.1

23.1

23.123.1

23.1

23.1

23.1

23.1

23.1

23.123.1

23.1

23.1

23.1

23.1

23.123.1

23.1

23.1

23.1

23.1

23.1

23.123.1

23.1

23.1

23.1

23.1

23.1

23.123.1

23.1

23.1

23.1

23.1

23.1

23.1

23.1

25.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.425.4

25.4

25.4

25.4

25.4

25.4

25.4

25.4

6.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.56.58.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.38.3

0.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.70.725

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.425

.4

16.2

16.2

16.2

16.2

16.2

16.2

16.216.2

16.2

16.2

16.2

16.2

16.2

16.216.2

16.2

16.2

16.2

16.2

16.2

16.216.2

16.2

16.2

16.2

16.2

16.216.2

16.2

16.2

16.2

16.2

16.2

16.216.2

16.2

16.2

16.2

16.2

16.2

16.216.2

16.2

16.2

16.2

16.2

16.2

16.2

16.2

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.4

36.436.436.436.436.436.436.436.435.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.635.637.837.837.837.837.837.837.8

37.837.837.837.837.837.837.8

37.837.837.837.837.837.837.8

37.837.837.837.837.837.8

37.837.837.837.837.837.837.8

37.837.837.837.837.837.837.8

37.837.837.837.837.837.837.837.8

5811

5811

5811

5811

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58115811

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36.536.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.536.5

36.536.536.536.536.536.536.536.5

40.440.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.440.4

40.440.440.440.440.440.440.440.432.4

32.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.432.4

32.432.432.432.432.432.432.432.435.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.535.536.736.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.736.7

36.736.736.736.736.736.736.736.7

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

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34.434.434.434.434.434.434.4

34.434.434.434.434.434.434.4

34.434.434.434.434.434.434.4

34.434.434.434.434.434.4

34.434.434.434.434.434.434.4

34.434.434.434.434.434.434.4

34.434.434.434.434.434.434.434.436.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.0

36.036.036.036.036.036.036.036.035.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.935.929.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.8

29.829.829.829.829.829.829.829.8

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31.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.031.0

21.821.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.821.821.8

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.3

34.334.334.334.334.334.334.334.3IFM

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28.928.928.928.928.928.928.9

28.928.928.928.928.928.928.9

28.928.928.928.928.928.928.9

28.928.928.928.928.928.9

28.928.928.928.928.928.928.9

28.928.928.928.928.928.928.9

28.928.928.928.928.928.928.928.9

23.823.823.823.823.823.823.8

23.823.823.823.823.823.823.8

23.823.823.823.823.823.823.8

23.823.823.823.823.823.8

23.823.823.823.823.823.823.8

23.823.823.823.823.823.823.8

23.823.823.823.823.823.823.823.825.9

25.925.925.925.925.925.9

25.925.925.925.925.925.925.9

25.925.925.925.925.925.925.9

25.925.925.925.925.925.9

25.925.925.925.925.925.925.9

25.925.925.925.925.925.925.9

25.925.925.925.925.925.925.925.932.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.8

32.832.832.832.832.832.832.832.816.516.516.516.516.516.516.5

16.516.516.516.516.516.516.5

16.516.516.516.516.516.516.5

16.516.516.516.516.516.5

16.516.516.516.516.516.516.5

16.516.516.516.516.516.516.5

16.516.516.516.516.516.516.516.5

23.423.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.423.4

23.423.423.423.423.423.423.423.4

ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-00692.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m

26.226.226.226.226.226.226.2

26.226.226.226.226.226.226.2

26.226.226.226.226.226.226.2

26.226.226.226.226.226.2

26.226.226.226.226.226.226.2

26.226.226.226.226.226.226.2

26.226.226.226.226.226.226.226.2

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19.819.819.819.819.819.819.8

19.819.819.819.819.819.819.8

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19.819.819.819.819.819.819.819.8

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ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-00792.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m

IFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFL

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30.730.730.730.730.730.730.7

30.730.730.730.730.730.730.7

30.730.730.730.730.730.730.7

30.730.730.730.730.730.7

30.730.730.730.730.730.730.7

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30.730.730.730.730.730.730.730.728.5

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ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m

CONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONGCONG

CONG

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50m E

lev 150m

Elev

5,644,250mN 5,644,350mN

5,644,350mN

250m E

lev

5,644,050mN

5,644,250mN

5,644,150mN

5,644,150mN 5,644,550mN

5,644,450mN

5,644,450mN

350m E

lev 4

50m

Ele

v 450m

Elev

250

m E

lev

5,644,650mN

50m

Ele

v 1

50m

Ele

v 3

50m

Ele

v

5,644,550mN 5,644,650mN

Scale 1:1,000Section Origin (top left)540,810 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

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ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007

ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-006ES56-00692.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m92.96m

ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-007ES56-00792.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m92.05m

ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m

ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008ES56-008

ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186m186mES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011ES08-011

Raytec Metals Corp.

El Sol ProjectA Zone

Section E540810

0 25

metres

50

Scale: 1:1000

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

IFMJ

IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

Quartz Porphyry

Granitic Dyke

Biotite dyke

GD

QP

CASCasing

OVEROverburden

BD

Legend

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QBS

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199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m

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RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

IFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJIFMJ

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

RMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRMRM

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

PGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPG

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES08-0

09

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

ES56-0

22

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

ARG

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

GWK

PGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPGPG

QBS

QBS

QBS

QBS

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QBS

QBS

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QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

QBS

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23

ES56-0

23 CASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASCASOVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m

QBS

QBS

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QBS

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.5

41.541.541.541.541.541.541.541.5

41.841.841.841.841.841.841.8

41.841.841.841.841.841.841.8

41.841.841.841.841.841.841.8

41.841.841.841.841.841.8

41.841.841.841.841.841.841.8

41.841.841.841.841.841.841.8

41.841.841.841.841.841.841.841.8

6.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.16.132.6

32.632.632.632.632.632.6

32.632.632.632.632.632.632.6

32.632.632.632.632.632.632.6

32.632.632.632.632.632.6

32.632.632.632.632.632.632.6

32.632.632.632.632.632.632.6

32.632.632.632.632.632.632.632.635.9

35.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.9

35.935.935.935.935.935.935.935.9

0.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.0

39.039.039.039.039.039.039.0

39.039.039.039.039.039.039.0

39.039.039.039.039.039.039.0

39.039.039.039.039.039.0

39.039.039.039.039.039.039.0

39.039.039.039.039.039.039.0

39.039.039.039.039.039.039.039.044.9

44.944.944.944.944.944.9

44.944.944.944.944.944.944.9

44.944.944.944.944.944.944.9

44.944.944.944.944.944.9

44.944.944.944.944.944.944.9

44.944.944.944.944.944.944.9

44.944.944.944.944.944.944.944.9

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.535.5

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.637.6

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.9

34.934.934.934.934.934.934.934.9

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.636.6

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.8

34.834.834.834.834.834.834.834.8 39.3

39.339.339.339.339.339.3

39.339.339.339.339.339.339.3

39.339.339.339.339.339.339.3

39.339.339.339.339.339.3

39.339.339.339.339.339.339.3

39.339.339.339.339.339.339.3

39.339.339.339.339.339.339.339.349.1

49.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.149.146.0

46.046.046.046.046.046.0

46.046.046.046.046.046.046.0

46.046.046.046.046.046.046.0

46.046.046.046.046.046.0

46.046.046.046.046.046.046.0

46.046.046.046.046.046.046.0

46.046.046.046.046.046.046.046.051.5

51.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.551.551.5

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16444164441644416444164441644416444

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16444164441644416444164441644416444

16444164441644416444164441644416444

16444164441644416444164441644416444

1644416443164431644316443164431644316443

16443164431644316443164431644316443

16443164431644316443164431644316443

164431644316443164431644316443

16443164431644316443164431644316443

16443164431644316443164431644316443

16443164431644316443164431644316443

1644316445164451644516445164451644516445

16445164451644516445164451644516445

16445164451644516445164451644516445

164451644516445164451644516445

16445164451644516445164451644516445

16445164451644516445164451644516445

16445164451644516445164451644516445

16445

16446164461644616446164461644616446

16446164461644616446164461644616446

16446164461644616446164461644616446

164461644616446164461644616446

16446164461644616446164461644616446

16446164461644616446164461644616446

16446164461644616446164461644616446

16446

16448164481644816448164481644816448

16448164481644816448164481644816448

16448164481644816448164481644816448

164481644816448164481644816448

16448164481644816448164481644816448

16448164481644816448164481644816448

16448164481644816448164481644816448

16448

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16449164491644916449164491644916449

16449164491644916449164491644916449

16449164491644916449164491644916449

164491644916449164491644916449

16449164491644916449164491644916449

16449164491644916449164491644916449

16449164491644916449164491644916449

16449

16450164501645016450164501645016450

16450164501645016450164501645016450

16450164501645016450164501645016450

164501645016450164501645016450

16450164501645016450164501645016450

16450164501645016450164501645016450

16450164501645016450164501645016450

16450ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

16453164531645316453164531645316453

16453164531645316453164531645316453

16453164531645316453164531645316453

164531645316453164531645316453

16453164531645316453164531645316453

16453164531645316453164531645316453

16453164531645316453164531645316453

1645316451164511645116451164511645116451

16451164511645116451164511645116451

16451164511645116451164511645116451

164511645116451164511645116451

16451164511645116451164511645116451

16451164511645116451164511645116451

16451164511645116451164511645116451

16451

16452164521645216452164521645216452

16452164521645216452164521645216452

16452164521645216452164521645216452

164521645216452164521645216452

16452164521645216452164521645216452

16452164521645216452164521645216452

16452164521645216452164521645216452

1645235.235.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.235.2

35.235.235.235.235.235.235.235.2

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.8

27.827.827.827.827.827.827.827.835.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.6

35.635.635.635.635.635.635.635.6

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.135.1

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.2

34.234.234.234.234.234.234.234.232.5

32.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.532.5

32.532.532.532.532.532.532.532.535.4

35.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.435.435.0

35.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.035.0

16455164551645516455164551645516455

16455164551645516455164551645516455

16455164551645516455164551645516455

164551645516455164551645516455

16455164551645516455164551645516455

16455164551645516455164551645516455

16455164551645516455164551645516455

16455

16456164561645616456164561645616456

16456164561645616456164561645616456

16456164561645616456164561645616456

164561645616456164561645616456

16456164561645616456164561645616456

16456164561645616456164561645616456

16456164561645616456164561645616456

1645616457164571645716457164571645716457

16457164571645716457164571645716457

16457164571645716457164571645716457

164571645716457164571645716457

16457164571645716457164571645716457

16457164571645716457164571645716457

16457164571645716457164571645716457

16457

16458164581645816458164581645816458

16458164581645816458164581645816458

16458164581645816458164581645816458

164581645816458164581645816458

16458164581645816458164581645816458

16458164581645816458164581645816458

16458164581645816458164581645816458

1645835.335.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.335.3

22.422.422.422.422.422.422.4

22.422.422.422.422.422.422.4

22.422.422.422.422.422.422.4

22.422.422.422.422.422.4

22.422.422.422.422.422.422.4

22.422.422.422.422.422.422.4

22.422.422.422.422.422.422.422.4

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.1

34.134.134.134.134.134.134.134.121.8

21.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.821.8

21.821.821.821.821.821.821.821.829.6

29.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.629.629.635.1

35.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.1

35.135.135.135.135.135.135.135.135.0

35.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.0

35.035.035.035.035.035.035.035.0

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.3

36.336.336.336.336.336.336.336.3

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.0

34.034.034.034.034.034.034.034.0

29.629.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.629.6

29.629.629.629.629.629.629.629.6

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

ES57-0

25

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25

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25

OVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVEROVER

OVER

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

28.028.028.028.028.028.028.0

28.028.028.028.028.028.028.0

28.028.028.028.028.028.028.0

28.028.028.028.028.028.0

28.028.028.028.028.028.028.0

28.028.028.028.028.028.028.0

28.028.028.028.028.028.028.028.0

32.732.732.732.732.732.732.7

32.732.732.732.732.732.732.7

32.732.732.732.732.732.732.7

32.732.732.732.732.732.7

32.732.732.732.732.732.732.7

32.732.732.732.732.732.732.7

32.732.732.732.732.732.732.732.7

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.4

37.437.437.437.437.437.437.437.436.6

36.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.6

36.636.636.636.636.636.636.636.635.5

35.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.5

35.535.535.535.535.535.535.535.5 52.0

52.052.052.052.052.052.0

52.052.052.052.052.052.052.0

52.052.052.052.052.052.052.0

52.052.052.052.052.052.0

52.052.052.052.052.052.052.0

52.052.052.052.052.052.052.0

52.052.052.052.052.052.052.052.050.6

50.650.650.650.650.650.6

50.650.650.650.650.650.650.6

50.650.650.650.650.650.650.6

50.650.650.650.650.650.6

50.650.650.650.650.650.650.6

50.650.650.650.650.650.650.6

50.650.650.650.650.650.650.650.631.4

31.431.431.431.431.431.4

31.431.431.431.431.431.431.4

31.431.431.431.431.431.431.4

31.431.431.431.431.431.4

31.431.431.431.431.431.431.4

31.431.431.431.431.431.431.4

31.431.431.431.431.431.431.431.455.8

55.855.855.855.855.855.8

55.855.855.855.855.855.855.8

55.855.855.855.855.855.855.8

55.855.855.855.855.855.8

55.855.855.855.855.855.855.8

55.855.855.855.855.855.855.8

55.855.855.855.855.855.855.855.8

23.623.623.623.623.623.623.6

23.623.623.623.623.623.623.6

23.623.623.623.623.623.623.6

23.623.623.623.623.623.6

23.623.623.623.623.623.623.6

23.623.623.623.623.623.623.6

23.623.623.623.623.623.623.623.637.6

37.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.6

37.637.637.637.637.637.637.637.6

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.1

49.149.149.149.149.149.149.149.1

29.929.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.929.9

29.929.929.929.929.929.929.929.933.9

33.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.9

33.933.933.933.933.933.933.933.9 42.1

42.142.142.142.142.142.1

42.142.142.142.142.142.142.1

42.142.142.142.142.142.142.1

42.142.142.142.142.142.1

42.142.142.142.142.142.142.1

42.142.142.142.142.142.142.1

42.142.142.142.142.142.142.142.148.4

48.448.448.448.448.448.4

48.448.448.448.448.448.448.4

48.448.448.448.448.448.448.4

48.448.448.448.448.448.4

48.448.448.448.448.448.448.4

48.448.448.448.448.448.448.4

48.448.448.448.448.448.448.448.4

51.551.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.551.5

51.551.551.551.551.551.551.551.5

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.734.736.836.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.836.8

36.836.836.836.836.836.836.836.831.0

31.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.0

31.031.031.031.031.031.031.031.0

53.453.453.453.453.453.453.4

53.453.453.453.453.453.453.4

53.453.453.453.453.453.453.4

53.453.453.453.453.453.4

53.453.453.453.453.453.453.4

53.453.453.453.453.453.453.4

53.453.453.453.453.453.453.453.4

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.2

36.236.236.236.236.236.236.236.2 42.2

42.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.242.2

42.242.242.242.242.242.242.242.2

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.5

37.537.537.537.537.537.537.537.536.1

36.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.136.1

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

32.132.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.132.132.130.8

30.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.8

30.830.830.830.830.830.830.830.8

16461164611646116461164611646116461

16461164611646116461164611646116461

16461164611646116461164611646116461

164611646116461164611646116461

16461164611646116461164611646116461

16461164611646116461164611646116461

16461164611646116461164611646116461

1646116459164591645916459164591645916459

16459164591645916459164591645916459

16459164591645916459164591645916459

164591645916459164591645916459

16459164591645916459164591645916459

16459164591645916459164591645916459

16459164591645916459164591645916459

16459

16460164601646016460164601646016460

16460164601646016460164601646016460

16460164601646016460164601646016460

164601646016460164601646016460

16460164601646016460164601646016460

16460164601646016460164601646016460

16460164601646016460164601646016460

1646016462164621646216462164621646216462

16462164621646216462164621646216462

16462164621646216462164621646216462

164621646216462164621646216462

16462164621646216462164621646216462

16462164621646216462164621646216462

16462164621646216462164621646216462

16462

16463164631646316463164631646316463

16463164631646316463164631646316463

16463164631646316463164631646316463

164631646316463164631646316463

16463164631646316463164631646316463

16463164631646316463164631646316463

16463164631646316463164631646316463

1646329.329.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.329.329.328.1

28.128.128.128.128.128.1

28.128.128.128.128.128.128.1

28.128.128.128.128.128.128.1

28.128.128.128.128.128.1

28.128.128.128.128.128.128.1

28.128.128.128.128.128.128.1

28.128.128.128.128.128.128.128.128.8

28.828.828.828.828.828.8

28.828.828.828.828.828.828.8

28.828.828.828.828.828.828.8

28.828.828.828.828.828.8

28.828.828.828.828.828.828.8

28.828.828.828.828.828.828.8

28.828.828.828.828.828.828.828.8

31.331.331.331.331.331.331.3

31.331.331.331.331.331.331.3

31.331.331.331.331.331.331.3

31.331.331.331.331.331.3

31.331.331.331.331.331.331.3

31.331.331.331.331.331.331.3

31.331.331.331.331.331.331.331.3

0.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.40.4

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.2

30.230.230.230.230.230.230.230.2

27.427.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.427.427.427.7

27.727.727.727.727.727.7

27.727.727.727.727.727.727.7

27.727.727.727.727.727.727.7

27.727.727.727.727.727.7

27.727.727.727.727.727.727.7

27.727.727.727.727.727.727.7

27.727.727.727.727.727.727.727.721.2

21.221.221.221.221.221.2

21.221.221.221.221.221.221.2

21.221.221.221.221.221.221.2

21.221.221.221.221.221.2

21.221.221.221.221.221.221.2

21.221.221.221.221.221.221.2

21.221.221.221.221.221.221.221.2

0.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.80.8

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16464164641646416464164641646416464

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16464164641646416464164641646416464

16464164641646416464164641646416464

16464

16465164651646516465164651646516465

16465164651646516465164651646516465

16465164651646516465164651646516465

164651646516465164651646516465

16465164651646516465164651646516465

16465164651646516465164651646516465

16465164651646516465164651646516465

16465

16466164661646616466164661646616466

16466164661646616466164661646616466

16466164661646616466164661646616466

164661646616466164661646616466

16466164661646616466164661646616466

16466164661646616466164661646616466

16466164661646616466164661646616466

16466

13.113.113.113.113.113.113.1

13.113.113.113.113.113.113.1

13.113.113.113.113.113.113.1

13.113.113.113.113.113.1

13.113.113.113.113.113.113.1

13.113.113.113.113.113.113.1

13.113.113.113.113.113.113.113.17.37.37.37.37.37.37.3

7.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.37.3

16468164681646816468164681646816468

16468164681646816468164681646816468

16468164681646816468164681646816468

164681646816468164681646816468

16468164681646816468164681646816468

16468164681646816468164681646816468

16468164681646816468164681646816468

16468

16469164691646916469164691646916469

16469164691646916469164691646916469

16469164691646916469164691646916469

164691646916469164691646916469

16469164691646916469164691646916469

16469164691646916469164691646916469

16469164691646916469164691646916469

16469

16470164701647016470164701647016470

16470164701647016470164701647016470

16470164701647016470164701647016470

164701647016470164701647016470

16470164701647016470164701647016470

16470164701647016470164701647016470

16470164701647016470164701647016470

16470

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.7

34.734.734.734.734.734.734.734.735.3

35.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.3

35.335.335.335.335.335.335.335.335.4

35.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.4

35.435.435.435.435.435.435.435.436.1

36.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.1

36.136.136.136.136.136.136.136.132.1

32.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.132.1

32.132.132.132.132.132.132.132.129.3

29.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.329.3

29.329.329.329.329.329.329.329.327.4

27.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.427.4

27.427.427.427.427.427.427.427.426.0

26.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.026.0

26.026.026.026.026.026.026.026.0

16471164711647116471164711647116471

16471164711647116471164711647116471

16471164711647116471164711647116471

164711647116471164711647116471

16471164711647116471164711647116471

16471164711647116471164711647116471

16471164711647116471164711647116471

16471

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16472164721647216472164721647216472

16472164721647216472164721647216472

16472164721647216472164721647216472

164721647216472164721647216472

16472164721647216472164721647216472

16472164721647216472164721647216472

16472164721647216472164721647216472

16472

ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m

ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-02562.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

IFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFLIFL

IFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFMIFM

QBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBSQBS

ARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARGARG

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150m E

lev

5,644,150mN

5,644,150mN

5,644,050mN

50m E

lev

5,644,250mN

5,644,350mN

5,644,350mN

5,644,250mN

250m E

lev 350m

Elev

450

m E

lev

250

m E

lev

350

m E

lev

50m

Ele

v 1

50m

Ele

v 450m

Elev

5,644,550mN

5,644,550mN

5,644,450mN

5,644,450mN 5,644,650mN

5,644,650mN

Scale 1:1,000Section Origin (top left)541,791.32 m E5,644,680 m N500 m ElevOrientation 180.0 degNAD83 UTM Zone 15

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ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m506.27m

ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m121.92m

ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m130.45m

ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-02562.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m62.18m

ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031

ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031ES57-031199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m199.34m

ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009

ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES57-036ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022ES56-022

ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009ES08-009201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m201m

ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES56-023ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025ES57-025

Raytec Metals Corp.

El Sol ProjectA Zone

Section E541791

0 25

metres

50

Scale: 1:1000

Drawing: Series 2

Projection: NAD83 UTM Zone 15

Date:21/9/2009

Author: AM, JF

Office: Vancouver

QV

QBSQuartz Biotite Schist

SSSericite Schist

Lost Core

Quartz Vein

FLTFault

XLC

Paragneiss

Argillite to Greywacke

GWKGreywacke

PG

Conglomerate

IFLHornblende Schist

CONG

ARG

Pink Text

Green Text

Blue Text

IF-Chlorite Magnetite Chert

IF-Magnetite Chert Jasper Hematite

IFMIF-Magnetite Chert

IFML

IFLMIF-Chlorite Chert Magnetite Garnet

All lines have 1cm offset = 25% Fe at 1:1000 scale

Percent magnetite measured from Satmagan.

Percent total Fe calculated from whole rock analysis Fe2O3.

Percent Fe. Analysis method uncertain.

RM = Result Missing

IFMJ

IFMRIF-Magnetite Chert Grunerite

IFMSIF-Magnetite Chert Chlorite Sediment

Quartz Porphyry

Granitic Dyke

Biotite dyke

GD

QP

CASCasing

OVEROverburden

BD

Legend

EL SOL PROJECT 2008 DIAMOND DRILLINGGeotechnical Data

HOLE ID From_m To_m Length_ REC_m REC_% RQD_m RQD_% Core Size Geotech Date RemarksES08-011 99.00 102.00 3.00 2.97 99.00% 2.52 84.85% NQ JT NOV 4 / 08ES08-011 102.00 105.00 3.00 2.95 98.33% 2.52 85.42% NQ JT NOV 4 / 08ES08-011 105.00 108.00 3.00 3.00 100.00% 3.00 100.00% NQ JT NOV 4 / 08ES08-011 108.00 111.00 3.00 2.75 91.67% 1.50 54.55% NQ JT NOV 4 / 08ES08-011 111.00 114.00 3.00 2.94 98.00% 2.10 71.43% NQ JT NOV 4 / 08ES08-011 114.00 117.00 3.00 2.97 99.00% 1.85 62.29% NQ JT NOV 4 / 08ES08-011 117.00 120.00 3.00 2.90 96.67% 1.83 63.10% NQ JT NOV 4 / 08ES08-011 120.00 123.00 3.00 2.85 95.00% 1.94 68.07% NQ JT NOV 4 / 08ES08-011 123.00 126.00 3.00 2.62 87.33% 0.47 17.94% NQ JT NOV 4 / 08 1.32cm crushed coreES08-011 126.00 129.00 3.00 2.97 99.00% 2.39 80.47% NQ JT NOV 4 / 08ES08-011 129.00 132.00 3.00 3.00 100.00% 2.47 82.33% NQ JT NOV 4 / 08ES08-011 132.00 135.00 3.00 2.90 96.67% 2.52 86.90% NQ JT NOV 4 / 08ES08-011 135.00 138.00 3.00 2.87 95.67% 2.06 71.78% NQ JT NOV 4 / 08ES08-011 138.00 141.00 3.00 2.92 97.33% 2.14 73.29% NQ JT NOV 4 / 08ES08-011 141.00 144.00 3.00 2.83 94.33% 2.06 72.79% NQ JT NOV 4 / 08 10cm gougeES08-011 144.00 147.00 3.00 2.97 99.00% 1.96 65.99% NQ JT NOV 4 / 08 24cm redrilled / 2cm gougeES08-011 147.00 150.00 3.00 2.90 96.67% 1.96 67.59% NQ JT NOV 4 / 08ES08-011 150.00 153.00 3.00 3.00 100.00% 1.60 53.33% NQ JT NOV 4 / 08ES08-011 153.00 156.00 3.00 3.00 100.00% 2.55 85.00% NQ JT NOV 4 / 08ES08-011 156.00 159.00 3.00 2.90 96.67% 2.08 71.72% NQ JT NOV 4 / 08ES08-011 159.00 162.00 3.00 3.00 100.00% 2.78 92.67% NQ JT NOV 4 / 08ES08-011 162.00 165.00 3.00 2.92 97.33% 2.88 98.63% NQ JT NOV 4 / 08ES08-011 165.00 168.00 3.00 3.00 100.00% 2.80 93.33% NQ JT NOV 4 / 08ES08-011 168.00 171.00 3.00 3.00 100.00% 2.87 95.67% NQ JT NOV 4 / 08ES08-011 171.00 174.00 3.00 3.00 100.00% 2.77 92.33% NQ JT NOV 4 / 08ES08-011 174.00 177.00 3.00 3.00 100.00% 2.31 77.00% NQ JT NOV 4 / 08ES08-011 177.00 180.00 3.00 3.00 100.00% 2.70 90.00% NQ JT NOV 4 / 08ES08-011 180.00 183.00 3.00 3.00 100.00% 2.18 72.67% NQ JT NOV 4 / 08ES08-011 183.00 186.00 3.00 3.00 100.00% 2.73 91.00% NQ JT NOV 4 / 08 E.O.H.