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32D12SW2022 2.20610 LAMPLUGH 010

2.206 10

REPORT ON THE 1999 GROUND EXPLORATION PROGRAM

BY R. A. CAMPBELL AND G. N. HENRIKSEN

ON THEIR WISHING WELL PROPERTY

LAMPLUGH TWP., LARDER LAKE MINING DIVISION, ONT.

Dec. 15, 1999

ECEIVED

GEOSCIENCE ASSESSMENT OfFlCE ____ .

R. A. Campbell Geologist

G. N. Henriksen Geologist

32D12SW2022 2.20610

TABLE OF CONTENTS

INTRODUCTION

PROPERTY DESCRIPTION, LOCATION AND ACCESS

REGIONAL AND LOCAL GEOLOGY

POTENTIAL MINERALIZATION

SUMMARY OF PREVIOUS WORK

WORK PERFORMED AND METHODS USED Grid Establishment Prospecting Program Geochemical Sampling Program Detailed Total Field Magnetic Survey Very Low Frequency - Electromagnetic Survey Geological Mapping and Rock Sampling Program

SURVEY RESULTS AND INTERPRETATION Geochemical Sampling Program Detailed Total Field Magnetic Survey Very Low Frequency - Elecctromagnetic Survey Prospecting, Geological Mapping and Rock Sampling Programs

CONCLUSIONS AND RECOMMENDATIONS

LAMPLUGH 010C

REFERENCES

FIGURE l FIGURE 2 FIGURES

APPENDIX l APPENDIX 2

GC-1 M-1 VLF-1 PG-1

FIGURES

Recent Claim Map with Work Area Outlined Regional Geology Map Local Geology Map

APPENDICES

Certificates of Analysis Rock Sample Descriptions

MAPS

Geochemical Sampling Total Field Magnetic Survey VLF-Electromagnetic Survey Prospecting and Geology

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356

REPORT ON THE 1999 GROUND EXPLORATION PROGRAM

BY RA. CAMPBELL AND G.N. HENRIKSEN

ON THEIR WISHING WELL PROPERTY

LAMPLUGH TWP., LARDER LAKE MINING DIVISION, ONT.

INTRODUCTION

Between June 26 and September 24, 1999, R. A. Campbell and G. N. Henriksen completed a ground exploration program on their Wishing Well Property in Lamplugh Township, Ontario. The 1999 exploration program, made possible by an OPAP grant, was completed to delineate the geological-geophysical-geochemical environments underlying the property and to test the potential of these environments to host precious and base metal mineralization. The exploration work was comprised of linecutting-chaining-picketing, prospecting, geological mapping, rock and geochemical soil and stream sediment sampling and geophysical surveying (very low frequency-electromagnetics and detailed total field magnetics).

The property is situated in an area of northeastern Ontario that has favourable geology and structures for mineral deposition but has seen very little past exploration. The project appears to be underlain by tholeiitic basalt and intermediate to felsic metavolcanics of the Stoughton- Roquemaure Assemblage overlying calc-alkalic intermediate to felsic metavolcanics of the Kidd Munro Assemblage (Hunter Mine Group). These metavolcanics may lie at the nose of a possible fold and have been intruded by a felsic intrusive body. The North Branch of the Porcupine Destor Fault Zone crosses the southern part of the property along the unconformable contact between the Stoughton-Roquemaure Assemblage, to the north, and the Kidd Munro assemblage to the south. A possible splay of the Porcupine Destor Fault Zone, as represented by a breccia zone intersected in drill holes, lies along a contact between the mafic to intermediate metavolcanics and intermediate to felsic metavolcanics of the Stoughton-Roquemaure Group.

Data collected in the minimal amount of past work in the region outlines the location of an airborne Input anomaly along a northern interflow intermediate to felsic metavolcanic band, a quartz vein lies in Mg rich pyroclastic basalts and intermediate to felsic metavolcanics in the eastern region and trace amounts of pyrite, sphalerite and chalcopyrite were intersected in rhyolite tuff in the drill hole collared on the project. Anomalous to very high amounts of Au in till samples have been collected by the O.G.S. in Lamplugh Twp., including an irregular Au grain in sample 85-60B in the eastern part of the property, near the quartz vein.

The 1999 program of ground exploration was designed to: test the potential of the metavolcanics to contain Au-Cu and base metals in one or more of 4 potential deposit types; explain the unexplored Input anomaly and airborne magnetic signature; delineate Au bearing quartz veins in metavolcanics and felsic intrusives; and expand upon the data obtained in the past O.G.S. geochemical sampling in the area.

PROPERTY DESCRIPTION. LOCATION AND ACCESS

The 1999 exploration program was completed by R. A. Campbell and G.N. Henriksen on their Wishing Well Property in the north-central part of Lamplugh Twp. (G.3662), Larder Lake Mining Division, Ontario. The Wishing Well Property is comprised of two contiguous claims (23 units), 1140876 (15 units) and 1225710 (8 units), covering approximately 368 hectares. The 1999 program was concentrated on the northern claim (l 140876) and the western 65 "/o of the southern claim (1225710), as outlined in the enclosed figure 1.

The Wishing Well Property is located on topographical map NTS 32/D12 (Lightning River Sheet), at a latitude of 48 degrees, 35 minutes (UTM 5382000 m. N.) and at a longitude of 79 degrees, 48 minutes and 30 seconds (UTM 588000 m. E.). The claims are registered in the name of G. N. Henriksen of 850 Route des Pionners, Bellecombe, Quebec at the Office of the Mining Recorder in Sudbury.

The 2 claims are forest covered with second growth alder, poplar, moose maple, balsam, birch and spruce. It appears that the logging was conducted in the area approximately 20 to 40 years ago. Local topographical relief over 95 "/o of the property is low, less than 15 meters, with a large swamp lying in the southwest corner of the property and a hill of exposed outcrop situated in the eastern part of the northern claim. Systems of creeks, connecting small beaver ponds, flow across the property and the northeast corner is flooded. Makua Bay of Lake Abitibi lies 2 km. to the north.

The 2 claims are best accessed via logging roads trending north, west and east from Highway 101, 4 km. east of the Ghost River (see figures l and 3). The logging road splits after 3, 5 and 8 km., with access via the first left, and next two roads to the right. At the last intersection the road turns to the east, crossing the western boundary of claim 1140876 after a further 2 km. This road bisects the central region of this claim, with a secondary road north towards Lake Abitibi crossing the northwest corner of the property. Various skidder roads cross the eastern part of the area of exploration, see Map PG-1.

Supplies and services were obtained in the Matheson and Kirkland Lake areas.

LOCAL AND REGIONAL GEOLOGY

The Wishing Well Property is located in the western part of the Abitibi greenstone belt, the world's largest Archean belt, which is approximately 800 km. long in a west-east direction and up to 240 km. meters wide. It extends from west of Timmins, Ontario, to east of Chibougamou, Quebec and hosts numerous precious and base metal deposits within the Timmins, Kirkland Lake, Harker-Holloway, Noranda, Val D'Or and Chibougamau mining camps.

The Abitibi greenstone belt is composed of a complex assemblage of interbedded volcanic and sedimentary rocks, intruded by a variety of ultramafic to felsic intrusives. The rocks are Archean in age and have been metamorphosed to the subgreenschist facies. Numerous Late Precambrian diabase dykes cut the rocks of the belt. The rock units generally strike west-east, have near vertical dips and are highly faulted and folded. Geological interpretation of the Abitibi

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belt is complicated by the wide scattering of outcrop exposures and thick overburden cover in most areas and the complex underlying structural relationships.

O.D.M. and O.G.S. geology maps 2205, P.2433 and P.3398, outline the geology in the Lake Abitibi area, including the area surrounding the property. Figure 5 of O.G.S. Misc. Paper 123 and figure 4.1 of O.G.S. Misc. Paper 169 also define the geology and structures in the area. Figure 4.1 of Misc. Paper 169 and Map P.3398, published in 1999, contain the latest stratigraphical revision and the nomenclature used by the O.G.S. Figure 4.1 and Map P.3398 in the area of the property are copied in the attached figure 2 and 3, respectively, and assemblages and rock types defined on them will be quoted in this report.

The property is situated in a region underlain by east-northeast to east-southeast trending calc-alkalic, tholeiitic and komatiitic metavolcanics, which are intruded by an elliptical southwest striking felsic intrusive body. The Abitibi Batholith is located 11 km. north of the project. The North Branch of the Porcupine Destor Fault Zone crosses the southern part of the southern claim and the Main Branch of the Porcupine Destor Fault lies 7 km. to the south. The O.G.S. geology maps show that the contact between the calc-alkalic metavolcanic rocks (dacitic and andesitic tuff-breccia and flows) and minor metasediments of the newly defined Kidd Munro Assemblage (formerly the Hunter Mine Group) and the overlying metavolcanics (flows of peridotitic and basaltic komatiite and Mg rich tholeiitic basalt with minor Fe rich basalt and interflow rhyolite tuff and cherty tuff) and interbands of minor metasediments (chert and iron formation) of the Stoughton-Roquemaure Assemblage is thought to be along the North Branch of the Porcupine Destor Fault Zone (see enclosed figure 2).

L.S. Jensen mapped the outcrops in the area in 1973, producing O.G.S. Geological Series Preliminary Map P.2431 of the Ghost River Area, 1982, at a scale of 1:15,840. The data presented on this map better defines the results shown on map P.2433. Exposures of intercalated tholeiitic Mg rich basalt (massive fine and medium-grained lava, pillow lava, pillow breccia, flow top breccia, tuff-breccia, tuff, middle greenschist facies basalt), calc-alkalic mafic to intermediate metavolcanics (tuff-breccia) and calc-alkalic felsic metavolcanics (crystal tuff) and interflow sediments have been mapped in the central part of the eastern end of claim 1140876. Outcrops of tholeiitic Fe rich basalt (fine to medium grained lavas) are exposed in the southeast corner of the property. These rocks strike east-northeast to east-southeast. Quartz veining was mapped, in an outcrop of Mg rich basaltic flow top breccia and tuff-breccia, intercalated with felsic metavolcanic rocks, in the central part of the northern claim.

O.G.S. Map P.3398 (see figure 3), published in the summer of 1999, best defines the local geology underlying the two claims. The recent data provided on this map indicates that the southern 2/3 of the property is underlain by east-southeast trending intermediate to felsic metavolcanic rocks. North of these intermediate to felsic metavolcanics three units of tholeiitic mafic to intermediate metavolcanics strike east-southeast to east, south of an elliptical shaped suite of felsic to intermediate intrusive rock which is thought to across the northern boundary of the property. In the extreme southwestern region, south of the North Branch of the Porcupine Destor that strikes 102 degrees across the southern claim, are calc-alkalic intermediate to felsic metavolcanic rocks of the Kidd Munro Assemblage. These calc-alkalic metavolcanics are in contact with a 0.3 to 0.5 km. wide band of intermediate to felsic massive flows, tuff and lapilli tuff, (Stoughton-Roquemaure Assemblage ?) north of the fault. The three units of mafic to inter-

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Figure 4.1. Revised stratigraphic subdivisions for the northern pan of the Abitibi greenstone belt in Ontario with geochronology sample locations as discussed in (he text.

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mediate metavolcanics that underlie the northern 2/3 of the property are high Fe and Mg tholeiites. An anticlinal axis trends southwest through the tholeiitic mafic to intermediate metavolcanics, 400 to 800 meters west of the claim, ending 400 meters north of the fault zone.

Diamond drilling by Seal River Exploration in 1987, including hole LR 87-4, collared just north of the southern boundary of the northern claim and drilled into the southern claim, and hole LR 87-3 located just west of the southwest part of claim 1140876, confirm the geology presented on Map P.3398. These holes intersected felsic lavas and tuffs, representing the southern intermediate to felsic band of the Stoughton-Roquemaure Assemblage. These felsic rocks lie south of a quartz-carbonate breccia, up to 12 meters in width, that strikes 118 degrees across the southern part of the property. This breccia zone represents a possible splay of the North Branch of the Porcupine Destor Fault Zone, lying along the contact between the southern intermediate to felsic metavolcanic band and the tholeiitic metavolcanics of the Stoughton-Roquemaure Assemblage.

Mapping in 1998, on a claim situated immediately north of the Wishing Well property, delineated the position of a small outcrop of mineralized rhyodacite lying along the north-central boundary. This outcrop defines the location of interflow felsic metavolcanic rocks of the Stoughton-Roquemaure Assemblage.

The total intensity magnetic contours presented on O.G.S. airborne Map 80589, strike east-northeast across the northern and central parts of the property and east-southeast through the southern region. The south edge of a large elliptical shaped high, representing the boundaries of the felsic intrusive body, crosses the northwest part of the property. Two narrow lows trend east-northeast, crossing claim 1140876, and a third, wider low strikes east-south east through the southern part of claim 1225710. The northern edge of the northern low, lies over the rhyodacite outcrop mapped in 1998 and an unexplained 2 channel Input anomaly. A magnetic high is situated between the two east-northeast trending lows in the north. The southern east-northeast trending low is located over the outcrops of intermediate to felsic metavolcanic rocks in the western part of the northern claim. South of this low is an area containing a relatively weak high and areas of low relief. The southern most low lies south of this weak high, trending 102 degrees along the North Branch of the Porcupine Destor Fault Zone. The shape and distortions in the magnetic contour pattern suggest that a linear zone of deformation strikes 118 degrees through the property at the exact location of the breccia zone delineated in the 1987 drill holes. This zone continues to the east-southeast, joining the North Branch of the Porcupine Destor Fault Zone, 500 meters east of the southeast corner of the property. This breccia zone may be caused by an underlying splay of this of this fault zone. Also there is also a chance that a fold axis strikes east through the southern part of the project, as represented by the directions of the magnetic contours, trending east-northeast in the north and central regions and east-southeast in the south.

The property lies in an area where O.G.S. backhoe till and sonic drill hole samples contain anomalous to very high amounts of gold. Of the two backhoe till samples collected on the project, sample 85-60B in the eastern part of the claim, contained one irregular gold grain. Backhoe sample 85-54B, collected near the North Branch of the Porcupine Destor Fault Zone, 1.2 km along strike east-southeast of the property, assayed 2000 ppb Au. Sonic hole 84-2, collared 2.8 km. southwest of the property, intersected 31,000 ppb Au over 6 feet. Six more holes were drilled

8

near this hole in 1988, intersecting anomalous Au values in each hole.Quartz veining and sulphide mineralization has been found on or near the two claims

during the O.G.S. mapping program. A quartz vein has been discovered in basaltic flow top breccia and tuff-breccia and calc-alkalic intermediate to felsic metavolcanics in the western part of claim 1140876. Rhyolite tuff in hole LR 87-4 contained trace amounts of pyrite, sphalerite and chalcopyrite. Pyrite has been mapped in calc-alkalic rocks and Fe and Mg rich basalt, 1.6 km. along strike northeast and 2.4 km. to the north. Chalcopyrite mineralization has been found in Fe rich basalt, 3.2 km. to the north.

POTENTIAL MINERALIZATION

From studying: geology maps, O.G.S. P.2431, P 2433 and P.3398 and O.D.M. 2205; O.G.S. Mics. Papers 123 and 169; the results of O.G.S. overburden drilling and airborne geophysical surveying; and past exploration on the western 40 07o of the property, it is determined that the two claims are situated in an area that has the potential to host base and precious metals. On O.G.S. map P.2433, L. S. Jensen and F. F. Langford state that 4 types of mineralization may exist on or in the area of the Wishing Well Property. They include:

l) Cu (H-7-Au-Pb-Zn) in Gale-Alkalic Intermediate to Felsic Metavolcanic Rocks of the Kidd Munro and Stoughton-Roquemaure Assemblages.

Past O.G.S. mapping, prospecting and mapping north of the property in 1998, the results of l Seal River Exploration diamond drill hole collared near the boundary of the two claims and a second hole just west of the western boundary and the data presented on the airborne map 80589, indicates that intermediate to felsic metavolcanic rocks underlie at least 4 regions of the project. O.G.S. Maps P.2431, P.2433 and P.3398 show that the southern part of the southern claim, south of the North Branch of the Porcupine Destor Fault Zone, is underlain by intermediate to felsic calc-alkalic metavolcanic rocks of the Kidd Munro Assemblage.

The results of the drilling in 1987 by Seal River Explorations intersected felsic metavolcanic lavas and pyroclastics in a zone trending east-southeast through the southwestern part of the northern claim and across the northwestern part of the southern claim. These drill intersections confirm the data presented on O.G.S. Map P.3398, showing a 0.3 to 0.5 km. wide band of intermediate to felsic metavolcanics of the Stoughton-Roquemaure Assemblage striking 100 to 115 degrees across the southern part of the property, north of the North Branch of the Porcupine Fault Zone. Rhyolite tuff in hole LR 87-4 contained trace amounts of pyrite, sphalerite and chalcopyrite.

Geological mapping by Jensen in 1973 (Map P.2431) outlined outcrops of calc-alkalic felsic metavolcanics (crystal tuff), intermediate to mafic metavolcanics (tuff-breccia) and possible interflow sediments, striking west-southwest to west-northwest in the west-central part of the northern claim.

Mapping in 1998 on a claim, located due north of the Wishing Well Property, delineated a mineralized rhyodacite outcrop lying along the northern boundary of the property. Observations made during staking of claim 1140876 in the fall of 1998, indicate that areas

of modest relief are situated north of the felsic to mafic metavolcanic outcrops in the west-central part of the claim and south of the rhyodacite outcrop in the north. These may represent unmapped and unexplored exposures of felsic to intermediate metavolcanic rocks.

Three linear airborne magnetic lows, define the limits of probable felsic to intermediate metavolcanic units. The northern two lows are narrow and trend east-northeast through the northwestern and central regions. A 2 channel Input anomaly lies in the northern low, along the northern boundary of the property, 250 meters east of the rhyodacite outcrop. The third low is broader and strikes east-southeast across the southern claim.

Chalcopyrite occurrences have been discovered 3.2 km. north of the property and along the southern shore of Lake Abitibi, 8 km. west-northwest along strike. Three chalcopyrite occurrences lie in felsic to intermediate rocks of the Kidd Munro Assemblage (Hunter Mine Group) in Rand Twp., 8 to 10 km. to the southwest. The Millstream Mines sulphide bearing Cu-Zn deposit in Munro Twp. is situated 28 km. east of the property. 2) AU(H-/- Ag) in Sheared, Fractured, Fault and Breccia Zones within Metavolcanic, Metasedimentary and Felsic Intrusive Rocks.

The property is situated in an area where 3 mines are in production and numerous deposits have been discovered associated with deformation zones. The 2 claims are thought to be underlain by faulted and brecciated felsic to mafic metavolcanic* rocks, with interflow metasediments, lying south of a felsic intrusive body. The North Branch of the Porcupine Destor Fault Zone strikes 102 degrees across the southern part of the southern claim. The Seal River Ex. drilling outlined a breccia zone of quartz-carbonate striking 118 degrees in the southern part of the property, north of the North Branch of the Porcupine Destor Fault Zone. This breccia zone lies along a linear zone of breaks, offsets and distortions that crosses the airborne magnetic contour pattern. This fact suggests that the breccia zone is a possible splay of the fault zone.

The Holt-Mcdermott and Holloway producing gold mines are located 8 km. south of the property. At the Holloway Mine, Au is associated with a splay of the Porcupine Destor Fault Zone in albite altered thoeiitic rocks, surrounded by halos of sericite and carbonate alteration. At the Holt-McDermott Mine a fault in albitic alteration with hematite and siliceous alteration hosts Au.

Au has also been discovered in alkalic rocks, within or near major faults or shear zones of the Porcupine Destor Fault Zone at the Buffonta, New Buffonta Garrcon, Jonpol Pangea, Ludgate and Moneta Porcupine deposits, located in Garrison and Michaud Townships 20 to 35 km. to the west-southwest. The Glimmer Gold Mine is situated in Hislop Twp., 43 km to the west-southwest. Pyrite mineralization has been discovered 1.6 km. to the north-northeast, along strike, 2.4 km. north of the property, and at various locations in the vicinity along the shore of Lake Abitibi. 3) Au in Quartz Veins, Fillings and Stockworks.

Au has been discovered in overburden in Lamplugh Twp. and quartz veining has been mapped on the property and along the shore of Lake Abitibi. A west-southwest trending quartz vein cuts basalt and felsic metavolcanics in the eastern part of the northern claim and a large (3 meters wide) quartz vein has been mapped along the shore of Lake Abitibi, 10 km. to the northwest.

10

O.G.S. backhoe sample 85-60B, with l Au grain, was collected near the quartz vein in the eastern part of the northern claim. Sample 85-54B, 1.2 km. along strike to the east-southeast, near the North Branch of the Porcupine Destor Fault Zone, contained 2000 ppb Au. Samples taken in sonic drill holes, 2.4 to 2.8 km. southwest of the property, exhibited high to very high Au values, up to 31,000 ppb Au over 6 feet. 4) Au in Mineralized Felsic Dykes which have been Carbonatized or Silicified with or without a Stockwork of Quartz Veining.

The southern edge of a southwest striking felsic intrusive body is thought to cross the north-central boundary and felsic dykes cut metavolcanic rocks, just north of the property. The east-southeast trending breccia zone also contains quartz-carbonate alteration.

SUMMARY OF PREVIOUS WORK

The only past field work on the area forming the Wishing Well Property, not produced by the O.G.S., was performed in 1986 and 1987 by Seal River Exploration on the area that comprises the western 40 "/o of the property (assessment report 2467). Three later assessment reports (3152, 3376 and 3398) by Seal River Exploration describe work performed west of the property or further describe and present compilations of the work conducted in 1986 and 1987.

All previous exploration work and recent O.G.S. surveying is presented below:1973 -L.S. Jensen of the O.G.S. regionally mapped Lamplugh Twp. producing geology

maps P.2431, P.2433 and Misc. Paper 123.1983 - Questor Surveys flew airborne EM and total intensity magnetic surveys over the

township for the O.G.S. (Map 80589)1985 - The O.G.S of the Ont. Ministry of Natural Resources collected 2 backhoe till sam

ples, 85-60B and 85-61B along the road trending east in claim 1140876.1986 - Seal River Exploration Ltd. (F. J. Sharpley) for Pronto Exploration Ltd. performed

linecutting at 020 degrees, magnetic and VLF-electromagnetic surveying, reconnaissance geological mapping and humus geochemical sampling (Au-As) over their L. River Property that covers the western 40 *Yo of the Wishing Well Property (assessment reports 2467, 3152, 3376, and 3398).

1987 - Seal River Exploration Ltd. (F. J. Sharpley) for Pronto Exploration Ltd., drilled one diamond drill hole (LR 87-4) on the 1999 project, near the boundary between the two claims (assessment reports 2467 and 3152).

WORK PERFORMED AND METHODS USED

The 1999 program of field work was performed by the authors between June 26 and September 24 (156 total field days). The exploration was completed over all of the northern claim (l 140876) and over the western 65 0/* of the southern claim (1225710), which after preliminary research was thought to have the best geological/geophysical/geochemical signatures. The various types of fieldwork and their methods of execution are described in the following sections.

11

Grid Establishment

Between June 28 and August 9, 1999, a grid was established on the property, covering all of claim 1140876 and the western 65 07o of claim 1225710 (80 total days). Baseline O was cut and chained east and west along or near the boundary between the two claims, extending westward to post 3 of claim 1140876 (15W) and eastward along the boundary and into claim 1225710 until 9+30 E. Tieline N was established along the northern boundary of claim 1140876 and tieline S was cut along the southern boundary of claim 1225710, from line 6W to line 5E. Crosslines were cut north and south from the baseline at 100 meter intervals from line 15W to line 5E and line 6W to 5E, respectively. All the lines were chained and picketed at 25 meter intervals, for a total of 41.7 line km.

Prospecting Program

The program of prospecting was completed on the property on June 26 and 27 and between August 10 and 17 and August 30 to Sept. 3, 1999. Approximately 52 line km. of prospecting traverses were walked by the authors during the 26 total days spent prospecting.

The prospecting was conducted to locate claim boundaries, claim posts, outcrop exposures, boulders, mineralization, drill hole locations, overburden cover, tree types, etc. and topographical features, such as: roads, trails, ponds, creeks, dams, hills, and cliffs. The prospecting traverses and the data collected are presented on Map PG-1, at a scale of l :2500.

Geochemical Sampling Program

A total of 80 geochemical samples (WW-01 to WW-80) were collected by the authors during August 24 to 27, 1999 (8 days). These samples were located near the outcrops of intermediate to felsic metavolcanics, surrounding the location of backhoe sample 85-60B, in the eastern part of the northern claim. Samples WW-01 to WW-69 were Ao soil horizons sampled at depths of 0.3 to 0.6 meters using a narrow spade. Except for the few samples near outcrop, the soil samples were generally collected in areas of low relief. Eleven stream sediment samples (WW-70 to WW-80) were gathered by hand along the edges of a creek in the northeastern corner of the property.

The geochemical samples were dried and taken to XRAL Laboratories (a division of SGS Canada Inc.) where they were sieved to 80 mesh and analysed for Au by the XRF-7 method for an additional 31 elements (Be, Na, Mg, Al, P, K, Ca, Se, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, As, Sr, Y, Zr, Mo, Ag, Cd, Sn, Sb, Ba, La, W, Pb and Bi) using the ICP 70 method with aqua regia digestion. The certificates of analyses are presented in Appendix l and the locations of the samples are drafted on Maps GC-1 and PG-1. The analytical results of the 5 elements, Au, Ag, Cu, Zn and Pb that are being explored for plus As analyses are plotted on Map GC-1 at a scale of 1:2,500. The results and locations of the soil and stream sediment samples that are considered to be anomalous are highlighted on Map GC-1. The units of concentration and detection limits are also shown in Appendix l.

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Detailed Magnetometer Survey

Between September 15 and 24, 1999 the authors spent 16 days completing a detailed total field magnetic survey along the 36.09 km. of crosslines. Gem Systems GSM 8 proton precession magnetometers were used to collect approximately 2900 readings at 12.5 meter intervals along the crosslines. The detailed magnetic survey was performed to collect data which will help define: contacts between rock units of varying magnetic susceptibilities; the locations of potential fault/shear zones; and concentrations of magnetic minerals. The readings were taken at the detailed 12.5 meter intervals to better outline the smaller anomalous zones and rock units.

The GSM 8 magnetometer measures the total field intensity of the earth's magnetic field in gammas. The instrument has a sensitivity and repeatability of one gamma or better. Two base stations, for determining the magnetic diurnal variations, were established on line O at 6N and on line HW at 6+25N. The raw data was corrected for the diurnal variations. The corrected total field readings, minus a base value of 57,000 gammas, were plotted on Map M-1 at a scale of l :2,500 and contoured at 100 gamma intervals till 58,000 gammas.

Very Low Frequency - Electromagnetic Survey

The very low frequency-electromagnetic survey was conducted using Geonics EM-16 units. Twelve total days were spent by the authors during September 7 to 10 and on September 12 and 14, 1999, collecting approximately 1500 readings at the 25 meter stations picketed along the 36.09 km. of crosslines.

The VLF-EM survey uses powerful radio transmitters located in different parts of the world which were established for military communications. Relative to the frequencies generally used in geophysical exploration, the frequencies used in VLF-EM surveying are considered to be high. These powerful radio waves induce electrical currents in conductive bodies thousands of miles away. The induced currents produce secondary magnetic fields which are detected at surface through deviations of the normal VLF field. This secondary field from the conductor is added to the primary field vector, so that the resultant field is tilted up on one side of the field vector and down on the other side. The VLF receiver measures the field tilt, with the in-phase and quadrature components of the vertical magnetic field as a percentage of the horizontal primary field, i.e. the tangent of the tilt angle and elipticity. The Geonics EM-16 unit has a repeatability and sensitivity of l Yo.

Interpretation of the results is quite simple, the conductor is located at the point marked at the crossover from positive tilt (vertical in-phase) to negative tilt. The main advantage of the VLF method is that it responds well to poor conductors and has been proven to be a reliable tool in helping to map faults-shear zones, mineralization, conductive horizons and rock contacts. The major disadvantage is that because of the high frequency of the transmitted wave, a multitude of anomalies from unwanted sources, such as edges of swamps, lakeshores, creeks and changes in topographical and bedrock relief, may be delineated. So some amount of care must be taken in interpreting the results collected in areas displaying the above-mentioned topographical features.

Because of the trend of the rock units underlying the property, the transmitting station at Cutler Maine (NAA), frequency 24.0 kHz. was used. The readings were collected with the instrument facing 015 degrees.

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The VLF-EM in-phase and quadrature data (in percent) was plotted on Map VLF-1 at a scale of 1:2500. These values were then profiled at a scale of l cm. equals 10 percent. The conductor axes were determined and given labels, A, B, C. etc. No priority or significance was attached to the labelling system.

Geological Mapping and Rock Sampling Programs

All outcrop exposure found in claim 1140876 and in the western 2/3 of claim 1225710 was mapped with examples of mineralization, alteration and shearing being sampled. The geological mapping and sampling programs were performed by the authors between August 18 and 23 and on September 4, 1999 (14 person days). Most of the outcrop exposures were mapped in the eastern part of the northern claim, but outcrops were found scattered through both claims. A total of 13 rock samples (61501 to 61513) were collected from outcrop exposures, 12 grab and one chip sample across 1.5 meters (sample 61507). All 13 samples were assayed for gold, with sample 61503 also being assayed for copper and zinc. Ag assays were also determined on samples 61503, 61504, 61506 and 61508 to 61510. These assays/analyses were completed at the XRAL Laboratories, using the fire assay/instrumental finish method for the precious metal determinations and the atomic absorption method for the Zn and Cu analyses. The results are reported in ppb for Au and ppm for Ag, Zn and Cu. The assay certificates and rock sample descriptions are shown Appendices l and 2, respectively.

The data compiled by the mapping and sampling program is presented on Map PG-1 at a scale of 1:2500.

SURVEY RESULTS AND INTERPRETATION

Geochemical Sampling Program

Except in areas of outcrop exposures, the large swamp in the southwest and along the creeks and ponds, the gridded region is overlain by glaciolacustrine clay and silt. Compared to the surrounding areas in the Abitibi region, drill hole information indicates that overburden cover on the property is relatively thin, less than 20 meters. A thin, < 5 cm. thick, layer of organics overlies the clay and silt in most areas. Thicker layers of organics cover the swamp in the southwest and in regions near the creeks and ponds in the southeast and northeast.

The geochemical samples were collected in the eastern part of claim 1140876, where felsic metavolcanics were mapped and where the Au grain in was found in the backhoe till sample 85-60B. Generally, the analytical results for Au, As, Zn and Cu were elevated compared to those found in the Abitibi area. Except for l anomalous Ag result of 0.4 ppm in stream sediment sample WW-72, all the anomalous geochemical values were in Ao soil samples.

Usually, As values in the area are less than the analytical detection limit of 3 ppm, but 4 samples collected on the property contained measurable amounts of As. A very high amount of As of 117 ppm was, reported in sample WW-21, lying near felsic metavolcanic and gabbro outcrops. The three other anomalous As results, between 7 and 54 ppm, also are located near felsic metavolcanic outcrops.

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The soil and stream sediment samples also contain elevated to anomalous amounts of Au. A total of 29 samples contain more than background amounts of Au, over 9 ppb Au and 7 samples with over 15 ppb Au contain anomalous amounts of Au. There is no discernible pattern associated with the positions of the anomalous Au values, but 6 of the 7 anomalous Au samples are situated west or southwest of outcrops of felsic metavolcanics. The amounts of Au in 12 of the 13 samples on line O are above background. Two of the 4 anomalous As values (54 and 7 ppm) in samples WW-54 and 61 also have coincident anomalous amounts of 16 and 17 ppb Au.

The Ag amounts in the geochemical samples are low, with 45 of the 80 samples collected exhibiting less than the analytical detection limit of 0.2 ppm. Four soil samples (WW-14, 19, 41 and 43) and stream sediment sample WW-72 contain over 0.3 ppm Ag which are considered to be anomalous on the property. The 4 soil samples anomalous in Ag are situated near outcrops of felsic metavolcanics. Anomalous Ag sample WW-14 (0.4 ppm) also contains an anomalous amount (18 ppm) of Au.

The values of base metals, Zn and Pb, are also shown on Map GC-1. Over one half of the soil samples collected contained elevated amounts of Zn of over 100 ppm, while most of the Pb results were low in the range of 10 to 15 ppm. Nine samples, WW- 09, 11, 17, 25, 37, 41, 52, 53 and 55, exhibit anomalous amounts of Zn of over 125 ppm. There appears to be two dispersal patterns of anomalous Zn, one trending southwest from the road at line 2E to line O at 2+50N, west of felsic metavolcanic outcrops and the second striking west from line 5W at 2+50N. The highest Zn value of 177 ppm (sample WW-09) lies at the east end of this west trending zone. Two samples (WW-25 and 41) with anomalous amounts of Zn, also contain anomalous amounts of As (7 ppm) and Ag (0.5 ppm), respectively. Only one geochemical sample (WW-25), lying at the west end of the west trending anomalous Zn zone, hosts an anomalous Pb value of 22 ppm. This sample also contains anomalous amounts of Zn (137 ppm) and As (7 ppm).

Anomalous copper was discovered in 6 samples, with over 40 ppm Cu. Background values are in the range of 5. l to 25 ppm. Five of the 6 samples anomalous in Cu are on line 5E, with 4 of these samples forming a continuous zone striking south, south and east of outcrops of felsic metavolcanics. The highest Cu result of 53.1 ppm is situated at the north end of this zone. Sample WW-61, with 50 ppm Cu, also contained 15 ppb Au and 7 ppm As.

Detailed Total Field Magnetic Survey

The magnetic contours have two definite strike directions, east-northeast in the central and northern regions and east to east-southeast in the southern part of the grid. Individual highs and lows form anomalies 12.5 to 110 meters in width, with sharp gradients. The magnetic readings vary from 53,764 gammas on line 3E at 8N to 61,315 gammas on line 9W at 0+75N. Local relief is the highest on line 3E, where there is a change of 4800 gammas across 100 meters. Over 50 *Yo of the surveyed area the magnetic readings are low, < 57,400 gammas, with little or no relief.

The highest magnetic values from 57,500 to 61,000 gammas, lie in 3 distinct, discontinuous, and narrow ^ 110 meters wide) anomalous zones that are linear in shape and are between 0.5 and 1.5 km. in length. These three narrow zones are labelled the north, central and south zones. The northern zone is 50 to 75 meters in width and strikes east-northeast from line

the eastern boundary at 9+25N. 100 to 200 meters to the south, the parallel

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trending central zone, crosses the northern claim from line 11W at 3+50N to line 4E at 7+25N. The highest values exhibited in these 2 zones are situated near their eastern ends, on lines 3E and 4E. The third anomalous zone lies near the southwest boundary of the northern claim, striking east-northeast to east from line 14W to line 9W, 70 meters north of the claim boundary. It appears that this southern zone continues in a east-southeast direction across an area not on the property, then on to the southern claim till line 5W. On line 10W, where the zone is the widest (110 meters), the magnetic values are the highest found during the surveying. The highest magnetic values of these 3 zones on lines l O W, 3 E and 4E are probably caused by concentrations of magnetite across narrow widths in the northern and central zone on lines 3E and 4E and across a wider section in the southern zone on line l O W. Over their remaining lengths these zones probably represent underlying gabbro sills or Fe rich basalt with disseminated amounts of magnetite mineralization.

A fourth magnetic high forms an anomalous zone striking northeast across the northwest corner of the property. The magnetic values decrease gradually southeastward, indicating that this high could define the south boundary of the elliptical felsic to intermediate intrusive body, containing zones of mafic intrusive rocks or disseminated magnetite along the margin.

A zone of 3 weak individual highs trends east-northeast between lines 15W and 12W, 500 meters south of the intrusive body. These highs are probably caused by a unit of Fe rich basalt.

Surrounding the northern and central zones of highs, striking east-northeast across the northern claim are areas defined by broad and weak highs. Magnetic relief in these areas is less than 200 gammas, forming a wedge shaped zone 500 to 700 meters wide, broadening to the northeast. Similar strength magnetic values 0^*57, 300 gammas) form a second broad anomalous zone of weak highs 600 meters in width. This second zone strikes east-northeast in the north and east-southeast in the south, across the south part of the north claim and northern 2/3 of the south claim. These two wide zones of weak magnetic highs are probably caused by 2 bands of Mg rich basalt and/or andesite. In the southern zone, the narrow and slightly stronger highs could define intercalated zones of Fe rich basalt or sills of low magnetite gabbro.

A narrow, < 50 meters in width, set of lows (53,764 and 57,000 gammas) lies between the northern and central zones of stronger highs in the central part of the northern claim. This narrow set of lows strikes east-northeast for 1600 meters, from line HW to the eastern boundary and is caused by rocks of low magnetic susceptibilities, probably altered felsic metavolcanics surrounded by the northern and central gabbro sills or units of Fe rich basalt.

Areas of low relief, O to 100 gammas across 250 to 700 meters, exhibit values of less than 57,300 gammas and form 3 wide zones in the north, central and southern regions. The northern zone is up to 700 meters in width, striking east-northeast across the northern and northeastern parts of the northern claim. The central zone, of low relief and values, is 250 meters in width and trends east-northeast from the boundary of the 2 claims to the eastern edge of the north claim near 5N. The third and southern most zone, has a width of 300 meters and strikes east-southeast across the southern part of the southern claim. This third zone contains narrow linear lows located near it's northern edge. The magnetic results indicate that these 3 areas are also underlain by rocks of low magnetic susceptibilities, with little or no magnetite, probably felsic metavolcanics with intercalated bands of intermediate metavolcanics. The North Branch of the Porcupine Destor

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Fault Zone lies along narrow and linear lows in the north edge of the southern zone, separating the felsic to intermediate metavolcanics to the south from the basalts to the north.

A broad low lies across the western boundary at 2N at the west end of the northern and central zones of magnetic highs that represent gabbro sill or Fe rich basalt. This low may define the nose of the fold that lies at the western end of the of the fold axis lying at the intersection of the sets of east-north and east-southeast trending contours. This possible fold axis appears to trend approximately 095 degrees across the property.

The breccia zone, intersected in the drill holes, strikes east-southeast across the southwest part of the northern claim and across the northern region of the south claim. In the west this deformation zone is well delineated following a linear zone of breaks and distortions in the magnetic anomalies and sets of magnetic lows. In the east this zone trends 118 from the baseline at 4+75W through areas of low relief to line 5E at 5+25S.

VLF-Electromagnetic Survey

The rocks and overburden underlying the Wishing Well Property are highly conductive as shown by the 108 VLF-electromagnetic individual crossovers that form the 25 anomalous zones (A to Y) and two unlabelled one-line conductors crossing the surveyed area. In the chart below, the zones are described and a possible cause, with geological setting, for each zone is also shown. Zone Total Length Topography Magnetic A Geochemical Cause A Geological Setting

Strength Signatures

2 conductors line 0-near a 0.4 km. long swamp weak

along the south edge of lin ear zone of narrow lows.

D

E

2 conductors 0.3 km. long weak3 conductors 0.7 km. long moderate- L 2W, 1W, 0. weak-L IE, 2E 8i 3E.

2 conductors 0.4 km. long weak

l conductor

west end- near a creek

line 2W at a swamp

in magnetic lows.

in weak lows.

west conductor is in a weak low Si. the east conductor is in a weak high.

in a weak low.

located near the NBPDFZ (North Branch of the Porcu pine Destor Fault Zone), re presenting the fault or shears in felsic to intermediate meta volcanics near the contact with basalt.near the NBPDFZ, defining the fault or shears in felsic to intermediate metavolcanics. line 2W-conductive overbur- en.remaining conductors-Fe Se Mg rich basalt contact, pos sibly sheared .the east end lies at the inter section with the breccia zone, shears in Mg *fe Fe rich basalt /gabbro.the west end lies at the inter section with the breccia zone, shear along a basalt/gabbro fc

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Zone Total Length Topography Magnetic A Geochemical Strength Signatures

H

0.2 km. longweak2 conductors0.3 km. longmoderate -lines O 81 2E.strong-line IE.2 conductors south of an0.4 km. long andesite/bas-moderate alt outcrop,

line 4E is in a swamp.


5 conductors 1.3 km. long weak-L 15W, 8W&6W. moderate- L 13W&3W.

4 conductors line IE is in 1.4 km. long swamp, weak

within a moderate strength magnetic high.

west conductor is in a nar row low.east conductor is in a broad low.line 4E is near 126 ppm Zn (WW-ll)Aline3Eisat sample WW-25 with 7 ppm As, 22 ppm Pb Se 137 ppm Zn.line 9W is along the south edge of a high, line 6W is in a broad weak low.

line 15W is in a broad low. line 13W is in a linear high, lines 8W, 6W A 3W are along the contact between a broad low Si. a weak high.

west 3 conductors are along the south edge of a linear high.

Cause Si Geological Setting

andesite contact.

shear in basalt/gabbro & an desite south of a contact with felsic metavolcanics. possibly mineralized on line. IE.line 4E- conductive overbur den.lines 2E ft 3E-shear in felsic to intermediate metavolcan ics.

line 9W-contact between gabbro/Fe basalt and felsic to in termediate metavolcanics. line 6W-shear in felsic to in termediate metavolcanics, cut off in the east by the breccia zone.line 15W-shear in felsic to in termediate metavolcanics, near the possible nose of the fold.line 13W-shear in gabbro/Fe basalt.lines 8W, 6W & 3W-contact between Mg basalt/andesite St felsic to intermediate meta volcanics.between lines 8 fe 6W at the intersection with the breccia zone.L IE-conductive overburden, rest-contact between gabbro/ Fe basalt and andesite/Mg basalt, line 11W is at the intersection

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K

M

N

O

4 conductors [.6km. long moderate L 10, 9, 8, 7, 6, 5, 4, 7 ft 3W. strong-L 2E, 3E&4E.

2 conductors 0.6 km. long weak-lines O, 2E Si 5E. strong- L IE.

2 conductors 0.6 km. long weak-lines 4W Se 3W. strong-line 0.3 conductors 0.5 km. long moderate- L 5, 3, 2 Si 1W. strong- L 8 &7W.

4 conductors 1.3 km. long weak-L l W, 2E, 3 E, 4E &5E. moderate- L 6W, 5W,

lines 4E Si west 3 conductors are in a 5E-between weak low along the north outcrops of edge of a linear high, rhyolite and lines IE&2E are in a high, gabbro. lines 3 E Si 4E are in a broad

weak high.line 2E- soil sample WW-41 with 0.5 ppm Ag Si 129 ppm Zn, line 4E-near 117 ppm As (WW-21) and along strike from WW-01 with 45.9 ppm Cu.

along strike lines O Si IE are in a linear from shears low.in dacite & lines 2E Si 5E are along the sediments. north edge of a linear high,

line O- 11 ppb Au in WW-60.

line 0-west of an outcrop of gabbro.

along the west edge of a high.

Cause Si Geological Setting

with the breccia zone, the west 3 conductors-shear ed contact between felsic metavolcanics and gabbro/Fe basalt, the west end is cut off by the breccia zone, lines IE to 4E-shears in gab bro, basalt and andesite, possibly mineralized on lines 2E, 3E, Si 4E.

lines O ft IE- shear in felsic metavolcanics, mineralized- line IE.lines 2E- sheared contact be tween felsic metavolcanics Si Fe rich basalt/gabbro. line SE-shear in gabbro/Fe rich basalt.shear in gabbro/Fe rich basalt, possibly mineralized on line 0.

line 2W- west conductor is in an area crosses a of low values and relief, creek. eastern 2 conductors are a-

long the north edge of a weak and broad high.

lines 2E to in areas of low relief, with 5E along a the west conductor in a creek weak low and the east con

ductor is in a weak high near contacts with weak, narrow lows.

west conductor-mineralized shear in felsic to intermediate metavolcanics. eastern 2 conductors- shear along a contact between felsic to intermediate metavolcanics Si andesite/Mg rich basalt, lines 2E to SE-conductive overburden.lines 6, 5 Se 4W-shear in fel sic to intermediate metavol canics.lines 1W Si 0-sheared contact between felsic and intermed-

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4W&0.

R

U

7 conductors 1.5 km. long weak-L 10W, 8W, 3W, IE, 3E & 4E. strong-L 7W &5W.


l conductor0.2 km. longweakl conductor0.5 km. longweak

4 conductors 1.2km. long

l conductor 0.3 km. long moderate l conductor 0.2 km. long weak

lines IE, 3E St 4E are near a pond, line 10W is near outcrop of rhyolite flow breccia & dacite, line 11W is in a swamp.

the western 5 conductors are in the north part of weak lows in a large area of low relief.

along the south edge of a broad high.

in areas of low values and relief.

crossing the contour pattern in an area of low relief ft on line 12W it lies at the east end of a high.

crosses the contour pattern, the western 2 conductors Se the conductor on line 7W are in areas of low values & re lief.on lines 6, 5 St 3 W the con ductors cross highs.

crossing weak highs.

along the north edge of a broad low.

Cause A Geological Setting

iate metavolcanics. lines 5 W Se 6W are along strike from carbonate altera tion in pillowed rhyolite, lines IE, 3E A 4E-conductive overburden.western 5 conductors- shear in felsic to intermediate meta volcanics.lines 7W Se 5W may be min eralized, lying 50 m. south of mineralization in dacite, line l IW-conductive overbur- en.rest-shears in intermediate metavolcanics, south of the intrusive body, shear in felsic to intermediate metavolcanics.

cross-cutting shear in felsic to intermediate metavolcanics, cut off in the southwest at the intersection with the breccia zone.the western 2 conductors St, the conductor on line 7W- cross-cutting shears in felsic - intermediate metavolcanics. possibly mineralized on lines 12W and 9W.lines 6W, 5W & 3W-shears crossing gabbro/Fe basalt, cross-cutting shears in felsic to intermediate metavolcanics and Fe basalt/gabbro. shear in felsic to intermediate metavolcanics, near the nose of the possible fold Se east of Fe basalt/gabbro.

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Total Length Topography Strength

W 2 conductors 0.5 km. long moderate- L 1E&4E. strong- L 2E &3E.l conductor 0.3 km. long moderate- line 5E. strong-L 4E. l conductor 0. l km. long weak

line 4E is in a creek.

south of out crops ofrhy olite, dacite fc andesite.

near outcrop of slightly mineralized dacite.

Magnetic A Geochemical Signatures

lines IE fe 2E are in a broad and weak high, lines 3 E ft 4E are in highs, the east end of the east con ductor is near sample WW- 22 with 0.4 ppm Ag. crossing weak high A low. located at sample WW-19 with 0.4 ppm Ag.

in area of low values and no relief.

Cause A Geological Setting

line 4E-conductive overburd en.rest-shears in Mg rich basalt and andesite, mineralized on lines 2E&3E.

cross-cutting shear in felsic to intermediate metavolcanics, mineralized on line 4E.

shear in felsic to intermediate metavolcanics, near the 3 channel Input anomaly.

Prospecting. Geological Mapping and Rock Sampling Programs

During the detailed prospecting program the topography and vegetation on the property was well defined. The claim boundaries are well blazed, marked with flagging tape and easily followed in the bush. In the northern claim, 1140876, all 16 posts were found and 8 posts in the surveyed area were mapped along the boundaries of the southern claim (1225710). The casing of diamond drill hole LR87-4 was located, producing water near the baseline at 3+75W.

Since the prospecting traverses were run at intervals of 100 meters or less, all the outcrops on the Wishing Well was found and prospected in detail. There are large exposures of outcrop forming hills in the eastern part of claim 1140876. Smaller outcrops are exposed in the north-central, southwest and central parts of this claim. In the southern claim, a large hill of bedrock was found 230 meters southeast of the drill collar and small outcrops lie across the southern boundary at the east end of the areas surveyed.

Outcrops of felsic metavolcanic rocks are predominant in the exposures mapped over the grid. Exposures of rhyolite and dacite were found concentrated in the eastern part of the northern claim and scattered in the north-central region of this claim. The felsic metavolcanic outcrops in the north-central region are positioned over areas exhibiting low magnetic values with little or no relief.

The western and southeastern felsic metavolcanic outcrops vary in composition, from rhyolite to dacite, with the contacts being graditional. Most of these outcrops are fine-grained massive, yellow to black in colour and very siliceous lavas which contain intercalations of flow breccia, zones of amygdaloidal dacite and sills or bands of feldspar porphyry. In the southeast, cross-cutting VLF anomaly X crosses the area between two distinct sets of outcrop in central zone of low magnetic values and relief. Pillowed structures were observed in rhyolite and dacite exposures in the north part of the grid and in the top of the hill on line 3E between 4N and 5N.

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Rhyolite lava and breccia and cherty tuff/breccia grade into each other in 2 small outcrops near line 10W, in the vicinity of lines 9w and 7W. Generally, the contacts between the rhyolites and dacites were gradational but distinct contacts were observed striking 060 to 080 degrees between: rhyolite flow breccia/fine-grained rhyolite lava and fine-grained dacite lava near line 3E at 7+25 to 7+5 ON; and interbands of rhyolite flow breccia, feldspar porphyritic rhyolite and massive dacite lava in the western part of the outcrop on line 3 E, between 4 and 5N. These contacts dip steeply to the north in the north and steeply to the south in the south.

Massive dacite lava also exists in individual outcrops: on line 3E at 7+10N; on lines O and IE at ION; on line 4W at 11+50N; and near lines 6W and 5W at the northern boundary. The dacite outcropping on line 4W at 11+5 ON lies 100 meters west of the position of the airborne Input anomaly. The large outcrop north of the road, between 6+50 and 7+50N on lines 3 and 4E, is mostly comprised of massive east-northeast striking dacite, grading into massive rhyolite in the south and andesite in the central part of the outcrop. Small zones of interflow shale and siltstone, narrow chert pyroclastic horizons and feldspar porphyritic rhyolite sills strike parallel to the lineation observed in the massive dacite lava.

Andesite lava, which is massive, fine-grained and dark green in colour, outcrops in small exposures located near outcrops of felsic metavolcanics and in contact with these felsic rocks in the eastern part of the northern claim. In a small outcrop on line 2E at 3+50N the andesite grades into black, massive basalt. The large outcrop exposed along and on top of the hill in the northwestern part of the southern claim is comprised of andesitic to basaltic, fine to medium-grained lava and pillow lava. These contacts are gradational, with the basalt being exposed mostly along the edges of the hill.

Exposures of fine to medium-grained gabbro were mapped in the north claim, at various locations including: in small outcrops near and in contact with felsic metavolcanics in the vicinity of line 4E at 6N; in a small outcrop and a large exposure forming the north part of a hill between lines O and 4E at 7 to 9N; in small individual outcrops located near the road in the central part of this claim; and in the southwest region between lines 10 and 9W at IN. Two small outcrops of gabbro were also found in the southern claim at the southeast corner of the grid. The gabbros are mostly fine-grained, grading into medium-grained in the east part of the northern claim, unaltered, non magnetic and slightly fractured. Little or no magnetite was observed in the exposures.

The felsic metavolcanics in the eastern part of the northern claim are well lineated and contain numerous shear zones that strike 80 to 90 degrees. The shear zones are up to 2 meters in width and one is exposed at irregular intervals in interflow sediments and massive dacite lava over 70 meters along the south side of the hill, north of road on lines 3E and 4E. This series of shears lies along the south edge of a strong magnetic high, between 2 conductors of VLF-EM anomaly L. Geochemical soil sample WW-43, with 0.4 ppm Ag is situated along strike, 100 meters to the west of this zone of shears. Parallel striking shears cut dacite and cherty tuff, 10, 30 and 40 meters to the north. Shearing was also observed in the larger felsic metavolcanic outcrop south of the road. The felsic metavolcanics in the north-central region are slightly fractured, but otherwise undeformed. No deformation was mapped in the andesite, basalt and gabbro.

Alteration and quartz veining was also found within the felsic metavolcanic outcrops. Hematite, carbonate and epidote alteration were observed in the east and north-central outcrops, including: up to 207o carbonate in the margins of pillows near line 7W at 9+50N (sample 61512)

22

that lies along strike 50 meters west of a conductor of VLF-EM anomaly O; carbonate and epidote within massive dacite in the large outcrop on line 3E at 5N (sample 61502); and hematite in sheared dacite (sample 61508), in massive rhyolite lava and in intercalations of cherty tuff and breccia. Quartz veins, barren of mineralization and up to 10 cm. in width, strike east-northeast and north-northeast through the felsic metavolcanics in the eastern part of claim 1140876. Samples 61512 and 61508, with carbonate and hematite alteration, contained very small amounts of Au, 6 and 3 ppb, respectively. Minor epidote alteration was observed in a 10 cm. quartz vein cutting massive dacite near line 3E at 5N.

The altered and deformed felsic metavolcanic rocks and interflow sediments in the east are also well mineralized with up to 10 y0 pyrite and magnetite and trace amounts of chalcopyrite. The outcrops of dacite and rhyolite in the north-central region contain lesser amounts of pyrite, trace to 2 "/o. There appears to be good correlation between the shearing, alteration and the amount of mineralization in the felsic metavolcanics and interflow sediments. Along the southern part of the hill, that lies north of the road near lines 3 E and 4E, three shears in dacite and interflow sediments are intermittently exposed over 70 meters and are highly mineralized with up to W/o pyrite and magnetite. The sheared interflow sediment in massive dacite, between lines 3 E and 4E at 6N, forms the west end of this zone, hosting 5 to 10 ^o disseminated pyrite and magnetite. Sample 61509 of sediments and mineralization at the west end assayed 4 ppb Au and 1.9 ppm Ag. Sheared dacite is exposed 50 to 70 meters, along strike to the east-northeast, containing up to 8 Vo pyrite and trace magnetite (61508 and 61506). Sample 61508 of two parallel trending shears with weak hematite alteration and 5 to 8 Vo pyrite and trace magnetite, 50 meters east of 61509 was shown to contain 5 ppb Au and 1.6 ppm Ag. At it's east end, the zone was uncovered across l meter and sample 61506 with up to 5 07o disseminated pyrite was collected there, assaying 5 ppb Au and 1.7 ppm Ag. The magnetic high on line 3E at 6+87N also lies along strike from the mineralized shears, with the high extending 350 meters to the west-southwest.

Approximately 10 meters north of the east end of the 70 meter shear, in the same exposure, another similar trending shear was exposed across 2 meters. Sample 61507, a chip sample over 1.5 meters, was collected in this sheared and mineralized (IVo pyrite) dacite, assayed low in Au (4 ppb). Small mineralized shears in dacite were also mapped 40 meters north and 40 meters south of the 70 meter zone. These small shears contained 2 to 5 0A pyrite in dacite (sample 61510 with 5 ppb Au and 1.9 ppm Ag) and l Vo pyrite and trace amounts of chalcopyrite. Also in the same outcrop, at it's extreme southeastern edge, an example (sample 61505) of rhyolite and minor shale, containing l Yo pyrite and trace amounts of chalcopyrite, was found to host 5 ppb Au.

The outcrops of rhyolite and dacite, located south of the road between lines 3E and 5E, also contain mineralization, generally trace amounts to Wo pyrite, as found in sample 61501, with 6 ppb Au, collected in the small northern outcrop. Anomalous amounts, up to 5 07o pyrite, were found (61503 and 61504) in the larger outcrop to the southwest. Sample 61503 of rhyolite flow breccia, 5 07o pyrite and trace chalcopyrite was found to host low amounts of precious and base metals (6 ppb Au, 1.8 ppm Ag, 189 ppm Cu and 68 ppm Zn). Twenty meters to the southwest, mineralized, sheared and fractured rhyolitic to dacitic massive lava was sampled (61504), assaying 8 ppb Au and 1.5 ppm Ag. Anomalous amounts of Au, Ag, As, Cu and Zn in soil samples were collected near these felsic metavolcanics south of the road, including: WW-27 with 16 ppb Au

23

and 54 ppm As, located 10 meters west, along strike from the mineralized shear/fracture zone (rock sample 61604); WW-37, 52 and 53, containing 126, 136 and 144 ppm Zn, respectively, and WW-36 with 18 ppb Au, all lie 150 to 200 along strike of the western outcrop; WW-17, 19 and 21 with anomalous Zn, Ag and As (135, 0.4 and 117 ppm, respectively) are positioned within 50 meters of the east outcrop; and WW-01 containing 45.9 ppm Cu, 50 meters north of the eastern outcrop.

In the outcrops of rhyolite and dacite scattered in the north-central part of the northern claim examples of l to 2 07o pyrite were uncovered and sampled. An example of mineralized rhyolite flow breccia, sample 61511, lying 50 meters west of the east end of conductive zone P contained the highest Au assay reported (9 ppb). Sample 61513 of l 0A pyrite in dacite with only 6 ppb Au, is located 50 meters north of the axis of conductive zone P on line 4W. Conductive zone Y, a one line conductor, situated on line 3W near the airborne Input anomaly, lies 100 meters east, along strike from sample 61513.

CONCLUSIONS AND RECOMMENDATIONS

After compiling and interpreting the data collected during the exploration program completed on the property, the geology in areas of outcrop exposures has been well delineated and the geological, geophysical and geochemical signatures in overburden covered areas have been outlined. The Wishing Well Property appears to be underlain by felsic to mafic metavolcanics of the Kidd Munro and Stoughton-Roquemaure Assemblages, lying south of a felsic to intermediate intrusive body, and which have been intruded by sills of gabbro. Felsic to intermediate metavolcanics are thought to underlie 50 07o of the property surrounding 2 bands of mafic to intermediate metavolcanics that have been intruded by narrow gabbro sills. These rocks may be folded and are mineralized, altered and deformed with: alteration and mineralization being observed in the felsic to intermediate metavolcanics; shearing being exposed in felsic metavolcanics and interflow sediments in the eastern part of the northern claim; the North Branch of the Porcupine Destor Fault Zone lying along a 102 degree contact between mafic/intermediate and felsic/intermediate metavolcanics in the southern claim; a major breccia zone striking 118 degrees through the metavolcanics in the south; and 25 VLF-EM anomalies representing potential shearing, with 8 of these anomalies possibly defining concentrations of sulphide mineralization. Elevated to anomalous amounts of precious and base metals and Cu in soil samples lie near mineralized, altered and sheared felsic metavolcanics in the east.

Magnetic responses and the positions of outcrops show that two wedge shaped bands of mafic to intermediate metavolcanics, probably massive and fine-grained lavas of Mg rich basalt and andesite of the Stoughton-Roquemaure Assemblage, 400 to 700 meters in width, strike east-northeast to east-southeast across the central and southern regions. The northern band is 500 to 700 meters wide, contains two fine to medium grained gabbro sills or units of Fe rich basalt, and strikes east-northeast east-northeast through the northern claim. Between the two gabbro sills/Fe rich basalt in this band lies a horizon of felsic metavolcanics, dacite lava with narrow zones of rhyolite and chert breccia and interflow sediments. Approximately 300 to the south, a second,

24

400 to 700 meter wide, band of Mg rich basalt and andesite, with small intercalations of Fe rich basalt and sill of gabbro, trends east-northeast and east-southeast through the southern part of the northern claim and north-central part of the southern claim, broadening eastward. A 100 meter wide gabbro sill lies north of this second band, near the west end of the boundary between the two claims.

These two bands of mafic to intermediate metavolcanics and gabbro sill in the west are surrounded by felsic to intermediate metavolcanics in three wide bands, covering approximately 50 *Yo of the property. Magnetic data indicates that the northern band is 500 to 700 meters wide and is exposed on surface in scattered outcrops of rhyolitic and dacitic massive and pillow lava with narrow zones of cherty tuff and flow breccia. It strikes east-northeast through the northern part of the northern claim and the southern edge of the felsic to intermediate intrusive body intrudes the metavolcanics across the extreme northeastern corner of the property. The central felsic to intermediate band is narrower, 250 meters, and is exposed in outcrops containing rhyolite and dacite lavas (massive fine-grained and amygdaloidal), pyroclastic horizons (tuff and flow breccia) and feldspar porphyries. In the extreme southern part of the grid, as defined from the magnetic results, lies the southern wide band of felsic to intermediate metavolcanics of the Kidd Munro Assemblage, south of the North Branch of the Porcupine Destor Fault Zone and in contact with mafic to intermediate metavolcanics of the Stoughton Roquemaure Assemblage to the north.

The felsic metavolcanic rocks exposed on the property are also mineralized with up to 10 'Yn pyrite and magnetite and trace amounts of chalcopyrite. In the eastern part of the north claim including: the narrow horizon of felsic metavolcanics, north of the road, in contact with the two sills of gabbro or Fe basalt units; and the outcrops south of the road that form the 250 meter wide central band. These felsic metavolcanics are mineralized, altered (hematite, carbonate and epidote) and deformed (sheared and fractured), contain small barren quartz veins and stringers and they lie in an area containing elevated to anomalous amounts of Au, As, Ag, Zn, Pb and Cu in soil samples. Shearing, mineralization and alteration is the most prevalent in an outcrop of dacite that is exposed along the south side of the hill, north of the road and that forms the east end of the narrow felsic horizon in contact with gabbro or Fe rich basalt. A mineralized shear has been uncovered intermittently along a length of 70 meters in an interband of altered sediment and massive dacite, overlying a magnetic high and lying between two conductors of VLF-EM anomaly L. The geophysical results indicate that the mineralized shear may extend 100 meters to the east-northeast and 250 meters to the west-southwest. Parallel trending and mineralized shear zones cut the felsic metavolcanic rocks within 40 meters of this zone of shears.

All the precious and base metal and Cu assays of the 13 samples collected in outcrops of altered, sheared and mineralized felsic metavolcanics were low. The highest Au assay of 9 ppb was in a sample of rhyolite flow breccia collected in the northern part of claim 1140876.

Parts or all of the 25 VLF-EM conductive zones may represent shearing forming an extensive system of shears in the metavolcanics and gabbros and along their contacts and the North Branch of the Porcupine Destor Fault Zone. The breccia zone, delineated in the drill holes, cuts off or intersects with conductors of 6 VLF-EM anomalous zones. The unexplained airborne Input anomaly is situated over anomaly Y near outcrops of slightly mineralized dacite lava.

25

The results of the exploration program prove that the felsic to mafic metavolcanics and the south edge of the felsic to intermediate intrusive body that underlie the two claims have the potential to host Au, Ag, Cu, Pb and Zn in mineralized zones, shear and fault zones, quartz veining and in alteration, as outlined previously in this report. Examples of mineralization, shearing, alteration and quartz veining have been found in the felsic metavolcanic exposed on the property. These felsic metavolcanic rocks are more widely exposed and magnetic data indicates that 3 bands of felsic to intermediate metavolcanics extend over larger areas than previously indicated before the 1999 exploration.

The felsic lavas and pyroclastic horizons, interbands of sediments and the narrow feldspar porphyries in outcrops are favourable geological environments for mineral deposition and there are numerous examples of geological/geophysical/geochemical anomalies in overburden covered areas that represent targets for potential mineralization, including:

1) VLF-EM conductors representing shearing in favourable geological environments and potential sulphide mineralization, including:- Zone F: line IE, mineralization in basalt near a contact with felsic to intermediate

metavolcanics.- Zone I line 3 W, shear along a contact between Mg rich basalt/andesite and felsic

intermediate metavolcanics.- Zone K lines 11W to 3 W, shear along a felsic to intermediate metavolcanics and Fe

basalt/gabbro contact.lines IE to 4E, shear in Mg rich basalt and andesite, possibly mineralized on lines 2E, 3E St 4E.

- Zone L shear in felsic metavolcanics and gabbro/Fe rich basalt, mineralized line IE near the 70 meter mineralized shear.

- Zone M line O, mineralized shear in gabbro/Fe basalt.lines 8W fc 7W, mineralized shear in felsic to intermediate metavolcanics.

- Zone N lines 5W, 3W, 2W te IW, sheared contact between felsic to intermediate metavolcanics and basalt/andesite.

- Zone O lines 6W, 5W fe 4 W, shear in felsic to intermediate metavolcanics along strike from carbonate alteration in pillowed rhyolite, lines l W 8c O, sheared contact between felsic and intermediate metavolcan ics.

-ZoneP lines 10W to4W, shear in felsic to intermediate metavolcanics, possibly mineralized lines 7W Si. 5 W, line 5W is 50 meters south of pyrite in dacite.

- Zone T lines 13 W to 7W, cross cutting shear in andesite 8t Mg rich basalt, possibly mineralized on lines 12W and 9W.

- Zone W lines 2E and 3E, mineralized shear in andesite and Mg rich basalt.- Zone X cross cutting shear in felsic to intermediate metavolcanics, possibly miner

alized on line 4E.- Zone Y line 3 W, shear in felsic to intermediate metavolcanics, near mineralized

dacite outcrop and Input anomaly.2) VLF-EM conductors near the North Branch of the Porcupine Destor Fault Zone:

- Zone A and B in felsic to intermediate metavolcanics.

26

3) VLF-EM conductors at the intersection with the breccia zone:- Zones C (line 4E), D (line 0), H (line 6W), I (line 8W), J (line 11 W), K (line 11W)

and S (line 12W) and the one line conductor on line 15W at 5+25N.4) VLF-EM conductors with coincident geochemical soil anomalies:

- Zone G line 3E A WW-25 (7 ppm As, 22 ppm Pb Se 137 ppm Zn)- Zone K line 2E fe WW-41 (0.5 ppm Ag A 129 ppm Zn)

line 4E A WW-21 (117 ppm As)-Zone X line5EAWW-05(45.7ppm)

Because of the positive results obtained during the 1999 program of exploration, in outlining mineralization, deformation, quartz veining and alteration in outcrops of felsic metavolcanics and in delineating the potential of the rocks under overburden cover to host Au, Ag, Cu, Pb and Zn, further work is warranted. A horizontal loop-electromagnetic should be performed over the grid to better define and classify the numerous VLF-EM anomalous zones. After the HLEM surveying is completed and interpreted the anomalous zones should be detailed by using induced polarization. The I.P. anomalies should then be tested by a program of diamond drilling.

Respectively submitted,

Dec. 15, 1999 Bellecombe, Quebec

ftR. A. Campbell, B. Se., Geologist

G.N. Henriksen, B.Se., APGGQ, Geologist

27

REFERENCES

Ayer, J. A.1999: The Abitibi Greenstone Belt: a Program Overview, O.G.S. Misc. Paper 169, p. 11-13.

Ayer, J. A, Trowell. N.F., Amelin, Y. and Corfu, F.1999: Project Unit 95-2, A Geological Compilation of the Abitibi Greenstone Belt in Ontario: To

ward a Revised Stratigraphy Based on Compilation and New Geochronology Results, O.G. S. Misc. Paper 169, p. 14-24.

Ayer, J.A., Berger, B.R. and Trowell, N.F.1999: Geological Compilation of the Lake Abitibi Area, Abitibi Greenstone Belt; O.G. S. Map

P.3398, scale 1:100,000.

Berger, B. and Amelin, Y.1999: Project 97-024, Geological Investigations Along Highway 101, Guibord, Michaud and Gar

rison Townships, O.G.S. Misc. Paper 169, p. 25-32.

Jensen, L. S.1982: Precambrian Geology of the Ghost Range Area, Lightning River Area, Cochrane District,

Ontario Geological Survey, Map P.2431, Geology Series-Preliminary Map, Scale l: 15,840or l inch to Vi mile, Geology 1973.

Jensen, L.S. SL Langford, F.F.1985: Geological and Petrogenesis of the Archean Abitibi Belt in the Kirkland Lake Area, Ontario

O.G.S. Miscellaneous Paper 123.

Jensen, L.S. 8z. Langford, F.F.1985: Precambrian Geology of the Lightning River Area, Cochrane District, O.G.S. Map P.2433,

Scale 1:63,360, Mapping completed in 1973.

Lainstra, B. and Benn, K.1999. Project Unit 97-013, Structural Investigations of the Holloway Mine and Vicinity, O.G.S.

Misc. Paper 169, p. 33-38.

Lovell, H. J. Si Frey, E. D.1973: Lamplugh Twp., District of Cochrane, O. D. M., Preliminary Map P.799, Kirkland Lake

Data Series, Scale l inch to Vi mile. Data compiled 1972.

Ontario Geological Survey1986: Lamplugh Twp., Sonic Drill Hole 85-42, Overburden Geochemistry Map 80880.

Ontario Geological Survey1986: Lamplugh Twp. Overburden Geochemistry Map 80839.


Ontario Geological Survey

28

1989: Lamplugh Twp. Sonic Drill Hole 88-21, Overburden Geochemistry Map 81154.





Ontario Geological Survey1984: Airborne EM and Total Intensity Magnetic Survey, Matheson-Black River Area, Lamplugh

Township, District of Cochrane; by Questor Surveys Ltd. for the O. G. S., Map 80588, Geophysical/Geochemical Series, Scale 1:20,000, Survey A Compilation March-July, 1983.

Pyke, D. R., Ayres, L. D., and Inness, D. G.1973: Timmins-Kirkland Lake Geological Compilation Series, O. D. M., Map 2205, Scale l inch

equals 4 miles, Geological Compilation 1970-1971.

Ropchan, J.C., Nattress, S.D. and Fowler, A.D.1999: Project Unit 97-014, Petrographic and Geochemical Studies of the Alteration Zones Assoc

iated with the Au Mineralization at the Holloway Mine and the Down-Dip Extension of the Holt-McDermott Deposit, Southwest Abitibi Greenstone Belt, O.G.S. Misc. Paper 169, p. 39-42.

Sharpley, F. J.1986: Report on the Geophysical Surveys, Lightning River Project for Pronto Exploration by Seal

River Exploration Ltd.

Sharpley, F.J.1991: Exploration Report on the Lightning River Property, Lamplugh Twp., Seal River Explora

tion.

Sharpley, F.J.1992: Report on the Lightning River Property, Harker-Holloway Area, Seal River Exploration.

Vagners, U. J. and Courtney, S. L.1985: Quarternary Geology of the Lightening River Area, District of Cochrane, O. G. S., Geolog

ical Series Preliminary Map P.2734, Scale 1:50,000, Geology 1983.

APPENDIX l

CERTIFICATES OF ANALYSIS

Page l

XRAL LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC.

129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 7B9TEL.: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Norn de la Compagnie/Company: Gordon N. HenriksenBon de Commande No/ P.O. No:Projet/ Project No :Date Soumis/ Submitted : Aug 27, 1999Attention : Robert Campbell

R16599

Oct 07, 199

No. D'Echantillon AU Sample No. PPB

AU CHK AG CU ZN PPB PPM PPM PPM

61501615026150361504615056150661507615086150961510615116151261513

6368554545966

101.8 1.5

1.7

1.6 1.9 1.9

189 68

Certifie par Certified by :®SGS imbre du Groupe SGS (Sotiete Generate de Surveillance)

Page l

XRAL LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC.

129 AVE. MARCEL BARIL * ROUYN-NORANDA - QUEBEC J9X 7B9TEL: (819) 764-9108 FAX: (819) 764-4673


Nom de la Compagnie/Company: Gordon N. HenriksenBon de Commande No/ P.O. No:ProjetX Project No :Date Sounds/ Submitted : Aug 27, 1999Attention : Robert Campbell

No. D'Echantillon AUAU CHKSample No. PPB PPB

R16600

Oct 07, 1999

WW1WW2WW3WW4WW5WW6WW7WW8WW9WW10WW11WW12WW13WW14WW15WW16WW17WW18WW19WW20WW21WW22WW23WW24WW25WW26WW27WW28WW29WW30WW31WW32WW33WW34WW35WW36WW37WW38WW39

253635468645519121288451095686169991099121218121410

Certifie par l CertifiedGroupe SGS (Societe Generate de Surveillance)

XRAL LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE 7 A DIVISION OF SGS CANADA INC.

129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 7B9TEL: (819) 764-9108 FAX. (819) 764-4673


Norn de la Compagnie/Company: Gordon N. HenriksenBon de Cornmande No/ P.O. No:Projet/ Project No :Date Sounds/ Submitted : Aug 27, 1999Attention : Robert Campbell

No. D'Echantillon AUAU CHK Sample No. PPB PPB

R16600

Oct 07, 19 l

WW40WW41WW42WW43WW44WW45WW46WW47WW48WW49WW50WW51WW52WW53WW54WW55WW56WW57WW58WW59WW60WW61WW62WW63WW64WW65WW66WW67 'WW&8WW69WW70WW71WW72WW73WW74WW75WW76WW77WW78

12846686676118888812151512111512111315121112910107569664

10

11

Membre du Groupe SGS (Societe Generale de Surveillance)

XRALPage 3

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE t A DIVISION OF SGS CANADA INC.

129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 7B9TEL: (819) 764-9108 FAX: (819) 764-4673


R16600Nom de la Compagnie/Company: Gordon N. Henriksen Bon de Commands No/ P.O. No: Projet/ Project No :Date Sounds/ Submitted : Aug 27, 1999 Oct 07, 1999 Attention : Robert Campbell

No. D'Echantillon AUAU CHK Sample No. PPB PPB

WW79 9WW80 6 5

Membre du Groupe SGS (Societe Generate de Surveillance)

COm -o

KRAL XRAL LaboratoriesA Division of SGS Canada Inc.

Work Order: 056633 Date: 13/09/99 FINAL Page l nl 9

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Element. Method. Det.Lim. Units.

W W WO l WWW02 WWW03 WWW04 WWW05

WWW06 WWW07 WWWOS WWW09 WWW 10

WWVVl) WWW 12 WWW 13 WWW 14 WWW 15

WWW 16 WWW 17 WWW l X WWW 19 WWW20

WWW21 WWW22 WWW23 WWW24 WWW25

WWW26 WWW27 WWW 23 WWW29 WWW30

BeK.'P70

O.Sppm

0.8^).5

1.01.11.0

0.70.80.80.90.8

0.80.5U.50.8

c 0.5

cO.50.50.90.9

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0.6-c 0.5T 0.5^-0.5

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NaICP70

0.01ft

0.040.020.040.030.04

0.050.040.040.030.05

0.030.030.030.040.02

0.020.040.040.040.02

0.040.040.040.020.03

0030.030.020.030.04

MgICP70

0.01ft

1.300.281.490.601.43

1.401.371.11.04.45

.27

.30

.36

.320.24

0.211.191.191.070.2)

1.171.161.130.401.16

1.191 030.250.861.24

Al1CP70

0.01ft

3.031.643.422.533.07

2.793.002.933.032.91

3.172.842.913.060.84

2.373.223.523.140.83

2.882.752.721.032.69

2.681.702.241.802.92

PICP70

0.01ft

0.040.030.040.100.06

0.060.060.080.090.06

0.060.050.050.060.05

0.190.060.090.070.10

0.040.030.030.060.06

0.050070.070.020.08

KICP70

0.01ft

o.3y0.040.480.230.52

0.470.460.350.380.50

0.400.360.400.470.04

0.030.300.390.290.03

0.340.350.320.080.37

0.370.060.030.160.41

CaJCP70

0.01?o

0.610.200.802.521.07

1.030.941.111.092.44

0.980.820.881.240.17

0.240.750,911.200.13

0.410.410.380.210.88

0.490.390.080.451.67

SeICP70

0.5ppm

7,41.68.65.38.2

7.67.87.57.37.7

7.06.16.57.30.9

2.26.37.37.01.0

5.85.85.81.65.4

5.93.02.33.96.6

TiICP70

0.01fc

0.120.060.110.030.10

0.110.100.080.070.11

0.080.120.120.090.09

0.070.070.060.080.07

0.150.150.150.080.10

0.130.170.000.110.08

V1CP70

2ppm

7225744070

6966645669

6880776648

7058676354

6663633471

69126565960

CrICP70

1ppm

8433895285

10188

1059880

8877818226

5380837431

8281797073

77104396--I80

Mn1CP70

2ppm

75986

738147346

36634751?409391

572718990903151

20039545?568

63

52648547?181826

64146910249*582

FeICP70

0.01ft

4.241.754.692.724.03

3.793.764.083.784.12

4.104.344.444.232.54

4.653.784.303.812.12

3.543.353.281.774.00

3.964.543.022.823.75

Co1CP70

Jppm

216

205

18

1618171517

18212419

3

41416142

1514135

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1920j

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Work Order: 056633 Date: 13/09/99 FINAL Page 2 of

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WWW41 WWW42WWW43 WWW'14 WWW45


WWWS1 WWW52 WWW'53 WWW54 WWW55

WWWf6 WWW57 WWW'S WWW59 WWW60

BeICP70

0.5ppm

0.70.6

c 0.5 CO. 5<0.5

0.90.70,70.70.8

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MaICP70

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0.040.040.020.030.02

0.030.040.040,030.04

0.040.040.040.040.04

0.040.030.030.020.04

0.040.030.040.040.04

0.040.040.040.040.04

MgICP70

0.01ft

1.231.240.310.430.19

.25

.05

.22

.24

.23

.340.961.280.981.43

1.351.31.14

0.40.31

1.411.151.31.32

1.2)

0.690.571.201.411.39

AlICP70

0.01ft

2.832.852.022.281.17

3.663.242.933.043.00

3.692.063.042.183.39

3.083.062.610.613.09

3.413.373.653.032.84

2.111.652.982.953.35

PICP70

0.01ft

0.040.030.110.080.05

0.090,090.070.070.06

0.080.030.030.020.05

0.050.040.040.040.03

0.050.070.090.040.05

0.040.030.080.040.06

KICP70

0.01ft

0.370.370.020.060.03

0.450.330.400.390.42

0.490.260.380.250.45

0.440.420.360.090.42

0.450.360.590.480.42

0.130.120.420.460.55

Ca1CP70

0.01ft

o.so0.400.130.190.12

0.841.080.890.920.81

1.090.480.400.320.55

0.710.520.450.210.38

0.870.920.840.480.37

0.260.270.970.810.84

SeICP70

0.5ppm

7.06.02.42.21.0

6.76.67.26.97.0

7.24.66.14.27.7

7.46.75.61.45.7

7.46.67.16.05.2

3.02.57.26.67.4

TtICP70

0.01ft

0.120.150.090.060.04

0.080.070.100.090.10

0.080.130.150.150,13

0,120.120.120.050.17

0.120.100.080.160.16

0.110.09O.JO0.120.09

VICP70

1ppm

6970733022

7560676870

7156715781

7675652474

8375778076

4740647580

CrICP70

1ppm

7776564423

8676787878

9061786693

8380

1022885

8684888982

10915?

818884

MnICP70

2ppm

664624

8413269

688720493790612

646548649478803

1770748629191617

821556773943

1430

262228500963

1640

FeICP70

0.01ft

3.913.923.671.951.37

4.673.714.124.254,08

4.542,903.992.824.61

4.884.383.731.204.00

4.773.844.534.283.96

2.622033.664.284,64

CoICP70

1ppm

1816463

1915161718

171417122i

2822186

17

2115192423

98

162331

CO-o-3

x:x-t i 30rooTO

12mCO

~n

x:

g

ji.OT.e*-c*.en;fien ro

1"T-l

Member of the SGS Group (80086 Generate de Suivefflartoe)Oco


Work Order: 056633

Element.Method.Det.Lim.Units.

\v\y\VG iWWW62 WVVWGj WWW64 WWW65

WWW66 WVVW67 WWW68 WWVV69 WWW70

WWVV71 WWW72 WWW73 WWW74 WWW75

WWW76 WWW7? WVVW73 WWW79 WWW80

*Dup WWW01*DupWWWJ3*Dup WWW25*Dup WVVW37*Dup WWW49

*DupWWW61*Dup WWW73

Date: 13/09/99 FINAL 3 01 9

COm-oi

OJ

CO CD

CO-e*

BeICP70

0.5ppm

0.90.80.80.60.9

1.10.90.7

^0.50.6

0.70.70.70.70.7

0.70.70.80.80.6

0.80.50.60.7

K: 0.5

0.80.6

NaICP70

0.01K

0.050.040.040.040.04

0.050.040.040.040.06

0.060.070.060.060.06

0.060.060.060.060.05

0.040.030.030.040.02

0.050.06

Mg1CP70

0.0 1Ve

1.601.381.331.331.45

1.47i. 481.260.931.68

1.781.681.641.661.55

1.591.501.571.481.33

1.361.391.141.080.41

1.571.67

AlICP70

0.019fc

3.453.073.163.003.46

3.873.482.832.062.82

2.852.962.852.952.92

2.952.742.912.932.70

3.232.992.663.350.62

3.402.91

P1CP70

0.01ft

0.050.060.060.030.05

0.060.050.050.030.06

0.060.060.060.060.06

0.060.060.060.060.06

0.040.040.060.090.04

0.050.06

K1CP70

0.01'?6

0.630.530.510.430.60

0.610.530.400.250.57

0.550.580.540.570.55

0.550.520.560.540.48

0.420.410.3(50.340.09

0.610.55

CaICP70

0.01Ve

0.750.760.780.530.75

0.900.730.640.451.84

2.291.801.771.751.27

1.451.331.611.311.08

0.630.870.851.090.22

0.731.79

SeICP70

0.5ppm

S.67.47.56.28.4

9.18.66.64.97.5

7.77.87.47.97.5

7.87.37.87.76.9

7.76.55.36.91.4

8.47.6

TiICP70

0.01ft

0.120.110.100.140.11

0.110.130.130.1 L0.13

0.130.130.120.130.13

0.130.130.130.130.12

0.130.130.100.070.04

0.120.13

V1CP70

2pimi

SO76797976

7679775570

7374727372

7368727165

7778706123

7974

CrICP70

1ppm

9388847887

9088887989

89114898992

9393918893

8779707729

9190

MilICP70

2ppm

7351040868639602

552570952525765

6789)2804929992

953729907967933

787999818'37195

734815

Fe1CP70

0.01ft

4884,334.444.244.74

4.744.794.132.824.08

4.214.354.284.344.41

4.344.024.284.334.11

4.384.433.873.761.22

4.804.35

CoICP70

1ppm

2223222020

1820231319

2224232323

2119212221

212318141

2122

1 w-C*-o-s

70t r

COo

ciss

TJ

px*O5-b.

en.b.enro

Member of the SGS Group (Soctett G4n*ratecle Surveillance)

r0CD


Work Order: 056633 Date: 13/09/99 FINAL Pa|f t of 9

m-oi

COiCDCD

Element. Method. Oef.Lini. Units.

WWWOl WWW02 W WWW WWWOl WWW05

WWW06 WWWCI7 WWWG8 WWW09 W W W J O

WWW 11W W W J 2 WWW 13 WWW 11 WWW 15

WWW 16 WWW 17 WWW 18www iyWWW20

WWW'21 WWW22 WWW23 WWW'24 WWW'25

WWW2& \VW\V2? WWW2S WWW29 WWW30

NiICP70

1ppm

4815542752

5953514546

47424548

9

10454139

7

4240383141

4254113244

CuJCP70

0.5ppm

45.96.3

32.653.145.7

40.941.630.536.338,5

26.622.718.630.27.6

12.030.425.228.17.0

27.421.621.416.931.8

26.127.015.416.631.3

ZuICP70

0.5ppm

99.735.689.342.7

122

108111102177105

12686.8

10484.244.8

122135

93.979.021.9

75.880.967.548.6

137

95.962.140.652.890.0

AsICP70

3ppm

OO C 3Oooo0ooC3<$^: 3OC3

O<3O<'3

o117c3 C3C3

7

C 354

* 3 ^ j O

Si-ICP70

0.5ppm

24.012.832.293.347.8

'38.541.645.647.243.6

38.631.433.041.610.0

10.633.841.140.3

6.0

25.723.822.611.636.0

21 67.15.1

19.746.4

YJCP70

0.5ppm

10.51.8

15.415.815.2

12.013713.817.314.5

12.87.881

1221.0

2.06.0

11.214.3

1.5

4.53.7431.87.7

5.84.61.75.2

11.3

'LvICP70

0.5ppm

32.)2.9

36.717.653.7

46.749.019.719.438.0

25.417.919.627.7

1.9

3.67.8

11.312.82.7

16.817.917.03.7

15.3

20.96.44.1

10.314.6

Mo Ae Ccl SnJCP70 1CP70 1CP70 ICP70

1 0.2 I 10ppm ppm ppm ppm

<\ <Q.2 <^c 0.2*c c 0.2 <O 0.2 <<l CO.2 <

0 cO.2 << -^0.2 << 0.3 << CO. 2 << 0.3 <

< 0.2 << 0.3 <c 0.3 << 0.4 c< cO.2 c

s. c 0.2 ^c cO 2 << C0.2 << 0.4 CC C0.2 <

< -c0.2 <c CO. 2 << cO.2 <c cO.2 c< 0.3 c

< c 0.2 <c c 0.2 cc c 0.2c CO.2 <c 0.3 <

c 10c 10* 100000

oo< lo00< 10oo<10c 10ooc 10oooo00ooooooooooclOclO00

00clOooclOoo

Sb1CP70

5ppm

O^ c 5^^

c5c 5^<5<5

<5<5<5<5C5

c5<5<5<5-t 5

c 5C 5^c5c5

^C5c5<5<5

Ba1CP70

tppm

14334

176183181

174181161173160

17512613918450

38172165150

16

13112412147

129

10520IS72

152

i\j1 T t71'' Ci

ICP70 -o0.5

ppm

27.9 g4.7 ^

10 6 ETi 'j |~r^42.5 m42.6 g

35 f] OJJ ' U 5n39.2 238.2 Lo47.940.6

35.422.623.334.7 ^

3.2 g

4.7 g19.134.9 -^42.9 53.3 S

en17 R S 1 ( .0 ~^15.3 S17.27.3

23.7

10 Sjy. a4.7 ^4.1 I

16.731.8 1,

Membw of the SGS Group (Socift* Gyrate de Surveillance)OteCD


Work Order: 056633 Date: 13/09/99 FINAL Page 5 ol 9

COmT3

CO

CO CO

Element. Method. Det.Litn. Units.

W \V\V3l WWW32 WWW33 WWW34 WWW35


WWW4! WWW42 WWW43 WWW44 WWW45

WWW46 WWW47 WWW48 VVWW49 WWW50

WVVW51 WWW52 WWW53 WWW54 WWW55

WVVW56 WWW57 \VVVW53 WWW59 WWW60

NiId'70

1ppm

4142122310

4540404145

4934443440

5246561745

5138444541

2922404549

C liICP70

0.5ppm

24.622.612.87.85.1

28.124.425.823.626.7

36813.925.015.135.0

32.531.136.124.522.7

32.923.224.720.216.2

10.910534.717.026.5

ZnICP70

0.5ppm

10089. C.50.343.726.5

in126101109

84.4

12978.3S7.565.6106

10399.1107

31.394.6

116136144124134

60.441.1

117S8.697.0

As1CP70

3ppm

OOOoo

oo0o0

oo<3ooo*-:3OOooooooooooo

SrICP70

0.5ppm

27.221.17.3

11.56.7

34.642.734.736.433.2

44.520.322.519.526.6

24.921.719.17.6

22.2

35.541.237.222.421.3

14.617.639.434.541.0

YICP70

0.5ppm

11.25.01.82.11.7

12.612.612.510.312.8

14.25.84.43.78.8

12.76.45.63.03.8

12.310.911.75.94.6

2.62.6

18.09.3

11.5

Zr1CP70

0.5ppm

18.021.15.94.02.0

10.113.823.513.920.4

11.410.723.411.016.9

23.928.420.0

2.921.6

16614.812.018.313.2

7.04.1

2'J.222.419.4

Mo AU Cd SnICP70 KT70 ICP70 1CP70

1 0.2 1 10ppm ppm ppm ppm

O 0.2 -Z OOO <(.}.2 < OO< 0.2 < OO< ^.0.2 < OO< -C0.2 < OO

,,<<<<

<<<<<

<<<<<

<<<<<

<<<.<<

0.2 < OO^.2 < OO CO 2 < < 10

0.2 < OO0.2 < <10

0.5 < <10< 0. 2 < < 1 0

0.4 < < 10 ^0.2 < <10<0.2 < OO

0.2 < < 100.2 < <10

<0 2 < < 100.2 < OO0.3 ^A OO

0.3 O OO^.2 0 OO C0.2 < <10

0.2 O OO0.3 O OO

f. 0.2 O OO*^02 O OO cO.2 0 00^.2 0 00

03 <l OO

Sb1CP70

5Ppm

-c 5^<5<5<5

,C5<5<5<5<5

<5<5<5<5<5

^<5<5<5<5

^<5<5<5<5

^<5<5^'5<5

Ba1CP70

lppm

133115264924

169167146142162

18985

12484

144

16013011225

118

157156191123143

5958

165155182

La tjnICP70 -a

0.5 ^ppm

31.2 SIS. 4 r~4.2 ^6.3 pa5.7 |

42.6 o36.7 235.8 Lo29.536.8

48.117.217.714.0 -r,

34.9 g23.0 '20.4 J^10.7 Si15.2 g

en33.3 -33.6 fS37.119616.7

8.28.2

48.926.732.5

Memberoflhe SGS Group (Societe" Gfin&alede Sutvetenoe)

CZ) 05

XRALWork Order:


WWW6) WWW62 WWW63 WWW64 WWW65

VVWW66 WWW67 WWW63 WWW© WWW70

WWW'71 WWW'32 WWW'73 WWW74 WWW75

WWW76 WWW77 WWW73 WWW79 WWWSO

*DupWWWOl*DupWWW13*Dup WWW25*Dup WWW37*Dup WWW49

*Dup \VWW61*Dup \VWW73

!| XRAL Laboratories J A Division of SGS Canada Inc.

056633 Date: 13/09/99

NiICP70

1ppm

5448474349

5249413149

5253515251

5148505146

4944414118

5350

CuICP70

0.5ppm

50.023.126.622.125.8

35.332.120.317.232.7

36.635.032.634.931.2

33.931.534.332.226.1

36.119.130.625.225.4

51.233.3

ZnICP70

0.5ppm

10187.696.287.8

108

11392.278.772.6118

98.9120105113108

10996.8

105105

94.8

94.9102131127

31.9

99.1106

AsICP70

3ppm

7< 5•OO•C3

O•OO•C3O

0O*C30O

o•C3o<3oooooo

4o

FINAL

SrJCP70

0.5ppm

36.03S.536.724.538.8

42.033.729.123.244.5

48.845.242.043.639.1

42.936.342.840.237.6

25.833.835.544.0

7.8

35.443.0

YICP70

0.5ppm

12.S12.912.96.7

13.8

16.513.110.76.3

12.9

13.813.813.414.513.8

15.013.815.115.713.7

10.98.17.6

13.03.1

12.613.7

ZrICP70

0.5ppm

40.922.620.221.031.3

25.735.916.29.3

35.7

40.136.334.034.635.1

35.335.238.033.127.1

31.019.515.713.02.6

40.134.2

MoICP70

1ppm

-CI< 1O0oooooo0o0o0

o< ]ooooooo0

oo

Ag1CP70

0.2ppm

•c 0.20.2

•c 0.20.2

•c0.2

0.2<Q 2

0.3•CO.2^.2

0.30.4

•cO.2•CO.2^.2

0.30.30.2

•CO.2•cO.2

0,30.20.5

*C0.2•CO.2

0.40.3

Pag* 0 of y

Cd1CP70

1ppm

•^<< iO0

Ooo0o<<<<<•c•c•c<•c

0oo<<l^<\

Si)ICP70

10ppm

00ou00OO00

0000000000

00OOOO•c 10OO

00< 10<l6OO< 10

00•c 10< 10< 1000

OO< 10

Sb1CP70

5ppm

<5^<5<5<5

<5^<5<5<5

<5^<5<5<5

<5^<5vc5<5

<5•c5<5<5<5

<5O

Ba1CP70

1ppm

182161no125194

22218813096

187

187199188196192

194176190190174

15014313117329

179191

LaICP70

0.5ppm

33.335.136.722.439.0

47,535.629.919.439.1

41.842.941.244.543.0

46.442.046.246.844.5

29.223.824.238.19.2

33.041.6

COm -o

COCD CO

1O

l\jCO-o^

x;t—t—CDO1SmCO

^x

p.Ca.

CO

enSen ro

® SBS Member of the SGS Group (Socle^ Generate de Surveillance)CD

XRAL XRAL LaboratoriesA Division of SGS Canada Inc.

Work Order: 056633


W W WO] WWW02 WVVW03 WVW04 WWW05

WWW06 WVVW07 WVVW08 WWW09 WWW 10

WWW 11 W W W12 WWW 13 WWW 14 WWW 15

WWW 16 WWW l? WWW 18 WWW 19 WWW20


WWW26WWW27 WWW28 WWW29 WWW30

Date: 13/09/99

wICP70

10ppm-C!0<10•^10<10<10

<10<1000Odoo<10oooo0000

0000000000

00000000oo0000000000

PbICP70

2ppm

136

189

14

1313121012

H1917156

49

10143

128

129

22

1445

1012

BiICP7I)

5PPI"

O^^^^

^^<5<5<5

<5^<5<5^

<5<5<5<5^

6<5<5<5^

<5<5

7<5^

FINAL Page 7 of D

COm -a

CO

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lm to

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Mentor otlhe SGS Group (SociS* Gindralede Surveillance} OS

o


Work Order: 056633 Dale: 13/09/99 FINAL Page 8 of l)

COm-oi

OJi

CDCD

o

o



WWW36 VVWW37 WWW38 WWW39 WWW40

WWW-11 WWW42 WWW-13 WWW44 WWW45


WWW5I WWW52 WWW53 WWW54 WWW55

WWW56 WWW57 WWW58 WWW59 WW60

\vICP70

LOPPI"

OO< 10< 10

00

^0< 10< 10< 10<10

00< 10OO< 10oo00< 10< 10< 10<10

00< 10< 100000

oooooo00oo

PbICP7I)

2ppi"1416

f, 22

1311131313

137

131018

1718181114

1613131919

58

121520

BiICP70

SPI""

5•f 1)6

?5

<5^< 5< 5<5

6O•x 5^<5

^<5<5c 5<5

0OOOO

5^

5^<5

ro —j-o

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05

en

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Member of Ihe SGS Group (SocKU G4r^rate de Surveillance)CDCD

XRAL XRAL LaboratoriesA Division of SGS Canada Inc.

Work Order: 056633 Date: 13/09/99

Element.Md hod.IM.Lim.Units.

W\W'.'(ilVV\V\V6'2WWW63ww\v (HWWW65

WWW66WWW 6?WWW (SWWW'69WWWlO

WWW7IW\VW72WWW?}WWW74W\VW?5

WWVViiWWW?'w w isWWW?'WWW0

*Dup VW\V01 WpWWB

*Dup v\VW37 *Dup tWW-19

,Dii ,-\vW61*Dnn"^WW73

W1CP70

toppm

<IO< 10< 10<1000

00oo< 10< 10<10

oo< 10oo00oo00< 10oo00oooo00oooo00

0000

PbICP70

2ppm

1717M1613

1515177

12

13151316M

U13151913

17 17 1811 II

19II

Bi1CP70

5ppm

,;5

Ot S^0

^oo^4:5^^<50^

<5<5<5O0

^

<5

<5< l}

FINAL f f ge 9 of

enm-oi

to iCOCO

go

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4^

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en

en

Member of (he SOS Group (Sod^i Generate de Surveilanw) O

O

APPENDIX 2Rock Sample Descriptions

Sample #

61501

61502

61503

Type

grab

grab

grab

61504

61505

61506

61507

61508

61509

61510

61511

61512

61513

grab

grab

grab

chip 1.5m.

grab

grab

grab

grab

grab

grab

Description

Rhyolite flow - up to l % fine-grained dissemin ated sulphides and trace amounts of euhedral fine-grained pyrite.

Fine-grained dacite lava with moderate epidote and carbonate alteration and l 07o medium- grained sulphides.

Rhyolite flow breccia, highly fractured with up 5 "/o sulphides and trace chalcopyrite in the fractures.

Assay Results

6 ppb Au

3 ppb Au

6 ppb Au 1.8 ppm Ag 189ppmCu 68 ppm Zn

8 ppb Au 1.5 ppm Ag

5 ppb Au

Rliyolite/dacite fine-grained lava with a 10 cm. shear/fracture zone containing up to 5 IM) sulphides.

Fine-grained rhyolite lava with minor shale, con taining up to l "/o pyrite and trace amounts of chalcopyrite.

Fine-grained dacite lava with a l meter wide shear 5 ppb Au containing up to 5 "/o disseminated sulphides. l .7 ppm Ag

Fine-grained dacite lava with a 2 meter wide shear 4 ppb Au and up to l "/o sulphides.

Fine-grained dacite lava with 2 small parallel trend- 5 ppb Au ing shears containing weak hematite alteration, 5 to 1.6 ppm Ag 8 07o sulphides and trace amounts of magnetite.

Shale/siltstone, slightly sheared with 5 to 10 "/o dis- 4 ppb Au seminated sulphides and magnetite. l .9 ppm Ag

Fine-grained dacite lava, sheared and fractured 5 ppb Au with 2 to 5 *Mi pyrite in the shear and fracture planes, l .9 ppm Ag

Rhyolite flow breccia with lto2Vo fine to medium- 9 ppb Au grained disseminated pyrite.

Rhyolite pillow lava with 2 07o carbonate in the mar- 6 ppb Au gins, trace disseminated sulphides.

Fine-grained dacite lava with upto 1 0A disseminated 6 ppb Au pyrite.

Ontario Ministry ofNorthern Developmentand Mines

Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.0.1990

Transaction Number (office use)

6UOQ10 0037kAssessment Files Research Imaging

ubsection 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, sesment work and correspond with the mining land holder. Questions about this -them Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury,

32D12SW2022 2.20610 LAMPLUGH 900

Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary) 2 O 6A/e f t- tt e/y/t i k set! Client Number

Address Telephone Number

Fax Number

Name Client Number

Address Telephone Number

Fax Number

2. Type of work performed: Check (S) and report on only ONE of the following groups for this declaration.Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

Physical: drilling stripping, trenching and associated assays

Rehabilitation

WorkType L Office UseCommodityTotal S Value of Work Claimed f/ 9. ?C/

Dates Work From Performed Day

1 6 9| Month | Y

Global Positioning System Data (if available)

NTS Reference

Mining Division aM or G-Plan Numberc, . Resident Geologist

District t d.*

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Pereon or companies who prepared the technical report (Attach a list if necessary)Telephone Number

5? nAddress

Name h* Telephone NumberrAddress #.0

— t? S OFax NumBer

Name Telephone Number

Address Fax Number

4. Certificationi, G-fft

Recorded Hojdej^r Agent ' f L- o hereby certify that l have personal knowledge of the facts set forth in

(Print Name)this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion ajjd, to the best of my knowledge, the annexed repSignature itfjecorded Holderjr Agent

elephone NumberAgent's Address

LARDER LAKE MINING DIVISION

PROVINCIAL RECORDING OFFICE - SUDBURY

RECEIVED

OCT O k 2000 GEOSCIfNCC ASSESSMENT OfFICE

5. Wor't to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form.

Utow.Mining Claim Number. Or if work was done on other eligible mining land, show in this

column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

TB 7827

1234567

1234568

HfoSTt\^1-$-1^o

Column Totals

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

/rp

-z- 3

Value of work performed on this claim or other mining land.

126,825

0

S 8,892

•f 3 7. 4^4 •3*-j7*7' 1 ,2*r-2.

m- i Sol

Value of work applied to this claim.

N/A

524,000

S 4,000-j ——————————

7 30} oo l^ \*L. } 3CO

J

^^^o(

Value of work' assigned to other mining claims.

S24,000

0

0

^M r#e

.1-2-^6*

Sank. ValueW .work to be distributed at a future date

S2,825

0

S4.892

0

o

D

l, , do hereby certify that the above work credits are eligible under(Print Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim

where the work was done.Signature ©(Recorded Holder^ AgentAutho Date Oe±.*L i- o o

6. Instruction for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check K) in the boxes below to show how you wish to prioritize the deletion of credits:

ff 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.D 2. Credits are to be cut back starting with the claims listed last, working backwards; orD 3. Credits are to be cut back equally over all claims listed in this declaration; orD 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use Only____________________Received Stamp

0241 (03/97)

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

ECEIVED J

GEOSCiEME ASSESSMENT _____ OFFICE

Ontario Ministry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office use)

CO C f,ft". C CPersonal information collected on this form is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Art, this information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5. 8 .206 1.0

Work TypeUnits of work

Depending on the type of work, list the number of hours/day worked, metres of drilling, kilometres of grid line, number of samples, etc.

Cost Per Unit of work

Total Cost

2-4 f 3

gf^r to ,7A 2 /Z.

f/f-o/cl^

l 1! It*.

LJj f ^ ^*^y 1 ^00 O 0

Associated Coste (e.g. supplies, mobilization and demobilization).

^ ^ Z,OQ.OO1 V

ruJt/P/ijjriAJz t S f

Transportation Coste

-TWO /Pt

Food and Lodging Coste

f

Total Value of Assessment Work

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 1000Xo of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 500Xo of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 ' Total S value of worked claimed.

Mote:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

hereby certify, that the amounts shown are as accurate as may reasonably(please print full name)

)e determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying

declaration of Work form as ^—^_____ ^*-t l ———— i-'^^-x' ( D^r *—-t*r ^* f\*^———

recorded tiotber^Jent. or state company position with signing authority)l am authorized to make this certification.

212(03/97)LARDER LAKE

MINING DIVISION

OCT 2 RECEIVEDOCT -\ :::3

GEOSCIENCE ASSESSMENT _____OFFICE

Ministry ofNorthern Developmentand Mines

December 7, 2000

GORDON NEIL HENRIKSEN 850 ROUTE DES PIONNIERS BELLECOMBE, QUEBEC JOZ-1KO

Ministers du DeVeloppement du Nord et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (888) 415-9845 Fax: (877)670-1555

Dear Sir or Madam:

Subject: Transaction Number(s):

Submission Number: 2.20610

StatusW0080.00376 Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact JIM MCAULEY by e-mail at [email protected] or by telephone at (705) 670-5880.

Yours sincerely,

ORIGINAL SIGNED BYLucille JeromeActing Supervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 15494

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.20610

Date Correspondence Sent: December 07, 2000 AssessorJIM MCAULEY

Transaction First ClaimNumber Number Township(s) l Area(s) Status Approval Date

W0080.00376 1140876 LAMPLUGH Approval December 06,2000

Section:9 Prospecting PROSP 13 Geochemical GCHEM 12 Geological G EOL 14 Geophysical MAG 14 Geophysical VLF

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

Correspondence to: Recorded Holder(s) and/or Agent(s):Resident Geologist GORDON NEIL HENRIKSEN Kirkland Lake, ON BELLECOMBE, QUEBEC

Assessment Files Library Sudbury, ON

Page: 1Correspondence ID: 15494

R E F E R E N CESAREAS WITHDRAWN FHOM DISPOSITION

M.R.O. - MINING HKiHTSONL,Y

S. R-O. -SURFACE RIGHTS ONLYM.+ S. - MINING AND SURFACE RIGHTS

*, Otto (H^^Mfci f H*

(y st 1 30/117/71

SEC .7,' f!

fiffo

5HO 117 TM

NOTES

Or fOUKTUT

THIS TOWMHIFVAHEA F*LLS WITHIN THE * BIT l pi MAMAMMCKT

Jlia AND HAT BE SUBJECT TD

THC MMR OMIT POftltTEM TO* THI* AHA tAH |f

CONTACTED AT R O 10* IB*

S WAST 1*4 -ONT4ITIO

pent - IT*W9-MS-SS2*

32D12SW2022 2.20610 LAMPLUGH 200

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULP CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MIMES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HER EON,

G 1637 IROQUOIS POINT

O

o z < tr

1222001

1221895

1225237 l-----J t1229164

1229163 1229162

HARKER TOWNSHIP

CIRCULATED MARCH 23, 1993 CM

LEGENDHIGHWAY AND fiOuTF No OTHER ROADS TRAILS SURVEYED LIMES:

TOWNSHIPS. BASE LINES, E TC.LOTS. MINING CLAIMS. PARCELS, ETC

UN&LTHVEYED LINES:LOT LJNESPARCEL BOUNDARYMINING CLAIMS ETC

RAILWAY AND RIGHT OF UTILITY LINESNOW PERENNIAL 5THEAMFLOODING OR FLOOD IMG BIGHTSSUBDIVISION OR COMPOSITE PLANRESERVATIONSORIGINAL 5HOHEUNEMARSH OR MUSK ECMINESTflAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENTPATENT, SURF ACE* MINING RIGHTS.

" , SURFACE H*GHT5 ONLY—— 11 . MINING RIGHTSONLY ...——

LEAK, SURFACE It WINING RIGHTS... " , SURFACE RIGHTS ONLY—™- " . MINING HIOMTS ONLY.™——

OF OCCUPATION ...—..._.

SYMBOL

RESERVATION ™. CANCELLED -.SAND it GRAVEL ,

— Q .-. T--. OC

SCALE: 1 INCH-40CHAINS

FEBT41)00

IT KM) 12 KM i

TOWNSHIP

LAMPLUGHM.H.R. ADMINISTRATIVE DISTRICT

KIRKLAND LAKEMIMING DIVISION

LARDER LAKELAND TITLES/ REGISTRY DIVISION

COCHRANE

Ministry ofNaturalResources

Ministry OfNorthern Developmentand Mines

Ontario

on*MAY 1990 G ^^/^o -5662

ARCHIVED MAR, 7/97

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R. CAMPBELL S G. HENRIKSEN w*Q(

WISHING WELL PROPER!

GEOCHEMICAL SAMPLING

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SOIL lAo HORIZON J/STREAM SEDIMENT SAMPLE LOCATION SAMPLE NO.

w JVut ppb) 1 Aa l ppm) 1 A^( ppm) a w A iY PkCpfni Z. IpjWculppmJ ANAU

Q ANOMALOUS GEOCHEMICAu>l4(c obi 1 Ao*0.3lDDm)l As > 3loDm)Pb > 2O (ppm)' Zn > 1 25lppm) >Cu ( ppm )

YTICAL RESULTS AL SAMPLE LOCATION

ANOMALOUS GEOCHEMICAL ANALYTICAL RESULT

LAMPLUGH TWR CG-3662) ONT.DATE: DEC, |999 NTS'. 32 D/12

SCALE: 1=2,500 MAP NO: GC- l

JON.•vj

LEGEND

EQUIPMENT USED - GEM SYSTEMS- GSM 8 PROTON PRECESSION MAGNETOMETER READINGS ARE 57,000 gammas PLUSPLOTTED VALUES, CORRECTED FOR DIURNAL VARIATIONSBASE STATIONMAGNETIC LOWCONTOUR INTERVAL - 100 gammas

m IQO 50 50 100 m

Scale: 1:2,500

R.CAMPBELL a G. HENRIKSEN


TOTAL FIELD MAGNETIC SURVEY

LAMPLUGH TWP (G-3662) ONT.DATE: DEC,1999

SCALE: f. 2.5OO

NTS 32 D /I2

MAP NO:

1999 WORK AREA

\U-L2. ' J— _

f 1225710

LAMPLUGH TWP. (G-3662)SCALE l "- I/a mi

lltO 153

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CLAIM MAP

32D12SW2D22 2.20610 LAMPLUGH 220

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R.CAMPBELL a G. HENRIKSEN


VLF ELECTROMAGNETIC SURVEY

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SCALE; i: 2,500

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R. CAMPBELL S G. HENRI K SEN


PROSPECTINGa

GEOLOGYLAMPLUGH. TWP (G-3662) ONT.

DATE; DEC, 1999

SCALE; i; 2,500

NTS- 32 D X12

MAP NO: PG' l

4^/1/1^

LEGEND

4) MAFIC INTRUSIVE ROCKS

a FINE-GRAINED GABBROb MEDIUM- GRAINED GABBRO

c FINE-GRAINED DIORITE

3) FELSIC METAVOLCANIC ROCKSa 'FINE- GRAINED MASSIVE RHYOLITIC LAVA

b FELDSPAR PORPHYRITIC RHYOLITE

c RHOLITE FLOW BRECCIA d RHOLITE PILLOWED LAVA

e FINE-GRAINED MASSIVE DACITE LAVA t DACITE TUFF

g AMYGDALOIDAL DACITEh DACITE TUFF

i FELDSPAR PORPHYRITIC DACITE

j INTERFLOW SHALE S SILTSTONEk CHERTY TUFF, BRECCIA

2) INTERMEDIATE METAVOLCANIC ROCKS

o FINE-GRAINED MASSIVE ANDESITE LAVA

b MEDIUM-GRAINED ANDESITIC LAVAc ANDESITIC PILLOWED LAVA

l ) MAFIC METAVOLCANIC ROCKS

a FINE-GRAINED MASSIVE BASALTIC LAVA

b MEDIUM-GRAINED MASSIVE BASALTIC LAVAc BASALTIC PILLOWED LAVA

SYMBOLS'.'.l.'-1 OUTCROP

V BOULDERS" ~~ ~ CONTACT

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FRACTURE, WITH DIPDIRECTION ft PLUNGE OF PILLOWS

® (Q) ROCK SAMPLE LOCATION WITH NO. a AU RESULT tppb) 61501 • WW-OI SOIL/STREAM SEDIMENT SAMPLE LOCATION WITH NO.

NOTE: See map GC-1 for assays

CABIN

CLAIM LINECLAIM POST

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R.c JUNE27 R. CAMPBELL'S PROSPECTING TRAVERSE WITH DATEG. HENRIKSEN'S PROSPECTING TRAVERSE WITH DATE

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lamplugh 2.206 10 - search geologyontario · summary of previous work ... have been collected by...

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