apollo development inc. assessment report

RCTIOPI:

APOLLO DEVELOPMENT INC.

Assessment Report

on the

Y CLAIM GROUP

Greenwood Mining Division

December 28, 1990 Vancouver, B.C.

NTS 82E/6E

Sookochoff Consultants Inc. Laurence Sookochoff, P.Eng.

TABLE OF CONTENTS

Page

SUMMARY .............................................. 1 INTRODUCTION ........................................... 2 PROPERTY ............................................... 3 LOCATION ............................................... 3 ACCESS ................................................. 3 HISTORY ................................................ 4 GEOLOGY ................................................ 5 STRUCTURE ............................................. 6 REGIONAL MINERALIZATION ............................... 6 PROPERTY MINERALIZATION ............................... 7 1990 EXPLORATION PROGRAM .............................. 9

Base Map .......................................... 9 Geochemical Survey ................................ 9 VLF-EM Survey ..................................... 11

CONCLUSIONS ............................................ 11 RECOMMENDED EXPLORATION PROGRAM ....................... 12 CERTIFICATE

REFERENCES ............................................ 14 STATEMENT OF COSTS .................................... 16

L . Sookochoff. P.Eng. ......................... 13

APPENDICES

I ASSAY CERTIFICATES I1 VLF-EM RAW DATA

Figure:

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

LIST OF ILLUSTRATIONS

Location Map Claim Map Regional Geology Local Geology compilation Map Geochem Survey Results: Cu Geochem Survey Results: Pb Geochem Survey Results: Zn Geochem Survey Results: A g Geochem Survey Results: As Geochem Survey Results: Cd VLF-EM Survey Results

GEOCHEMICAL and GEOPHYSICAL

ASSESSMENT REPORT

on the

Y CLAIM GROUP

Greenwood Mining Division

SUMMARY

The Y Claim Group is located within four kilometers of the Highland Bell Beaverdell mining operation from which silver production has been continuous since 1913. The productive silver veins of the Beaverdell camp occupy shear zones within altered granodiorite or sodic granite. Native silver, as one of the minerals associated with the veins, is found throughout a vertical range of at least t t l O O O feet."

At Carmi, six kilometers north of Beaverdell, the mineralization is of gold with very little silver values. According to Reineke (1915), the Carmi ores were formed under the same geological and structural conditions as those on Wallace Mountain where the deeper parts of the shear zones carry ores which resemble those at Carmi.

On the Y Claim Group, the initial interest was aroused by impressive assay results obtained from samples taken in 1975 from an open cut of the WYE 8 claim by Eric R. Smith, P.Eng. in 1975. The assay returned 5.25 - 5.83 oz/ton in gold and 27.9 - 29.1 oz/ton in silver across "12 inches" of quartz vein.

In the October 1990 exploration program completed for Apollo Development Inc., the same opencut - Trench T1 - was mapped in detail and systematically sampled resulting in additional significance to the type of mineralization. It was determined that gold mineralization in the trench occurs not only restricted to the fissure filled quartz and sulphide structures (2.6 oz Au/ton across 0.9 meters), but also in the altered host rock ( 0 . 8 2 oz Au/ton) and unaltered host rock (0.08 oz Au/ton).

In addition, the exploration program resulted in the delineation of five correlative anomalous areas - Zones A to E - for future exploration. Zone B, with the significant gold values of Trench T1 is correlative to a limited degree to soil geochem and low magnetic values. The most significant aspect of Zone B was the proximal association with anomalous cadmium values in the soil.

Zone A, 400 meters south of Zone B, includes exploratory workings which reveal a lower degree of mineralization than in Zone B. Lower order anomalous cadmium values correlate directly with the workings. The zone is indicated to plunge to the west - northwest.

Zones C and D, 1500 meters distant to the south, include old workings exploring mineral zones and consist of widespread multielement anomalous soil geochem values with localized anomalous cadmium values. The anomalous cadmium values occur within 50 meters of the workings

A significant anomalous cadmium soil geochem at the southeastern corner of the survey area is open to the southeast and occurs over two grid lines with values of up to 4.6 times background. Other localized cadmium anomalies are scattered over the grid area.

INTRODUCTION

In September 1990, Sookochoff Consultants Inc. was commissioned by Fred Mackenzie, a director of Apollo Developments Inc. to perform an exploration program on the Y Claim Group. The purpose of the program was to determine the potential of the property for the containment of economic gold and/or silver zones as located at the Highland Bell mine on Wallace Mountain near Beaverdell or at Carmi six kilometers north of Beaverdell.

The exploration program was essentially the recommendations as set out by H.Kim, P.Geol.,F.G.A.C., in a 1981 report on the property. The work was carried out under the direction of H. Kim, P.Geol.,F.G.A.C., and L. Sookochoff, P.Eng., and consisted of geochemical, geophysical, geological and related surveys and was completed during September and October, 1990.

Scale 1:10.000.000

100 0 100 200 300 4OOKm 7 - a

LOCATION

APOLLO DEVELOPMENT INC. S O O K O C H n F F CONSULTANTS INC.

H K I M , P Geol , F G A C L SOOKOCHOFF P Eng

Y CLAIMS GREENWOOD, M.D.

I LOCATION MAP

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Although portions of the present grid area were previously covered by geochemical and magnetic surveys, ,only one former grid station was located. As a result, a new grid was completed and the surveys repeated in part in order to establish definitive anomalous areas for the future exploration of the property.

PROPERTY

The property is comprised of eight two post located claims included within two contiguous 2 0 unit grid located claim blocks with an overstaking of an approximate four contiguous two claim post area. The effective area of the Y Claim Group is 920 hectares. Particulars of the claim group are as follows :

Claim units Record Number Expirv Date*

WYE 1 - a 4465 - 4472 December 09, 1992 Y # l 20 6081 September 22 , 1993 Y # 2 2 0 6080 September 20 , 1993

* Upon the approval of two years assessment work applied November 16, 1990

The claims are registered in the name of Apollo Development Inc.

scope of this report Any legal aspects regarding the claim group is beyond the

LO CAT1 ON (49 24'N, 119 06'W)

The property is located 290 kilometers east of Vancouver, British Columbia and within three kilometers south of Beaverdell. The claims cover the southern portion of Cranberry Ridge between the Westkettle River to the east and Tuzo Creek to the west which also crosses the claims in the southwest.

ACCESS

The property is readily accessible west from Beaverdell, across the Kettle River, southward along an abandoned railroad grade, past the Highland Bell Mine concentrator and to the northeastern corner of the Property.

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/-

1 2 3 4 Km

Geo-Comp Systems

Scale I :50.000 CLAIM MAP

DATE: OCT.'90 I N.T.S. 82€/6 I FIGURE 2 SOOKOCHOFF CONSULTANTS INC.

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In addition, the Tuzo Creek forestry road, branching off to the west from Highway 3 3 , 6 . 4 kilometers south of Beaverdell, provides all weather access to the western and southwestern portions. Numerous dry weather logging roads provide access to, or near to, most of the major mineral zones.

HISTORY

In the Beaverdell area, prospecting and exploration dates back to the late 1890's. The Highland Bell Mine on the west slopes of Wallace Mountain has been continuously active since 1913 with intermittent production between 1900 and 1913. The B.C. Department of Mines report, Geology in B.C., 1975, reports that the Beaverdell Mine area produced about 32 million ounces of silver, 2 4 million pounds of lead, 28 million pounds of zinc, with minor production of gold, cadmium and copper.

On ground covered by the Wye claim group, four locations were explored for precious metal and base metal deposits by six adits with winzes and three open cuts prior to 1970. There is no information available on the analytical results of this exploration.

In 1975 a localized magnetic and a geological survey was completed for Argentia Mines Ltd. over a trenched area north of Logan Creek (present Wye 8 mineral claim) on the Doorn Group of mineral claims, which are now part of the Y Claim Group. Reported results (Smith 1975) include a channel sample of a "12 inch" quartz vein assaying 5.83 ozs/Au and with "one sample across 100 feet returning 0.043 ozs/ton Gold and 0.05 ozs/ton Silver."

The magnetic highs appear to reflect the andesite dykes and in one area the mineralized quartz veins are related to andesite dykes where "both the veins and the dykes have a NW-SE strike, and appear to parallel the magnetic zone immediately to the south and to the north." Smith concludes that several other targets exist within the grid area which should be examined for mineral potential.

In 1980 and 1981 Mohogany Mining Company Ltd. completed exploration work on the Dell claim group (twenty claims) and covered the ground presently designated as the Wye 1-8 claims. The reported results (Cruz 1980; Kim 1981) revealed geophysical and geochemical anomalies in the north and the south of Logan Creek.

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The anomalies consisted of four electro-magnetic anomalous zones, generally running east-west and anomalous coincident silver, lead and zinc soil geochemical values with erratically high geochem values up to 41,000 ppm in Pb, 2,290 ppm in Zn, 5.8 ppm in Ag and 127 ppm Cu. Cruz also states that two vein systems may occur; one east-west system and second north-south system dipping from 4 0 to vertical.

In 1987 six trenches within granodiorite were completed on the Wye 7 mineral claim. Results (Hainsworth 1987) of the trenching revealed minor local alteration in addition to weak silver values from the 3 3 trench samples.

GEOLOGY

The Y Claim Group is embraced within a large body of Cretaceous Nelson plutonic intrusives consisting of granodiorite, quartz diorite, diorite, quartz monzonite, monzonite and syenite.

The intrusive in the Beaverdell area which is referred to as the West Kettle Batholith is composed of an even grained granitic rock having an average grain size of about 1.5 millimetres. It has a speckled grey appearance due to approximately equal amounts of dark and light colored grains. Some of the feldspar has a pinkish tint.

The Beaverdell Stock intruding the West Kettle batholith, and occurring at the Beaverdell Mine, is a light colored pinkish rock resembling granite, having a grain size of about five millimeters, is highly chloritized and characterized by large pink orthoclase phenocrysts. The stock approximates the age of the bulk of the mineralization (50 My) and is considered to be genetically related to it.

The Y Claim Group is mainly underlain by granodiorite and quartz diorite, which are continuous with the country rock of the active Beaverdell Mine. The intrusive rocks are in turn intruded by quartz monzonite and monzonite in the central west and south part of the map area. Some outcrops of the later intrusives may be called syenodiorite, syenite or even porphyritic granite on visual inspection. All these various intrusive rocks may be associated with the Nelson pluton of Cretaceous period as variable phases.

It is also possible that these intrusives are a part of Tertiary porphyritic granite. On the western and southern boundary of the line grid geologic map, fine-grained diorite and aplitic dykes intrude the granodioritic country rocks. A fine-grained diorite appears to be a pulaskite-looking rock commonly associated with Tertiary volcanics. Aplitic dykes may be related to a granodiorite intrusion.

L E G E N D

61 ANDESITE. TRaCNYTE. MlNOR BASaLT

KETTLE RIVER FORMaTION

141 VaLHALLA PLUmNlC ROEIS

131 NELSON PLUTONlC RWLS

121 AN4RCHIST GROUP

MONASnEE GROUP

X MINERAL OCCURRENCES

I

SOOKOCHOFF CONSULTANTS INC. ~

iPOLL0 DEVELOPMENT INC

REGIONAL GEOLOGY ’ N.T.S. 82E/ 5 10 I5 I U . 0

L J

XALE 1:250.000

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The mineralized quartz veins or shears are hosted by granodiorite or quartz diorite with some remnant masses of pre-mineral Anarchist volcanics of Permian or Triassic period. All important showings and geochemical anomalies are localized in the granodiorite or quartz diorite. The later phase of the intrusives viz, monzonite, quartz monzonite, porphyritic quartz syenite, etc. appear not to carry significant sulphide mineralization.

STRUCTURE

The most striking feature on Wallace Mountain is the five sets of faults noted by previous workers. Some are pre-mineralization in age, some are mineralized and some occurred later than the mineralization. Of the five sets, two are most important in their effect on the mineralization. High-angle, northerly striking, steeply eastward dipping, normal faults cut Wallace Mountain into several large blocks. These faults are all post mineralization and thus displace the veins.

The other important fault-set strikes northeasterly and dips moderately to the northwest. This set comprises numerous normal faults with displacements ranging from a few centimetres to several meters. In several places these faults are spaced less than one meter apart slicing the veins into numerous short sections.

REGIONAL MINERALIZATION

The productive veins of the Beaverdell camp are up to "50 feet" wide and occur in zones of altered granodiorite or sodic granite of the West Kettle batholith. The altered rock adjacent to the veins is soft and appears speckled with small purplish blotches with abundant development of serecite and clay minerals, chlorite, calcite, epidote and hematite. The ore is in simple veins, composite branching veins and stringer lodes.

The veins host medium grained pyrite, sphalerite and galena with some arsenopyrite and some chalcopyrite. Commonly, the veins have a banded structure produced by a rude parallelism of sulphide stringers. The parts of the vein that constitute ore-shoots contain in addition to the common sulphides, visible amounts of silver bearing minerals such as tetrahedrite, pyrargyrite (ruby silver), polybasite, argentite and native silver. The native silver occurs in and is associated with the vein and other minerals and is found throughout a vertical range of at least "1,000 feet".

i I / \ i

ROPERTY OUTLINE'

\ I I

WHETRES SCALE -1 : 20,000 ~. 0 M

I t

DATE: OCT 1990 FIG NQ. 4

- 49 24 '

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At Carmi, six kilometers north of Beaverdell, the ores carry gold with a very little silver. Reinecke (1915) states that:

"the ores at Carmi were formed under the same geological and structural conditions as those on Wallace Mountain, it is believed that the Carmi ores represent the deeper parts of the orebodies whose upper parts have been eroded away: or in other words, the deeper parts of the shear zones on Wallace Mountain carry ores which resemble those at Carmi. ..The mine at Carmi is a low grade property, but the length of outcrop of the shear zone in which its ores lie indicate that the shear zone may continue to a depth of 1,000 feet or more."

PROPERTY MINERALIZATION

On the Y Claim Group, four locations were previously explored for mineral occurrences by at least six short adits and three open cuts. In the 1990 program, it was not possible to examine two adits and a winze of this earlier exploration program due to caving or flooding.

Analogous to the pattern and structure of the productive veins in the Beaverdell Mine area, mineralized quartz veins in shear zones on the property occupy two sets of fractures. One set striking generally east-west is represented in the trench north of Logan Creek. The other set strikes northeast and comprises the rustily weathered shears and quartz veins of the flooded winze in the southeast corner of the property.

All accessible showings examined on the property are summarized as follows:

Trench T1 The economic interest on the property was aroused by reported assays of 5.25 - 5.83 oz Au/ton and 27.9 - 29.1 o z Ag/ton across "12 inches" of quartz vein (Smith 1975). Sheared granodiorite and andesites host gold bearing quartz veins, veinlets and fracture filled sulphides (Sample Nos. T1-70 & T1-28). Significant gold mineralization occurs within bleached, jarocitized and limonitized zones along the contact. (Sample Nos. T1-14 & T1-18). The granodiorite and the andesite host rock also contain anomalous gold values (Sample Nos. T1-30 & T1-34) which increase with increased limonitic content along the fracture planes.

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Trench T2 and T 3 . Trench T2 exposes a weakly altered granodiorite with a 0.2

meter wide quartz vein from which a sample returned an assay of 0.1 oz Au/ton. A sample of a weakly bleached zone within the granodiorite returned 100 ppb Au. Trench T3 exposes granodiorite and andesite which are relatively unaltered. Samples of quartz vein material returned an assay of 130 ppb Au

Showings on L1 Two short adits expose narrow rusted shear zones hosting

quartz veinlets and massive sulphides with associated light argillic alteration. A sample from a 20 cm quartz vein returned 910 ppb Au.

Quartz veins on L1. There are a series of northwesterly trending quartz veins

to the west of the above noted two short adits. Widths of the quartz veins exposed in the trenches and adit are up to one meter, however show no visible sulphides. A 0.6 meter wide channel sample of the quartz vein in a short adit returned an assay of 360 ppb Au and 303 ppm Ba.

Iron oxidized rocks on L2. An impressive rustily weathered 10 meter wide zone in

granodiorite hosts 16 narrow quartz veins and veinlets. Samples taken across the 10 meter wide zone returned 12 ppb and 24 ppb Au.

Adit on L1200. A 150 meter long crosscut exposes over 18 fault-shear zones

with associated quartz veins attaining widths of up to 0 . 3 meters wide. Samples from the adit returned generally low gold values however one sample returned an assay of 250 ppb Au.

Winze on ~1100. A 0 . 8 meter wide sample from a zone between two mineralized

structures returned anomalous values in base metal values of 967 ppm Pb and 694 ppm Zn.

Winze on L400 - 1460 SW. A 0.6 meter wide highly oxidized structure with quartz

veinlets returned an insignificant gold value but the base metal and iron content would be anomalous being 692 ppm Cu., 418 ppm Zn., 112 ppm Ni. and 24.36% Fe.

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1990 EXPLORATION PROGRAM on the Y CLAIM GROUP

The 1990 exploration program on the Y Claim Group included the following:

1) Base map 2) Grid 3) Geochemical survey 4) VLF-EM survey

Base Map

A base map was prepared by Geo Comp Systems.

Geochemical Survey

A grid was set up to cover two areas of known bedrock mineralization. Initially two northeast-southwest baselines were established: one 1,400 meters long and a second paralleling the first 1,000 meters southwest and 1,400 meters long. The southeastern portion of the first baseline overlapped the northwestern portion of the second baseline by 400 meters in order to provide a control to the survey area.

Cross grid lines were fixed at 100 meters on the baseline with four lines common to the two baselines. Samples were taken at 4 0 meter stations along the grid lines and were taken from the llBll horizon of the brown forest soil at a depth of 12 to 18 centimetres. The soil was placed in wet-strength bags with the appropriate grid station marked thereon. Red flagging with the grid station was placed at the field station. A total of 595 samples were taken.

The samples were sent to Acme Analytical Laboratories Ltd. of Vancouver where a 30 element ICP test was completed with a portion of the samples analysed for gold. The ICP analysis involved the digestion of .500 grams of the soil sample with 3 ml 3-2-1 HCl-H20 at 95 deg. C for one hour and diluted to 10 ml with water.

The background, sub anomalous and anomalous values of six elements - arsenic, copper, silver, lead, cadmium and zinc - were determined utilizing a program developed for an IBM PC computer. The results were plotted on individual maps with a composite or compilation of results on a separate map.

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The statistical parameters are as follows:

Background Sub Anomalous Anomalous Arsenic 5 7 10 Cadmium 0.4 0.7 1.0 Copper 16 25 34 Lead 21 45 69 Silver 0.2 0.3 0.5 Zinc 112 188 263

All values are in ppm.

The results of the survey on each of the six elements is as follows:

Arsenic. The predominant portion of the arsenic anomalous values,

which range up to 39 ppm, are located in the southern part of the grid area. The localized anomalous trend is northwesterly, however the general trend is east-west. There is not a direct correlation to any of the two known mineralized zones in this area.

Cadmium. The maximum anomalous cadmium value, which occurs within

anomalous area B, is 7.9 ppm and is proximal to the trenches exposing the most significant mineral zone on the property. The anomalous and sub anomalous zone extends northwesterly for 150 meters and is open to the southeast.

An anomalous zone in area A extends west northwest for 300 meters and correlates directly with a trenched mineralized zone. Mineralized zones with workings in area C and D in the southern portion of the property are proximal to cadmium anomalous values. An anomalous zone south of area C contains values up to 2.6 ppm cadmium, covers an area of 200 by 100 meters and is open to the southeast.

Copper. The anomalous values are up to 152 ppm generally occur as

northwesterly to east-west trending anomalous zones. Specifically, the two highest values correlate with anomalous cadmium values: the open anomalous zone proximal to the main trenched zone at area B and a localized zone at Line 100 SE, 550 SW.

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Lead. Anomalous lead values range up to 1741 ppm from an

anomalous threshold of 69 ppm. This highest value occurs within an anomalous zone within area C, proximal to the mineralized zone. There is no anomalous value associated with the main zone at area C and only a single anomalous value associated with mineralized area A . Most of the anomalous values are in the southern sector of mineralized areas C and D.

Silver. The anomalous silver values are all one station scattered

values with only one area of significance. Low order anomalous silver values of up to 0.6 ppm occur across three grid lines correlating in part to anomalous copper, zinc and cadmium values in mineralized area A .

Zinc. The highest zinc value of 2,130 ppm does not correlate with

any mineralized area and occurs south of mineralized area C. The high value correlates with anomalous, arsenic, lead and cadmium values. There is also direct and indirect correlation with the other three mineralized areas.

VLF-EM Survey. Within the northern portion of the survey area the Fraser

Filtered survey results indicated localized discontinuous northwesterly trending zones. A general larger scale west-northwesterly trending anomalous zone incorporates the upper portion of mineralized zone A indicating a potential mineral controlling structure.

Similar anomalous zones occur in the south but to a lesser degree. Minor easterly structural trends are interpreted with a general north-northwesterly trend indicated. The survey was not completed over the Tuzo Creek mineral zones C and D and terminated adjacent to correlative zone E.

CONCLUSIONS

It is concluded that the Y Claim Group covers geologically favorable ground for the localization of potentially economic gold mineral zones. As a result of the 1990 exploration program, it was also indicated that known mineralized areas are or proximally associated with localized anomalous cadmium values in the soil. Cadmium thus appears as a favorable pathfinder element in the expression of gold mineralization. The anomalous cadmium values may be utilized in the location of near surface mineralized areas, whereas the sub anomalous or above background cadmium values may be indicative of deeper seated mineral zones.

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RECOMMENDED EXPLORATION PROGRAM

It is recommended that a two stage exploration program be completed on the Y Claim Group. Initially, additional IP surveys should be completed over Zone B to determine the configuration of the mineralized zone and the IP response to the west. Diamond drilling to test the results of the IP and the extent of mineralization to depth would follow. Utilizing the information obtained from the drilling of Zone B, Zone A would be explored accordingly.

Should the IP be effective in the detection of target areas for diamond drilling, IP surveys Would be completed over Zones C, D, & E and over the anomalous cadmium zone at 1270 SW 1400SE. All other anomalous, sub anomalous and above background cadmium zones should be examined for potential gold mineralization.

Contingent on the results of the initial stage of the recommended exploration program, a second stage of follow-up diamond drilling and preliminary exploration of the unexplored portions of the property would be initiated.

Respectfully submitted, SOOKOCHOFF CONSULTANTS INC.


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CERTIFICATE

I, Laurence Sookochoff, of the city of Vancouver, in the Province of British Columbia, do hereby certify:

That I am a Consulting Geologist with offices at Suite 603, The Standard Building, 510 West Hastings St., Vancouver, B.C., V6B 1L8.

I further certify that:

1. I am a graduate of the University of British Columbia

2. I have been practising my profession for the past

(1966) and hold a B.Sc. degree in Geology.

twenty-four years.

3. I am registered with the Association of Professional Engineers of British Columbia.

4. Information for the accompanying report was obtained from sources cited under References, from work performed on the property reported on herein since 1987 and including the work carried out on the Y claim group in 1990.

5. I have no direct, indirect nor contingent interest in the property described herein, or in the securities of APOLLO DEVELOPMENT INC., nor do I expect to receive any.

6 . I hereby grant my consent to the publishing of this report for the purpose of financing of APOLLO DEVELOPMENT INC. ,

Laurence Sookochoff, Consulting Geologist

P.Eng.


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REFERENCES

BABETT, C. and TOMASZEWSKI, G. (1980) - Personal

CHAPMAN, D. (1990) - Report on a Fracture Density Survey of the Y Claim Group.

CHRISTOPHER, P.A. (1975) - Highland Bell (Beaverdell) Mine in B.C. Dept. of Mines and Petroleum Resources Annual Report, "Geology in B.C."

CRUZ, E. (1980) - Report on the Geochemical Exploration of the Dell Mineral Claim Group for Mohogany Mining Company Ltd., Assessment Report #8504.

Communication at Beaverdell Mine.

G.S.C. MAP - 6-1957, Kettle River (East half) Similkameen, Kootenay and Osoyoos Districts.

HAINSWORTH, W.G. (1987) - Report on the Trenching Results over the WYE 1 to 8 Claim Group for Skyway Resources Ltd.

HARRIS, J.F. (1990) - Petrographic Report on Rock Samples from

HAINSWORTH, W. G. (1987) - Report on the Trenching Results Over the Eight Claim Group Wye 1 to 8 inl., for Skyway Resources Ltd.

the Beaverdell Area, Vancouver Petrographics Ltd.

KIDD, D.F. and PERRY, 0. (1957) - Beaverdell Camp, B.C., in Structural Geology of Canadian Ore Deposits, C.I.M. Congress Vol. 11, pp. 136 - 141.

KIM, H. (1981) - Geological and Geochemical Survey Dell - Kuz Claims for Mohogany Mining Company Ltd., Assessment Report #9557.

MEYERS, R.E. et a1 (1989) - Lode Gold - Silver Occurrences of the Okanagan Region, South - Central British Columbia, Ministry of Energy, Mines and Petroleum Resources, Open File 1989-5.

REINECKE, L. (1915) - Ore Deposits of the Beaverdell Map-Area, Geological Survey of Canada, Memoir 79.

SMITH, E.R. (1975) - Report on Geologic and Magnetic Surveys on the Doorn Group f o r Argentia Mines Ltd., Assessment Report #5441.

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REFERENCES (cont'd)

SOOKOCHOFF, L. and REYNOLDS, P. (1988) - Preliminary Exploration Report on the Shieba Claim Group for Andromeda Ventures Inc.

SOOKOCHOFF, L. (1988) - Geochemical Assessment Report on the Shieba Claim Group for Andromeda Ventures Inc.

SOOKOCHOFF, L. and KIM, H. (1988) - Summary Report and Recommendations on the Wye Claim Group for Skyway Resources Ltd.

STAPLES, A.B. and WARREN, H.V. (1946) - Minerals from the Highland Bell Silver Mine, British Columbia, Western Miner, May and June.

VERZOSA, R.S. and GOETTING, B. (1972) - Geology and History of the Highland Bell Mine, Beaverdell, B.C., C.I.M., Paper presented at fall meeting in Prince George.

Mines, B.C. Annual Report., 1949, pp. 138 - 148. WHITE, W.H. (1949) - The Beaverdell Silver Camp, Minister of

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APOLLO DEVELOPMENT INC. Y Claim Group

Statement of Costs

The field work on the Y claim group was carried out from September 15, 1 9 9 0 to November 9, 1 9 9 0 to the value of the following.

Grid, Geochemical and Geochemical Survey

Andrew Sostad: September 22, - October 6, 1 9 9 0

1 5 days @ $250.

1 4 days @ $275.

Don Hairsine: September 22, - October 5, 1 9 9 0

Pat Crook: September 15, - October 8, 1 9 9 0

24 days @ 300. Laurence Sookochoff, P. Eng.

Room & board 58 man days @ $75. Truck rental 20 days @ $55. plus gas Field supplies Assays Compilation & draughting Report & associated costs

5 days @ $500.

$ 3 , 7 5 0 . 0 0

3 , 8 5 0 . 0 0

7,200.00

2,500.00 3,364.00 1 ,228 .00 1 ,350 .00 5 ,187.00

675.00 2 ,896.00

$ 32 ,000.00

Appendix I

ASSAY CERTIFICATES

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17 .29 .111 7 26 .16 .039 10 23 .17 10

30 .21 14

3a .53 .082 20

27 .21 .026 11 29 .31 .031 12

' 26 .27 .028 16 ' M .28 .on 21

5 .24 246 6 .22 219 8 .24 202

10 .34 301 10 .31 526

6 .% 756 6 .25 292 7 .28 236

8 .24 439

20 .LO 2oL

2 1.29 .02 .16 6 1.23 .01 .16 4 1.31 . O l .12 2 2.76 .01 .12 4 2.96 .01 .W

7 2.18 .02 .20 2 1.60 .01 .12 5 1.a .01 .14 5 1.61 .01 .12 7 1.47 .02 .13

5 1.72 .02 .13 4 2.14 .01 .17 4 1.97 .01 .16 8 1.59 .02 .15 2 2.17 .01 .15

4 2.77 .02 .21 5 1.78 . O l .20 2 1.93 .02 .13 4 1.94 .02 .15 6 2.17 .02 .I0

6 1.96 . O l .14 5 1.67 .01 .17 5 1.87 .02 .19 7 1.64 .01 .20 2 1.76 .02 .13

5 2.50 .02 .14 3 2.78 .01 .25 3 1.36 .02 .13 3 1.23 .02 .10 3 1.79 .02 .14

4 .73 .02 .ll 4 1.29 .02 .10 5 .81 .02 .18 3 1.86 .a2 .20 5 2.59 .01 .16

1 2 1 1 1

3 1 3 3 1

2 3 1 1 1

2 3 2

12 5

8ookochoff Consultants Inc. PROJECT BEAVERDELL FILE # 90-5169 Page 3

1 1 1 1 1

1 1 1 1 1

1 1 1 1 1

1 1 1 1 1

1 1 1 2 1

1 2 1 1

24 10 14 28 12

12 18 8 9

23

7 10 6

22 19

18 6 8 6

25

10 9

10 14 13

3 7 8

10 8

7 7 6 6 9

6 7 5 4 5

5 6 7 4 7

8 10 6 8 5

6 7 7

ND ND NO ND YD

WD ND N D NO NO ND

ND ND NO NO

WD ND NO N D ND

NO ND NO NO ND

ND WD NO NO

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 3 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2

5 5 5 5 5

5 5 5 5 5

5 5 5 5 5

5 5 5 5 5

5 5 5 5 5

5 5 5 5

1 225 .4 3 47 .5 8 57 1.2

15 3.97 .2R 7 21 .42 .132 7 36 .56 .037 36

4 3 1 1 1

1 2 1 4 2

5

1 2 2

3 1 2 1 3

f f 3 1 1

i

a

9

11 118 21 353 53 169 38 198 77 228

69 356 22 200 27 197 30 146 59 149

L a m BBON LBO0 84ON Lam B O O N LBW 7 6 0 s LBO0 RON

5 2256 1.09 5 462 1.64

11 2134 3.38 12 2094 3.38 8 1306 2.69

24 .71 .02 .14 4 .19 1288 6 1.77 .03 .14 6 .26 M4

7 .61 T86 2 2.64 .02 .23 13 .55 1217 3 3.43 .02 .m 9 .43 534 2 2.66 4 2 .24

5 73 .9 5 49 .8

28 15

11 20

8 18 22

4 15 8 5

16

10 11 15 6

16

12 13 9

17 9

5 14 10 8

60 .46 .D99 58

4 n .? 7 51 .9 4 82 .4 7 MI .6 6 67 .9

... 6 2.01 .02 .24 5 2.42 .02 .30 4 1.86 .03 .24 5 1.93 .01 .31 2 2.44 .02 .19

7 1569 2.44 8 1399 2.81 5 1056 1.89 7 921 2.47

11 1026 3.68

3 411 1.26 7 1409 2.44 4 u6 l.M 4 2146 1.10 7 1203 2.49

6 2111 1.88 5 1013 2.00 6 630 2.29 4 &c5 1.68 8 2117 2.42

7 1627 2.31 6 577 2.43 5 418 2.11 8 2559 2.63 4 1046 1.99

9 .32 647 8 .so 797 8 .22 532 7 .30 609 8 .46 868

6 .15 377

LPOD 84ON LPOO B O O N

L p w 760N 4 1.00 .03 7 1.86 .01 3 1.49 7 .BO 3 1.89

4 1.44 .02 4 1.97 .02 2 2.05 .02 7 1.21 .02 3 1.92 .02

.02

.02 4 1.63 .02 2 2.67 .02 2 1.79 .02

4 1.00 .03 .10 7 1.86 .01 .29 3 1.49 .02 .ll 7 .BO .03 .19 3 1.89 .01 .30

4 1.44 .02 .ll 4 1.97 .02 .18 2 2.05 .02 .17 7 1.21 .02 .22 3 1.92 .02 .14

4 1.99 .02 .21 2 2.63 .02 .12 4 1.63 .02 .17 2 2.67 .02 .16 2 1.79 .02 .24

2 1.27 .03 .ll 4 1.92 .02 .16

4 1.39 .03 .14 2 1 . n .02 . i 4

57 .B? 182 ' .07 34 1.89 .06 .13 4i

23 182 34 176 21 191 18 321 19 78

.10 ~~. .29 .02 .ll .03 .19 .01 .30

.ll

.18

.17

.22

.14

.21

.12

.17

.16

.24

.03 .ll

.02 .16

.02 .14 4 1.39 .03 .14

57 .B? 182 ' .07 34 1.89 .06 .13 4i

9 .34 372 8 .24 311 6 .16 883 6 .45 389

6 .28 1051 8 .26 448 9 .30 390 7 .19 429 9 .36 573

L l o W 920SU L l o w 880N L l o w & O N L l w o B O O N L l o w 760%

46 277 33 142 53 130 14 241 35 174

58 181 .1 31 152 .2 27 97 .1

10 .33 531 .DB 12 .32 476 .10 8 .29 333 -06

4 1.99 2 2.63

4 36 .2 L l l W RON L11W BBON I 58 173 .f

229 s n .I 10 .40 709 .!I5 7 .24 351 .C5

5 M .3 4 51 1.3

1 39 1.6 2 73 1.5 5 73 1.0 2 95 .3

7 40 52 18.6

7 .17 392 .06 11 .33 m .M 7 .35 518 .06 8 .21 544 -06

2 1.27 4 1.92 2 1 . n

8 44 751 4 996 1.28 35 1741 564 10 3611 2.99 22 60 389 7 1619 2.13 12 69 271 6 4 1595 1.45

18 57 42 129 7'2 31 1054 3.97 19 (STU(O*RD CIAUU-s 15 22 __

SAMPLE# -

no Cu Pb Zn Ag N i Co Mn Fe AS U A U l h S r Cd Sb B i v C o P t a C r ug aa T i

L10 NU-240 WE L10 NU-280 WE L10 NU-320 WE L10 NU-360 YE L10 NU-400 YE

L10 NU-440 NE L10 NU-480 NE L 9 NU-00 L 9 NU-040 NE L 9 NU-080 WE

L 1 0 N U - 0 4 0 N E L l O N U - 0 8 0 N E L10NU-120NE L10NU-160NE L 1 0 N U - 2 0 0 N E

1 9 9 96 .1 6 6 1 0 0 7 1 . 7 4 4 5 NO 3 30 .3 2 2 29 .27 .093 7 9 .32 259 .05 2 1 . 4 9 .02 .12 1 7 6 71 .1 4 5 7 2 4 1 . 5 4 2 5 NO 2 25 .2 2 2 26 .25.054 4 7 .27 229 .04 2 1 . 0 3 .02 .12 1 10 3 67 .1 4 5 6 5 4 1 . 5 4 2 5 ND 2 33 .2 2 2 25 . 2 8 . 1 5 6 6 7 .26 273 .04 2 1 . 1 9 .02 .ll 1 7 7 49 .1 2 6 502 1.65 2 5 NO 3 27 .2 2 2 29 .26 .054 5 7 .34 140 .04 2 .m .02 . I 2 1 9 9 63 .1 4 6 5 2 7 1 . 6 1 4 5 ND 4 23 .2 2 2 27 .25 .074 7 8 .31 123 .04 2 1 . 0 1 .02 .10

1 10 13 122 .1 5 6 1 5 1 1 1 . 7 7 5 5 NO 2 37 .2 2 2 28 .39 .105 5 8 .40 305 .03 4 1 . 1 2 .02 .12 2 6 2 101 .1 3 6 1 8 6 0 1 . 5 9 2 5 ND 4 26 .2 2 2 24 . 2 5 . 0 6 2 6 7 .30 357 .03 4 1 . 0 2 .02 .10 1 7 7 57 .1 5 5 1 0 1 9 1 . 6 7 4 5 ND 2 24 .2 2 2 30 . 1 9 . 1 1 7 4 7 .29 203 .05 2 1 . 1 0 .02 .09 1 6 6 41 .1 3 5 6 5 7 1 . 6 1 2 5 ND 3 25 .2 2 2 31 . 2 5 . 0 7 2 7 7 .28 115 .05 2 .87 .02 .ll 1 10 9 47 .1 5 6 7 1 8 1 . 9 3 3 5 ND 4 22 .2 2 2 39 . 2 5 . 0 5 7 7 8 .37 114 .06 2 .94 .02 .14

1 10 6 62 .1 5 5 6 3 4 1 . 6 8 3 5 NO 2 2, .2 2 2 29 . 3 1 . 1 2 6 6 6 .33 127 .05 2 1 . 2 4 .02 .09 1 9 9 64 .1 5 6 7 2 8 1 . 8 0 4 5 ND 3 4 L . 2 2 2 31 . 3 2 . 1 5 3 7 8 .39 180 .06 5 1 . 3 4 .02 .14 1 7 5 54 .1 4 6 7 2 7 1 . 7 3 3 5 ND 3 21 .2 2 2 33 .21 .050 5 7 .35 139 .05 3 .91 .02 .12 1 10 13 60 .1 5 7 8 9 9 1 . 8 7 3 5 ND 5 26 .2 2 2 34 . 28 .052 11 8 .37 l b 3 .(M 2 1 . 1 0 .02 .17 1 9 6 77 .1 3 6 1 4 1 0 1 . 6 8 4 5 NO 2 36 .2 2 2 37 .41 .042 7 7 .33 242 .05 2 .89 .02 .15

L 9 WU-120 WE L9 NU-160 WE L 9 NU-200 HE C9 NU-280 WE L 9 NU-320 WE

1 7 2 90 .1 3 6 1 8 5 4 1 . 7 2 3 5 ND 4 24 .2 2 2 26 . 3 3 . 0 5 3 5 8 .31 282 .03 2 1 . 0 4 .02 .13 2 7 10 70 .1 3 7 1 4 5 0 2 . 0 2 2 5 ND 4 21 .2 2 2 31 .28 .052 8 9 .45 208 .04 2 1 . 4 3 .01 .12 1 6 9 83 .1 4 6 1529 1.89 2 5 ND 6 19 . 4 2 2 30 .25 .069 6 8 .33 257 .04 2 1.13 .02 .16 1 9 7 50 .2 3 6 776 1.69 2 5 NO 3 31 .2 2 2 27 .43 .034 7 7 . 4 4 122 .03 2 1.04 .02 .W 1 6 10 98 .1 4 6 1 3 7 9 1 . M 2 5 NO 2 35 .4 2 2 29 .35 .093 5 8 .34 232 .04 4 .96 .02 .10 I

1 9 7 8 9 .1 4 6 1 2 4 9 1 . 7 7 2 5 ND 2 44 .2 2 2 28 . 4 4 . 1 3 6 5 8 .36 255 .05 2 1 . 1 9 .02 .14 1 34 10 50 .1 6 6 6 9 5 1 . 9 0 2 5 ND 3 33 .2 2 2 32 . 5 2 . 0 2 7 11 8 .34 117 .07 3 1 . 4 1 .03 .17 2 9 12 109 .1 6 6 1 3 4 5 1 . 7 2 4 5 NO 3 32 . J 2 2 28 . 3 4 . 0 7 8 7 8 .30 263 .05 4 1 . 3 1 .02 .15 1 8 10 63 .1 3 5 7 5 0 1 . 5 1 2 5 NO L 24 .2 2 3 26 . 2 5 . 0 4 7 7 7 .28 163 .04 2 .98 .02 .13 1 24 7 28 .2 3 5 4 4 2 1 . 5 6 2 5 ND 1 128 .4 2 2 2 4 5 . 9 4 . 0 2 9 11 9 .34 209 .04 3 .98 .07 .15

L8 NU.040 WE L8 NU.080 WE L 8 NU-120 NE L 8 WU-160 WE LB NU-200 NE

L8 NU-240 HE

L8 NU-320 NE L8 NU-360 HE L8 NU-400 WE

L 8 NU-280 HE

L 8 NU-440 NE 1 1 8 5 73 .1 3 6 1 3 7 8 1 . 7 7 2 5 ND 4 26 .2 2 3 28 3 0 . 0 5 6 6 7 38 244 .03 2 1 . 1 5 .02 .13 l I STANDARD C 18 59 41 131 7.0 70 31 1052 3.95 3 7 18 7 37 53 18 4 16 20 56 46 ,095 38 59 89 101 .07 35 1.89 .06 .13 - - ~

2 7 5 36 .1 2 5 6 1 6 1 . 4 4 2 5 NO 2 24 .2 2 3 28 . 2 7 . 0 3 0 6 7 .27 91 .05 2 .84 .02 .10 1 7 9 69 .1 3 5 1 4 1 2 1 . 5 8 2 5 NO 2 27 .2 2 2 26 . 2 2 . 0 9 7 6 6 .26 258 .05 2 1 . 2 6 .02 .10 1 6 8 48 .1 3 5 8 7 5 1 . 5 3 2 5 NO 3 27 .5 2 2 28 . 2 8 . 0 6 0 7 7 .27 160 .04 6 .95 .02 .ll 1 6 11 60 .1 4 6 1 0 3 0 1 . 6 6 2 5 NO 4 34 .2 2 2 29 . 3 2 . 0 6 9 9 8 .32 196 .OS 2 .92 .02 .ll 1 8 4 3 7 .2 3 5 6 0 8 1 . 5 0 2 5 NO 3 22 .2 2 2 29 . 2 5 . 0 4 1 6 6 .27 116 .04 4 .71 .02 .12

1 8 6 68 .1 4 5 1 1 5 8 1 . 5 7 2 5 ND 3 30 .3 2 2 27 . 3 2 . 0 9 0 b 8 26 225 .05 ' 2 1 . 0 1 .03 .14

1 20 35 02 .1 5 9 8 9 7 2 . 4 7 3 5 ND 10 22 .3 2 3 29 35 .053 14 7 51 4 0 2 .02 3 1 . 2 6 .01 .22 2 7 4 47 .1 5 6 1 0 6 6 1 . 7 7 2 5 ND 4 18 2 2 7 27 2 5 . 0 3 1 8 8 .34 271 .03 2 1 . 1 5 .02 . I 2 1 6 10 6 2 .1 4 6 1 4 2 4 1 . 6 4 4 5 ND 5 22 .2 2 2 26 . 2 9 . 0 4 4 6 9 . 37 204 .03 3 .W .02 .13

1 23 7 3 6 .2 3 5 5 3 5 1 . 5 9 2 5 NO 1 55 . L 2 2 2 3 5 . 7 4 . 0 4 2 10 8 32 139 .ox 3 .a8 .02 .12

ICP - .500 GRAH SAMPLE IS OIGESIED W I T H 3ML 3 - 1 - 2 HCL-HN03-HZO A T 95 DEG. C FOR ONE HOUR AND IS OlLUlED T O 10 ML U l I H UATER. T H I S LEACH IS PARTIAL FOR HN FE SR CA P L A CR MG EA 11 8 U AND LJHITED FOR HA K - SAMPLE TYPE: P b P 6 S O I L P7 ROCK

RU DElECllON L l M J T B Y ICP I S 3 PPM.

DATE RECEIVED: SEP 28 1990 DATE REPORT MAILED: 3 /70 . SIGNED BY.. . . . . . . . . .D.lOIE, C.LEONG, J.WkNG; CERTIFIED B.C. ASSAVERS '?

ISAHPLE# L7-00 N E L7-080 YE L7-120 NE L7-160 WE L7-200 WE

L7-240 WE L7-280 WE L7-320 NE L7-360 YE L7-400 WE

L7-440 WE L7-480 WE L6-00 WE L6-040 WE L6-080 WE

L6-120 WE L6-160 WE L6-200 YE L6-240 WE L6-280 YE

L6-320 W E L6-360 WE L6-400 NE L6-440 NE L6-480 YE

L6-520 YE L6-560 WE L6-600 NE L6-640 WE L6-680 NE

L5-00 NE L5-040 NE L5-080 WE L5-120 WE L5-160 YE

L5-200 WE

Luge 2 SOOkOChoff Consultants InC. I L J J E C T ALFA F I L E # 90-4883

MO Cu Pb 2n Ag N I Co Hn Fe As U Au Th S r Cd 86 B 1 Y Ca P La C r Mg Ba T i B AL NB K u m p p n p p n p p n p p n p p n m p p n X p p n p p n p p n w w P P n w F m P P n P P ” x x p p n p p n X p p n x m x x x p p n

1 1 2 1 1

1 1 1 1 6

1 1 1 1 1

4 1 1 1 1

1 1 1 2 1

1 1 1 1 1

2 1 1 1 1

1 18

33 11 8

10 30

6 7 8 8 8

8 12 11 23 24

16 7 8 5 7

6 8 5 5 9

16 8

10 17 12

8 10 8 7

11

8

11 12 8 5

10

5 8 4 6 4

5 6 6

11 2

15 10 8

12 5

10 10 9

6 7

4 5 6 9 8

8 5 2 8 5

12

59 86 70 77 35

47 32 45 53 53

41 71 54 60 46

131 56 55 40 52

71 83 77 7 7 90

92 66 93 59 97

70 82 46 3 7 b4

45

.2

.2

.2

.l

.2

.1

.1

.1

.1

.2

.2

.2

.2

.2

.2

.2 .1

.2

.1

.2

.1

.2

.1

.1

.3

.3

.1

.1

.2

.4

.1

.2

.2

.1

.2

.1

5 3 4 4 4

3 4 5 4 4

4 3 5 4 3

4 3 5 4 4

3 5 4 4 5

4 5 4 5 5

3 5 4 4 5

3

5 844 1.77 6 1313 1.87 7 1670 1.59 7 934 1.85 4 455 1.43

5 757 1.52 6 444 1.55 6 606 1.79 9 1030 2.34 7 874 2.13

6 615 1.91 8 700 2.44 7 737 2.18 6 b41 1.87 7 1224 1.82

7 1317 1.92 6 891 1.82 5 552 1.60 4 677 1.18 5 691 1.60

5 1125 1.45 6 971 1.80 7 956 1.73 6 989 1.61 7 860 2.05

7 965 1.74 6 630 1.83 6 937 1.88 8 420 2.23 7 936 2.16

7 1450 1.92 6 748 1.78 5 602 1.66 5 502 1.55 6 696 1.17

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

3 3 3 5 2

2 2 2 2 3

2 2 2 2 2

3 5 5 3 3

3

5 5 5 5 5

5 6 5 5 5

5 5 5 5 5

5 5 5 5 5

5 5 5 5 5

5 5 5 6 5

5 5 5 6 5

5

NO NO ND NO N D ND

N D N D ND N D

N D N D WD WD ND

N D N D N D ND NO NO

N D N D N D HD

UD N D N D ND ND

ND ND ND ND NO

3 3 2 5 1

3 4 6 7 6

5 8 6 3 3

6 3 3 2 3

4 6 5 4 4

3 6 3 6 7

4 4 4 4 4

5 586 1.51 . . NO 3 58 40 132 7.1 69 32 1051 3.95 41 18 7 38

33 48 30 27 81 18

26 27 13 24 17

20 25 31 35

28 29 26 2 7 25

2 7 31 18 19 26

59 20 23 25 22

27 30 24 20 30

.2

.4

.3

.2

.3

.2

.2

.2

.2

.2

.2

.2

.2

.3

.5

.6

.2

.2

.2

.2

.5

.2

.4

.5

.5

.4

. 3

. 2

. 3

. 2

.2

. 3

. 2

.2

.2

24 . 3 53 18.4 15

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2

2 35 .55 .028 2 30 .51 .071 2 33 .34 .049 2 31 .26 ,074 2 24 3.31 .059

2 27 .19 ,053 2 31 .22 ,037 2 29 .29 ,058 2 35 .22 ,068 2 36 .32 .050

2 33 .20 .035 2 38 . I 8 ,040 2 31 .27 .045 2 32 .43 .031 2 34 .51 .048

2 25 .31 .lo6 2 31 .27 ,094 2 28 .26 .060 2 23 .22 .045 2 27 .21 ,057

2 24 .25 .046 2 26 .26 ,144 2 29 .19 ,040 2 27 .23 ,045 2 32 .23 ,112

2 27 .81 ,059 2 29 .22 ,055 2 30 .24 ,103 2 34 .27 ,041 2 30 .2S ,060

2 30 .22 .086 2 29 .24 .122 2 29 .24 .060 2 29 .22 ,058 2 29 .28 .072

2 28 .25 ,036 21 55 .46 .094

10 9 5 9 9

6 12 11 13 9

9 11 11 9

11

6 6 6 5 7

10 9 8 5 7

8 9 8

11 10

7 7 8 8 8

7 39 -

9 .34 92 .07 6 .34 330 .04

14 .43 268 .04 10 .45 i 9 2 .03 8 .31 124 .04

8 .27 117 .03 9 .28 73 .05

11 .36 117 .05 10 .56 248 .01 9 .43 208 .03

9 .39 112 .03 10 .58 112 .01 8 .49 166 .05

11 .41 125 .06 9 .38 148 .06

7 .35 250 .03 9 .39 188 .05 8 .29 142 .05 6 .21 109 .04

10 .27 149 .05

8 .27 174 .05 8 .42 266 .04 8 .43 131 .03 9 .38 147 .03

11 .52 181 .04

9 . 4 4 258 .02 10 .40 167 .05

9 .41 202 .04 11 .51 3W .04 10 .52 166 .04

7 .24 247 .04 9 .31 245 .05 8 .30 157 .05 8 .26 113 .04

11 .33 162 .06

8 .28 104 .06 60 .91 181 .07

7 1.32 .03 .12 4 1.32 .02 .14 5 1.14 .02 .14 2 1.06 .02 .13 7 .W .03 .12

2 .76 2 .79 2 1.02 2 1.17 2 1.17

2 .89 2 1.11 3 1.69 2 1.27 4 1.22

4 1.28 2 1.20 3 1.03 4 .60 2 1.09

5 .98 2 1.27 2 .90 2 .94 4 1.41

2 1.01 4 1.38 2 1.42 2 1.45 2 1.52

2 1.15 3 1.28 7 1.00 2 .ba 3-1.09

2 .85 34 1.89

.02

.03

.02

.01

.02

.02

.02

.02

.02

.02

.02

.02

.02

.02

.02

.02

.02

.02

.03

.02

.02

.02

.02

.02

.02

.02

.02

.03

.02

.03

.02

.07 -

.10

.09

.16

.20

.13

.13

.13

.15

.13

.21

.14

.12

.12

.w

.oa

.14

.13

.14

.10

.10

.12

.12

.08

.16 . 14

.12

.10

.11

.10

.15

.13

.13 -

SOokOChOff Consultants InC. PROJECT ALFA F I L E # 9 0 - 4 8 8 3

1 9 11 45 .3 4 5 650 1.64 4 5 NO 5 27 .4 2 3 29 .27 ,040 9 9 .32 113 .06 1 10 7 41 .1 3 5 6101.66 2 5 UO 4 31 .4 2 2 32 .31.038 10 9 .35 93 .05 1 10 7 5 5 .2 4 6 7261.79 2 5 NO 5 28 .2 2 2 34 .26.057 10 10 .42 123 .04 1 12 9 82 .2 5 8 1115 2.02 3 5 NO 7 33 .7 2 4 34 .34 ,053 10 12 .47 326 .05 1 19 10 120 .3 5 8 1210 2.22 4 5 UD 11 32 1.0 2 2 28 .41 .053 13 9 .58 287 .02

L5-480 WE L5-520 WE L5-560 WE LS-600 H E L5-640 U E

L5-680 YE L4-00 N E L4-040 UE L4-080 N E L4-120 UE

L4-160 H E L4-200 N E L4-240 WE L4-280 WE L4-320 WE

L4-360 WE L4-400 WE L4-440 YE L4-480 WE L4-560 WE

L4-600 WE L4-640 WE L4-680 WE L3-00 NE L3-040 UE

L3-080 YE L3-120 NE L3-160 WE L3-200 NE L3-240 UE

L3-280 U E

1 13 14 150 .2 2 7 926 1.97 2 5 ND 5 28 1.4 2 3 32 .36 ,053 10 9 .49 214 .04 4 1.35 .02 .13 1 26 8 146 .5 4 7 5262.26 2 5 UO 8 25 1.0 2 2 29 .32.098 15 9 .43 197 .02 41.52 .02 .17 2 14 8 164 .3 3 6 1107 1.83 2 5 NO 5 4 2 2.5 2 5 25 .48 .079 8 8 .44 285 .03 3 1.26 .02 .17 1 19 7 84 .3 4 6 5501.89 2 5 ND 6 61 .8 2 2 30 .30.068 10 8 .40 379 .05 3 1 . 4 1 .03 .12 1 18 8 67 .4 4 7 6162.23 2 5 UD 6 32 .5 2 2 37 27.064 10 10 .54 181 .07 2 1 . 8 3 .02 .ll

1 18 8 69 .4 4 7 6032.35 2 5 UD 6 31 .3 2 3 39 .28.079 8 10 .48 127 .06 41 .61 .02 .ll 1 31 9 39 .2 5 6 4851 .67 5 5 ND 4 54 .6 2 4 26 55.023 8 9 .30 135 .05 4 1 . 2 8 .04 .12 1 7 7 65 .2 3 8 1 0 4 8 2 . 1 8 4 5 ND 6 27 .5 2 3 36 30.074 8 8 .52 170 .05 31 .25 .02 .16 1 7 10 70 .l 2 6 1 1 6 5 1 . 7 0 2 5 ND 3 29 .2 2 4 30 .26.071 7 9 .36 196 .04 3 .96 .02 .10 1 34 5 95 .2 5 6 7941.86 3 5 ND 6 34 .9 2 2 31 .43.041 11 12 .41 153 .06 5 1 . 3 8 .04 .15

1 8 8 38 .3 3 6 6151.61 4 5 ND 4 23 .2 2 4 30 22.050 7 8 .29 126 .05 4 .81 .02 .10 1 14 8 62 .2 4 5 3361.65 5 5 ND 4 25 .3 2 2 29 .25.057 10 8 .28 96 .06 2 1 . 2 9 .03 .ll 1 22 10 78 .3 4 6 4651.82 7 5 NO 4 27 .2 2 5 32 .36.047 10 9 .37 104 .07 51.38 .03 .ll 1 15 10 74 .3 7 7 491 1.82 10 5 UD 6 27 .7 2 4 31 .26 ,086 11 9 .37 122 .06 2 1.21 .03 .ll 1 23 10 74 .3 6 9 7132.38 3 5 ND 8 37 .3 2 4 43 .36.050 14 11 .59 100 .06 21.61 .02 .20

1 13 29 118 .5 4 9 1 7 8 6 2 . 6 9 2 5 NO 9 48 .6 2 3 45 .52.082 9 10 .67 331 .07 71 .74 .02 .16 1 14 9 79 .2 4 7 5712.32 2 5 NO 7 26 .2 2 2 38 .27.064 11 10 .52 176 .07 2 1 . 6 8 .02 .12 2 17 8 52 .4 3 6 9041.73 3 5 NO 5 30 .3 2 2 27 .28.043 9 8 .36 204 .05 5 1 . 4 7 .02 .13 1 16 4 65 .3 3 7 6302.10 2 5 NO 9 31 .3 2 4 35 .35.048 10 8 .44 178 .06 4 1 . 5 2 .02 .17 1 130 4 893 .5 4 7 7821.96 3 5 NO 6 37 7.9 2 3 29 .41.057 11 10 .50 153 .05 6 1 . 5 8 .02 .10

1 22 5 150 .1 4 8 6742.22 4 5 ND 6 25 1.3 2 4 33 .28.058 12 10 .55 169 .05 2 1 . 6 9 .02 .15 1 17 2 70 .2 3 8 9582.19 2 5 NO 8 25 .2 2 3 26 .28.055 13 7 .48 304 .03 41 .53 .02 .22 1 30 9 79 . 3 5 9 8082.67 3 5 NO 10 28 .2 2 3 4 3 .31 ,046 14 12 .56 152 .09 3 2 . 3 2 .02 .16 2 26 6 70 .3 4 8 5682.36 2 5 NO 6 26 .4 2 5 33 .30.063 12 7 .51 168 .04 4 1 . 6 6 .02 .16 6 12 8 98 .2 3 7 8482.41 5 5 UD 5 27 .3 2 2 32 .23.074 7 8 .42 170 .04 2 1 . 4 7 .02 .ll

2 43 11 143 . 4 5 5 6261.71 3 5 ND 4 51 1.7 2 4 23 .50.024 10 8 .31 116 .06 4 1 . 3 6 .04 .ll 1 10 11 75 .2 5 6 4971.85 7 5 NO 3 36 .2 2 2 32 .25.126 7 8 .32 156 .06 3 1 . 5 9 .03 .10 1 19 10 53 .2 5 6 4111.90 7 5 NO 6 30 .3 2 2 36 .31 ,035 13 10 .35 109 .06 41 .15 .03 .15 1 9 7 48 .1 3 5 4211.73 5 5 NO 4 27 .2 2 2 32 .26.053 8 9 .31 94 .06 4 .96 .03 .13 1 24 6 43 .6 4 4 3361.56 3 5 NO 3 101 .4 2 2 265 .02 .039 8 8 .35 109 .04 5 1 . 0 7 .05 .ll

1 9 7 40 .1 3 5 3401.69 2 5 NO 5 24 .3 2 4 31 .28.031 8 7 .29 61 .05 2 .91 .02 .10 1 18 60 39 130 7.2 70 32 1052 3.95 42 17 7 38 53 18.4 16 22 5 5 .46 .096 38 59 .89 181 .07 36 1.89 .06 .13 15 -

r

SAMPLE# no Cu Pb 2n Ag N I Co Hn Fe AS U Au l h Sr Cd Sb B1 V Ca P La C r Hg Ba T i 8 A l Ha K u

L3-320 LIE 1 6 8 42 .1 2 6 4641.75 2 5 ND 4 25 .2 2 2 30 .31 .028 5 8 .42 73 .05 2 .91 .02 .12 2 L3-360 WE 1 1 1 20 96 .8 3 8 9692.18 2 5 ND 7 17 .2 3 2 24 .24.071 8 7 .54 359 .01 21.23 .01 .20 I L3.400 WE 1 7 6 75 .2 3 6 9281.90 3 5 ND 6 18 .2 2 2 27 .21 ,055 6 6 .48 171 .04 41.23 .01 .10 1 L3-440 WE 2 9 7 69 .2 4 7 8602.03 4 5 ND 18 21 .2 3 4 29 .28.044 5 9 .47 191 .04 31.50 .02 . l l 1 L3-480 ME 1 12 10 101 .2 3 6 8411.79 2 5 NO 4 23 .2 2 2 24 .25.072 7 7 .40 231 .04 21.43 .02 . l l 1

w w w m m m w m ~ w w P P n P P n m w p p n m p p n % ~ w p p n x w x w % x x p p n

L2-00 WE L2-040 ME L2-080 HE L2-120 NE L2.200 HE

L2-240 HE L2-280 WE

L2.360 NE L2-400 NE

L2-440 n E L2-480 NE L1-00 NE L1.040 WE L1-120 NE

L1-160 WE L1.200 NE L1.280 NE L1-320 WE L1-360 NE

Ll-440 WE L1-480 WE LO-00 WE LO-040 WE LO-080 WE

L2.320 NE

1 10 10 99 .2 5 8 9302.52 4 5 NO 5 57 .2 3 2 35 .40.094 12 9 .70 246 .02 21.68 .02 .09 3 13 20 93 .3 3 7 4802.19 4 5 NO 6 29 .2 2 2 29 .22.037 10 7 .39 137 .06 21.38 .02 .14 5 21 40 207 .4 4 7 8142.35 5 5 N D 4 29 .9 2 2 28 .28.050 10 8 .38 179 .05 31.81 .02 .ll 5 20 36 309 . 3 3 710532.47 4 5 ND 5 23 3.1 2 2 23 .29.062 9 7 .45 300 .03 41,51 .01 .18 10 43 56 244 .9 7 9 957 3.60 3 5 N O 7 21 .8 2 2 20 .27 ,103 17 5 .45 254 .03 4 1.72 .01 .14

2 15 10 134 .1 3 7 7771.80 3 5 N O 3 28 .2 2 2 24 .27.039 6 6 .37 182 .04 21.20 .02 .14 1 10 7 90 .1 4 6 7281.94 4 5 N D 4 23 2 2 2 31 .24.051 6 7 .40 155 .05 51.30 .02 .15

1 12 7 82 .l 4 610212.03 2 5 N O 3 31 .2 3 2 32 .39.082 7 9 .46 179 .05 31.M .02 .10 1 51 19 95 .2 4 8 8 4 3 2 . 3 3 2 5 HD 3 35 . 2 2 2 33 .77.053 6 1 1 .59 186 .03 51.49 .02 .13

1 15 8 62 .1 4 7 4762.18 2 5 ND 6 26 .2 2 2 35 2s ,051 7 8 .49 103 .O6 21.64 .02 .14 1 14 12 105 .2 3 7 9 9 8 2 . 1 5 2 5 ND 5 36 2 3 2 33 .35.123 8 1 1 .55 201 .05 31.70 .02 .12 1 13 9 100 .1 4 5 6661.67 6 5 NO 3 28 .2 2 2 25 .24.0W 7 7 .34 147 .@4 21.23 .01 .09 1 14 12 108 .2 4 5 8861.70 3 5 N D 3 45 .2 2 2 25 .35.088 7 8 .37 199 .04 31,26 .02 .12 3 10 10 99 .2 3 912222.85 2 5 NO 6 26 . 3 3 2 37 .44.065 16 8 .71 313 .01 41.38 .Ol .I6

10 32 95 258 .9 5 9 785 3.32 2 5 N O 1 1 22 1.2 2 2 24 .28 .055 1 1 6 .51 348 .03 2 1.59 .01 .20 3 17 17 118 .1 4 7 6882.40 6 5 NO 6 24 .2 2 2 25 .28.059 10 7 .47 315 .03 21.57 .02 .18 1 10 12 102 .Z 5 6 587l.Z 3 5 NO 3 30 .2 2 2 26 .28.055 6 9 .38 162 .05 31.40 .02 .12 1 14 8 116 .2 4 5 9771.61 2 5 N O 2 47 .2 2 2 24 .55.102 6 6 .36 257 .04 61.24 .02 .15 1 22 12 BB .2 5 8 7792.21 2 5 NO 5 28 .2 2 2 35 .32.051 8 1 1 .52 130 .05 21.49 .02 .12

1 13 7 74 .2 6 711322.18 4 5 NO L 29 .2 2 2 33 .30.063 9 10 .49 246 .06 21.96 .02 .13 1 23 14 60 .1 6 7 4132.37 4 5 N O 6 29 .2 2 2 39 .32.045 12 1 1 .44 156 .08 32.51 .02 .ll 1 21 8 64 .2 4 6 5451.98 2 5 N D 5 97 .2 2 3 21 .59.045 10 9 .53 123 .04 51.35 .03 .14 1 1 1 13 68 .l 5 7 5912.22 2 5 ND 8 26 .2 2 2 32 25.048 8 10 .58 100 .04 51.40 .02 .14 1 18 15 63 .2 6 8 5162.54 2 5 N O 7 36 2 4 2 35 .28.060 14 1 1 .54 196 .06 22.27 .02 .17 1

1 10 7 90 .2 3 7 8542.31 z 5 no 5 35 .2 2 2 32 .40.108 Q Q .6i 128 .03 21.46 .oi .lo

LO-160 N E LO-ZOO n E LO.240 H E LO-280 N E LO-360 n E

1 14 12 83 . 3 6 7 6531.91 3 5 N D 6 22 .3 2 2 29 .21 ,075 P 10 .41 185 .05 31.48 .02 .ll 1 1 1 1 8 92 .1 4 6 4801.85 4 5 N D 5 24 .2 2 2 30 .22.106 P 8 .40 146 .05 21.37 .02 .10 1 1 22 10 50 . 4 4 7 2992.06 2 1 ND 5 37 . 2 7 2 32 .52.019 12 10 .38 '114 .05 11.49 .03 .09 1 1 51 9 79 .2 6 8 6762.68 2 5 ND 6 24 .2 2 ? 45 .2F.l28 V 1 1 .63 102 .05 21.85 .02 .09 1 1 43 13 102 .1 6 116762.08 3 5 ND 3 35 .3 7 2 3 1 . 5 0 . 0 8 8 f! i : .it? 344 .06 61.84 .02 .11 1

Sookochoff Consultants Inc. PROJECT ALFA F I L E # 9 0 - 4 8 8 3 Page 5 SAIIPLEU

LO-480 NE LOO-1600 SW LOO-1560 SW LOO-1480 su LOO-1440 sw

____ no Cu Pb 2n Ag N i Co nn Fe As U A" Th Sr Cd Sb E i

p p n p p n p p n p p n p p n p p n m p n p p n X m p p n m w p p n p p n F F m

1 12 11 72 .2 6 6 659 1.99 6 5 NO 4 24 . 4 2 2 1 8 14 78 .1 5 6 6 1 0 1 . 9 3 3 5 ND 4 23 . 4 2 2 1 9 13 87 .2 4 7 681 1.90 2 5 N O 4 31 . 4 2 2 1 8 22 183 .3 4 6 738 2.12 3 5 NO 6 30 .4 2 2 1 7 24 106 .2 5 7 559 2.20 2 5 NO 5 25 . 3 ? 2

LOO-1400 S W LOO-1360 SW LOO-1320 SW LOO-1280 sw LOO-1240 SW

I LOO-400 sw 1 7 7 11 33 .1 5 4 ?99 1.55 2 b NO 4 23 .2 7 4

LOO-1200 su LOO-1160 su LOO-1120 5Y LOO-1080 SY LOO-1040 sw

LOO-800 su LOO-760 SU LOO-720 SU 100-680 sw 100-640 su LOO-600 SW LOO-560 SU LOO-520 SU 100-480 SW LOO-440 SU

LOO-360 SW LOO-320 SU LOO-280 su L100-156OSW

LOO-1000 sw LOO-960 SW LOO-920 SW LOO-880 sw LOO-840 su

1 10 7 90 .2 5 b 1376 1.76 3 5 ND 3 40 .3 2 2 29 .30 ,137 1 25 15 75 .4 7 6 564 1.90 4 5 ND 4 57 . 3 2 2 27 .39 ,044 1 13 9 61 .3 6 6 496 1.79 5 5 NO 4 53 .I. 2 2 27 .20 ,On 1 17 8 120 .3 6 10 1027 2.94 3 5 ND 7 40 .2 2 2 26 .31 ,087 2 21 184 128 2.0 4 8 1257 2.41 2 5 ND 7 43 -4 2 ?

1 19 18 9 7 .7 6 9 8 5 5 2 . 5 2 2 8 N O 5 36 .2 2 2 26 . 2 0 . 0 8 7 1 1 10 .57 380 .03 b 1 . 8 7 .02 .19 1 1 32 24 150 . 4 5 1 2 1 3 4 7 3 . 1 6 2 5 NO 9 4 4 .3 2 2 36 . 4 3 . 1 2 4 15 I ? .74 580 .02 5 1 . 8 3 .02 .24 1 1 18 52 120 .5 7 10 8 5 4 2 . 8 2 3 5 NO 7 34 . 2 2 2 31 . 3 0 . 0 7 0 16 10 .65 306 .04 5 1 . 8 8 .02 .25 1 2 15 15 62 .3 5 6 3 3 0 1 . 9 5 2 8 ND 4 49 .2 2 2 29 . 4 0 . 0 3 8 1 1 10 .34 152 .05 4 1 . 3 9 .03 .14 1 2 11 3 7 193 .9 8 5 1 6 L 8 1 . 8 9 3 5 NO 1 1 41 .6 2 2 18 . 3 2 . 1 8 0 53 7 .Z2 295 .03 6 1 . 6 9 .02 .14 1

~~ ~ ~ ~~ ~~ 13 6 .28 95 .05 2 1.48 .02 .10 5 1 9 11 48 .1 6 5 5 5 5 1 . n 4 5 NO 4 29 . 4 2 2 29 . 2 8 . 0 4 9 9 8 .32 154 .04 3 1 . 2 9 .02 .13 1 1 12 12 68 . 3 6 7 6 9 5 2 . 0 4 4 5 NO 5 26 . 4 2 2 35 . 2 8 . 0 4 4 10 10 .37 164 .05 3 1 . 2 0 .02 .14 1 1 14 8 74 .3 6 8 1227 2.34 2 5 NO 5 49 .2 2 2 33 .49 ,095 12 10 .49 357 .05 7 1.94 .03 .22 1 1 13 112 673 . 4 5 7 2 2 5 2 2 . 2 6 3 5 NO 4 46 2.0 2 2 27 . 3 9 . 1 7 7 10 8 .50 489 .07 2 1 . 7 9 .03 .18 1

.

2 13 2 13 1 11 1 17 1 13

1 12 1 16 1 12 1 7 1 10

1 12 1 16 1 16 1 14 1 15

1100-1520 SY STANDARD C

64 224 3 1 213 24 156

1 55 382 790 .5 5 6 1156 2.79 2 5 ND 6 39 1.3 Z 3 18 59 38 132 7.1 69 32 1054 3.95 39 18 8 37 53 10.6 I4 L? .~ ~~ ~ ~ .. ~~ ~ ~

36 215 25 121

23 108 98 169 24 137 28 181 52 178

43 145 234 174 30 101 32 115 18 94

. 4 2 7 652 3.88

. 4 13 8 905 2.36

.3 9 7 1212 1.96

.3 14 11 1372 2.63

.5 7 9 781 2.98

. 4 7 9 766 3 .22

.3 7 11 804 3 . 4 4

.3 5 11 1085 3.27

.3 6 4 1501 1.20

.3 6 7 1307 2.37

.2 5 7 1004 2.05

.5 6 9 2172 2.72

.2 6 8 856 2.18

.4 6 8 1018 2.31

.3 6 8 1423 2.34

5 5 N D 2 5 3 . 4 2 2 2 5 N D 5 3 5 . 4 2 2 3 5 H D 5 3 0 . 0 2 2 2 5 N D 4 3 4 . 4 2 2 2 5 N D 7 3 5 . 2 2 2

2 5 NO 6 41 .3 7 2 ~. 3 5 N D 4 4 1 . 6 2 2 2 5 ND 6 38 . 4 2 2 4 5 YD 13 69 .5 2 2 2 5 N Q 6 3 2 . 3 2 2

3 5 N D 5 2 3 . 4 2 2 2 5 N D 6 2 5 . 2 2 2 3 5 N D 4 4 5 . 2 2 2 2 5 N D 5 2 7 . 3 2 2 3 5 N 0 5 3 1 . 4 2 2

v ca P P P n % X

35 .26 ,087 33 .26 ,036 39 .32 .023 33 .3? .a53 34 .27 .044

La Cr Wg Ea T i E A 1 Na I: U m m X p p n x p p n x x x m

9 11 .42 173 .06 7 1.63 .03 .12 1 8 11 .42 164 .07 5 1.34 .03 .16

10 12 53 118 .07 2 '.35 .03 .15

10 11 37 110 .09 5 1 27 .04 .21 11 12 . L l 155 .08 5 1.34 .OL .17

37 . 3 5 . 0 5 7 12 16 .54 193 .06 6 1 . 2 8 .03 .14

22 .46 ,107 11 6 .49 210 .10 2 1.68 .03 .24 51 .40 ,058 11 20 .78 161 .W 6 1.69 .04 .15

53 .41 ,064 53 .37 ,053

11 21 .96 190 .08 3 1.65 .03 .17 14 13 .64 121 .12 3 2.15 .03 . I8

58 . 4 4 -065 1 1 17 .77 112 .ll 2 2.24 .03 .16 1 63 .41 .067 13 13 .E l 118 .13 3 2.36 .03 .16 1 50 .41 ,063 12 11 .84 144 .ll 4 2.01 .03 .18 1 14 . 5 4 . 0 6 2 41 8 .19 210 .02 2 .75 .02 .ll 1 35 .28 ,056 15 14 .53 245 .05 2 2.07 .02 .15 1

32 .24 ,050 26 .25 .054 34 .35 ,037 30 .25 ,055 28 .32 ,082

24 .39 ,060

75 . 1 7 . 0 2 4

11 13 .L6 244 .04 2 1.28 .02 .17 1 14 9 .63 b06 .04 4 2.06 .02 .21 1 10 13 .50 267 .06 4 1.58 .03 . I 7 1 13 10 .66 301 .06 3 1.92 .02 .16 1 11 8 .50 494 .04 2 1.70 .02 .18 1

7 9 .36 345 .05 4 1 . 3 1 .03 .ll 1 14 F .35 174 .05 5 1.68 .04 .13 1 12 F 35 105 .06 L 1 71 .04 .10 1 12 I 2 .65 544 .02 6 1 85 .02 .19 1 0 8 60 340 .02 L 1 61 02 .17 1

74 .48 ,007 56 .46 .091

~ ~~

10 6 .48 170 .05 2 1.63 .02 .15 37 5Y .8Y 180 .07 35 1.89 .07 .13

~~ ~~~ ~ .

Sookochoff Consultants Inc. PROJECT ALFA F I L E i: 9 0 - 4 8 8 3 Page 6 SAMPLE#

1100-1480 SU L100-1440 SU 1100-1400 SU 1100-1360 SU 1100-1320 SU

. l oo -1231 S r

.109-1243 5.

.101-11t3 S" 1100-1120 su 1100-1080 su 1100-1040 SU 1100-1000 su 1100-400 SU 1100-360 SU L100.320 SU

1100-280 su L100-240 sv 1100-200 su 1100-160 SU L 1 0 0 ~ 1 2 0 su

1100-080 su 1100.040 SU L100-00 su BL OO+lOOO uu STANDARD C

no Cu Pb Zn Ag H I Co Hn Fe As U A" l h S r Cd Sb 01 V Ca P La C r Hg 0 a T i 0 A L Ua K u ) F m p p n p p n p p n p p n p p n w w ~ p p n w F P F P P P n p p n p P m P P n P p n % x w w x w % p p n % % x p p n

1 1 2 1 1

1 1 1 1 1

1 1 3 1 1

1 1 1 1 1

1 1 1 1

7 5

20 10

11

12 9

12 8

15

12 5

78 13 14

15 15 9

26 14

19 27 18 13

19 59

35 271 15 106 30 307 15 109 13 149

20 175 14 103 11 128 20 96 '79 101

14 70 11 84 9 91 5 94 5 8 1

5 83 5 71 5 108

13 75 5 77

7 50 7 72

13 113 7 68

36 131

.l

.1

.1

.1

.2

.2

.1

. 1

.2

.4

. 1

. 2

.6

.5

.2

.4

.l

. 4

.6

. 3

.2

.2

. 3

.1 7 . 1 -

1 6 9

10 9

6 7 4 3 7

3 10 5

6 6

7 6 4 6 6

5 6 5

72 4

-

5 687 1.59 6 593 1.64 7 980 2.16 8 667 1.86 9 1221 2.65

9 1034 2.66 9 544 2.76 6 934 1.78 6 706 1.81 6 816 2.05

5 4% 1.70 . . 6 953 1.64

18 996 4.38 7 568 2.19 6 800 1.73

7 5 8 8 1.97 6 513 1.86 7 999 1 .PO 8 546 7.12 8 673 2.25

7 574 2.12 9 664 2.33

11 908 2.73 5 789 1 .bC

32 1049 3.95

2 3 6 7 8

10 2 4 2 7

2 7 9 6 3

8 3 7 7 3

2 6 2 6

4 0 -

5 5 5 5 5

5 5 5 5 5

5 5 5 7 6

5 5 5 5 5

5 17

7 5

18 ~-

NO NO N D NO NO

NO NO NO ND NO

NO NO NO N O N D

NO NO NO NO NO

LID ND NO NO

7

2 2 4 3 3

7 4 3 5 8

3 3 7 5 4

5 2 6 6 5

4 4 6 2

39

27 .2 19 .7 28 1.0 24 .5 37 .2

42 1.1 39 .9 32 .2 27 .3 40 .4

29 .7 3 1 .2 53 .3 26 .2 26 .2

27 . 7 24 .2 32 .4 i 6 1.0 29 .2

61 .2 62 .5 3b .2 35 .2 56 19.0 -

2 7 2 2 3

3 2 2 4 2

2 2 2 4 2

2 2 2 2 2

2 7 2 2

1 5

2 2 2 3 2

2 2 7 2 2

2 3 2 2 2

7 2 2 2 2

2 2 2 2

20 ~~~

20 .28 ,024 7 26 .20 .035 9 35 .28 ,081 12 36 .25 ,042 8 46 .29 .138 9

5 .26 130 .06 6 .29 112 .05

10 .45 139 .06 15 .53 192 .08

11 ,&a 190 .06

42 .40 ,130 10 9 .63 139 .10 45 .34 ,051 11 8 .b6 97 .10 26 .39 ,041 10 5 .30 186 .04 26 .22 .048 13 7M .31 .003 102

30 .21 .037 75 .30 .048 74 .66 .119 38 .25 ,069 28 .74 ,063

32 .77 ,073 29 .22 ,064 28 .33 .074 31 .23 ,070 36 .33 ,060

32 -64 ,041 32 .34 ,045 38 .28 ,056 2 1 .78 ,175 57 .45 ,097

~ ~~~ ~~~~ ~-

7 12 8 7 7

8 4

10 10 11

10 15 11 6

39

6 .32 187 .04 8 .29 l a 6 .08

2 1.10 .01 .ll 2 .95 .01 .10 2 1.72 .02 .10 2 1.11 .01 .12 2 1.96 .02 .10

2 2.27 .02 .08 2 1 . 9 3 .01 .ll 4 .98 .02 .13 2 1 . 0 6 .01 .14 2 2.34 .02 .10

6 25 115 .06 4 .T3 .03 .15 1 7 .25 248 .05 3 1.08 .03 .13 1

13 1.11 133 .07 4 2.17 .02 .10 1 8 . 44 119 .06 2 1.32 .03 .09 1 6 .41 130 .05 2 1.19 .02 .09 1

6 .43 108 .06 5 .40 124 .05 7 .41 175 .05 6 .L6 148 .05 6 .50 151 .07

7 .52 141 .04 6 .57 136 .05 8 .67 154 .05

3 1.44 .02 .08 1 2 1.21 .02 .09 1 2 1 . 3 5 .02 .ll 1 2 1.46 .02 .12 1 2 1.64 .02 .13 1

Appendix I1

VLF-EM, RAW DATA

APOLLO DEVELOPMENT I VLF-EM R A W DATA

a o o N a o o N a o o N

a o o N 8 0 0 N

800 N 8 0 0 N 8 0 0 N 800 N 8 0 0 N 8 0 0 N 800 N

800 N

a 0 0 N 800 N 300 N 900 N 800 N 800 N 800 N 700 tJ 700 N '700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 700 N 650 N 650 N 650 N 650 N 650 N

a o o N a o o N

-320 w -240 w -200 w -160 W -120 w -40 w

o w 40 E 80 E 120 E 160 E 200 E 240 E

320 E 360 E 400 E 440 E

500 E -<so w -440 w -400 w -360 W -320 w -240 w -200 w -160 W -120 w -40 w o w

40 E

120 E 160 E 200 E 240 E

320 E 360 E 400 E 440 E 480 E 500 E 250 E 260 E 270 E 280 E 290 E

- 2 8 0 w

- a0 w

280 E

480 E

-280 w

- 8 0 w

a o E

280 E

5 7

9 7 4 5 6 G 7 6 5 5 7 2 8

1: 10

G

a

c

_. >

i

I

5 4

3 4 3 2 2 1 1 1 1 4 4 4 5 1 8 12 11

8 5 4 7 3 4 3 0

_I

APOLLO DEVELOPMENT I VLF-EM RAW DA'I'I?

650 N 650 N G50 N 650 N 650 N 650 N 650 N G 5 0 N G50 N G50 N 650 N 650 N G50 N 650 N G50 N G50 N 650 N 650 N 650 N G50 N 650 N 650 N 650 N 650 N C Ti (2 N 550 N 650 N 650 N G50 N G50 N 650 N GOO N GOO N GOO N 600 N 600 N GOO N 600 N GOO N GOO N GOO N GOO N G O O N GOO N GOO N GOO N GOO N GOO N GOO N 600 N GOO N GOO N 600 N

300 E 310 E 320 Fz 330 E 340 E 350 E 360 E 370 E 380 E 390 E 400 E $10 E 4 2 0 E ,430 E -140 E 450 E 4G0 E 470 E 480 E 490 E 500 E 510 E 520 E 530 E 540 E 550 E 5G0 i: 570 E 580 E 590 E GO0 E

-480 W -440 w -400 w -360 W -320 W -280 W -240 W -200 !.I -1GO W -120 w -80 W -40 w

o w 40 E 80 E 120 E 160 E 200 E 240 E 250 E 260 E 270 E

-1 -1

1 3

7 9

1 4 12 1i 11 10 1 0

3 r, 9 7

I 3 6

- 3

-,

- 3

7 2 5 6 2 8 3 2 3 4 7 4 i 4 5 7 3 1 0 2

-2 1 0 3 7 5 5 5 4

.I

APOLLO DEVELOPMENT I VLF-EM R A W DATA

GOO N GOO N GOO N GOO N G O O N G O O N 6 0 0 N 6 0 0 N G O O N G O O N GOO N 600 N C O O N GOO N 600 N G O O N ,500 N 600 1.1 G O O N C O O N GOO N 600 N 600 N G O O N GOO N 600 N GOO N GOO N GOO N GOO N GOO N GOO N GOO N GOO N GOO N G O O N G O O N G O O N 550 N 5 5 0 N 5 5 0 N 550 N 550 N 550 N 550 N 550 N 550 N 550 N 550 N 550 N 550 N 550 N 550 N

280 E 4 290 E 2 300 E 4 310 E 2 320 E 3 330 E 5 340 E 350 F.

4 7 -

360 E 7 370 E 10 380 E 12 390 E 13 400 E 1 1 ~~

410 E 12 420 E '3

430 E 10 440 E 0 450 E 8 460 E 9 470 E 1: 480 E 12 490 E 10 500 E 10 510 E 10 52c z G 530 E i 540 E 5 550 E G 5G0 E 3 570 E G 580 E G 590 E 7 GOO E 5 620 E 5 640 E 3 G G O E 4 6 8 0 E 3 7 0 0 E 4 G O O W -3 590 W 3 580 W 5 570 W 4 560 W 5 550 W 5 540 W 9 530 W 7 520 W 8 510 W 12 500 W 13 490 W 8 4 8 0 W 8 470 W 6 460 W 6

APOLLO DEVELOPMENT I VLF-EM RAW DATA

550 N 550 N 550 N 550 N 550 N 550 N 550 N 550 N 550 I.J 550 N 550 N 550 N 550 N 550 I T 550 N 550 N 550 N 550 N 550 N 550 N 550 N 500 IJ 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N 500 N

450 W 440 W 430 W 420 W 410 W 400 W 390 W 380 W 370 W 360 W 350 W 340 W 330 W 320 W 310 W 300 W 290 w 280 w 270 \$ 260 W 250 W

-480 W -440 w -400 w -360 W -320 w -280 W -240 w -200 w -160 W -120 w -80 W -40 w

o w 40 E 80 E 120 E 160 E 200 E 240 E 250 E 260 E 270 E 280 E 290 E 300 E 310 E 320 E 330 E 340 E 350 E 360 E

7 G 3 3 3 6 7 6 7 5 5 5 4 4 3

-3 -5 -1

2

4 3 2 2 4 2 3 3 3 4 4 2 3 2 1 0 5 5 9 9 9 5 4

-3 -1 -3 0 1 3 2 4 3

I

370 E 6


500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 190 500 500 500 2 50 4 50 < 50 4 50 $50 450 450 450 4 50 450 450 450 450 450 450 450 450 450 450 450 450 450 450 450 450

N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N N

360 E 5 390 E 4 400 E 5 410 E 420 E 2 430 F: 440 E 450 E 5 460 E 7

470 E 6 480 E 7 ~~~ ~

490 E 6 500 E 6

6 510 E 520 E 530 E 6

7

540 E 7 550 E a 560 E 570 E 580 E 590 E 600 E 7

620 E -3 640 E 2 G G O E 0 680 E 1 700 E 2 240 E 8 250 E 8 2G0 E 7 270 E 4 280 E 1 290 E -5 300 E -4 310 E 0 320 E 3 330 E 2 340 E 2 350 E 2 360 E 3 370 E 3 380 E 2 ~~~ ~

390 E 4 400 E 4 410 E 4 420 E 5 430 E 6 440 E 6 450 E 6 460 E 7 470 E 8 460 E 8

APOLLO DEVELOPMEN'T 1 VLF-EM R A W DATA

,150 N 4 5 0 N 350 N 4\50 N .I 5 0 N .i 5 0 1.J :so N .1 5 0 N ;50 ?J 450 P I *:>O N ; .5 0 :J .: 0 0 :J ** 0 0 IJ ; 0 0 I : .I 9 0 p; 1130 N r.00 1 .100 l.! : 0 0 f: 1 2 0 N ; (U3 1: -190 :I ~; 0 0 :J .; 0 0 PJ .:00 N

t o o N -2 0 0 TJ $00 N ;00 N ~1 0 0 N 400 !J -1 0 0 I i 100 N .'* 0 0 N ,400 N 400 N 400 N ,00 N 1, 0 0 N 400 N 400 N 400 N 400 N 400 N 400 N 4 0 0 N 4 0 0 N 4 0 0 N 400 N 4 0 0 N 4 0 0 N

. -

.I 0 o r:

4 9 0 E 500 E 510 E 5 2 0 E 530 E 5 4 0 E 550 E 5 6 0 E 5 7 0 E

5 9 0 E G O O E

-440 w - 4 0 0 w - 3 G O W - 3 2 0 w - 2 8 0 W - 2 4 0 w -200 w - l G O W - 1 2 0 w

-80 W - 4 0 w

0 I4 2 0 E 4 0 E G O E 8 0 E

1 0 0 E 1 2 0 E 140 E 160 E 1 8 0 E 2 0 0 E 2 2 0 E 2 4 0 E 2 5 0 E 2 6 0 E 2 7 0 E

2 9 0 E 300 E 3 1 0 E 3 2 0 E 3 3 0 E 3 4 0 E 3 5 0 E 3 6 0 E 370 E

3 9 0 E 4 0 0 E

580 E

- 4 8 0 w

2 8 0 E

3 8 0 E

G G 7 8 7 9 9 G I

1 0 6 5

-1 0 0 1 1

-1 0 2 5

3 5

0 -1 -2 -3 -1 1 1 2

-2 -2

5 9 9

10 8 9 8 6 1 0 3 2 6

9 9 9 9

.,

7 2

a

APOLLO DEVELOPMEI!T 1 VLF-EM R A W DATA

400 N 400 N 3 0 0 N 400 N ,400 N 400 N ,400 N 400 N 3 0 0 N .'. 0 0 N 400 N 400 N 400 N 400 N 400 N .:00 N .:00 N :00 N .; 0 0 PJ .: 0 0 I\' ;00 N .: 0 !I N .1 0 0 N :00 N -400 N 300 N 300 N 300 N 300 N 300 N 300 N 300 N 300 N 3 0 0 N 3 0 0 N 300 N 3 0 0 N 3 0 0 N 3 0 0 N 3 0 0 N 3 0 0 N 300 N 3 0 0 N 300 N 300 N 3 0 0 N 3 0 0 N 300 N 300 N 300 N 3 0 0 N 3 0 0 N 300 N

410 E 420 E 430 E 440 E 450 E 460 E 470 E 480 E 490 E 500 E 510 E 520 E 530 E 540 E 550 E 560 E 570 E 580 E 590 E G O O E 620 E 640 I.: G G O E 660 E 700 E

-480 w -440 W -400 w -360 W -320 w -280 W -240 W -200 w -160 W -120 W -80 W -40 w

O W 20 E 40 E 60 E 8 0 E 100 E 120 E 140 E 160 E 180 E 200 E 220 E 240 E 260 E 280 E 300 E

6 7 11 1 1 10 9 10 'I 0 il 11 1~ 2 11 9

; ? 1 0 I!

1 1

I i :3 I i

: '> . ..

L( - 3

7 >

~

i

3 G 5 G 5 5 2 3 3 2 4 2 3 2 1 2 0

-1 -2 -1 0

-1 -1 0 2 2 1


300 N 300 N 300 N 300 N 300 N 300 N 300 N 300 N 300 N 300 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 700 N 200 N 200 IJ 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 200 N 100 N 100 N 100 N 100 N 100 N

320 E 340 E 360 E 380 E 400 E 420 E 440 E 460 E 480 E 500 E

-460 w -440 w -400 w -360 W -320 w -280 W -240 w -200 w -160 W -120 w -60 w - 3 0 w 0 w

20 E 40 E 60 E 80 E 100 E 120 E 140 E 160 E 180 E 200 E 220 E 240 E 260 E 280 E 300 E 320 E 340 E 360 E 380 E 400 E 420 E 440 E 460 E 480 E 500 E

-480 W -440 w -400 w -360 W -320 w

-7 -4 -1 0 2 2 0 1 2 4 8 10 10 10 12

9 9 3 3

3 1

". ( 1

11 13 14 13 11 10 10 11

9 3 8 10 11 9 9 10

9 8 6 4 6 9 9 10 9 9 7 6 9 10


100 N 1 0 0 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 N 100 1J 100 N 100 N 100 N 100 N 100 N 100 N 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s

-280 W -240 W -200 w -160 W -120 w -80 W -40 w -20 w

o w 20 E 40 E 60 E 80 E 100 E 120 E 140 E 160 E 180 E 200 E 220 E 240 E 260 E 280 E 300 E 3?0 E 360 E 400 E 4 4 0 E 4 8 0 E

-1000 w -960 W -920 w -880 W -840 W -800 W -760 W -720 w - G 8 0 W -640 W -600 W -560 W -520 W -480 W -440 w -400 w -360 W -320 w -280 W -240 w -200 w -160 W -120 w -80 W

14 14 15 15 18 1 9 16

I 1 10 10 10 10

8 c

12 10 10 9

10

7 1 i .*

9 Y

-

5 4 2 0

- 3 -2 - 1 1 2 1 0 1 2 1 3 3 4 3 3 3 2 3 6 7

AF’O1.I.O DEVELOPMENT I VI>I’-EM RAW DATA

100 s 100 s

O N O N O N O N O N O N 0 N O N O N O N O N 0 N 0 1.1 0 N O N 0 N O N O N O N O N O N 0 PJ 0 N O N 0 tJ

100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s

-40 w o w

20 E 40 E GO E 80 E 100 E 120 E 140 E 1 G O E 180 E 200 E 220 E 240 E 260 E 280 E 300 E 320 E 340 E 360 E 380 E 400 E .: 2 0 E

-160 E 480 E 500 E

-1000 E -960 E -320 E -880 E -840 E -800 E -760 E -720 E -680 E - 6 4 0 E -600 E - 5 6 0 E -520 E -480 E -440 E -400 E -360 E -320 E -280 E -240 E -200 E -160 E -120 E

- 8 0 E - 4 0 E

O E

-:.:n E

8 7 7 3 6 4 5 3 1 1 0 ?

-1 1 1 1 3

3 3 2 3

., 2 4 6 4 3 0

-1 -5 1 2 3 1 2 0 1 2 4 3 3 G 5 6 6 7 7 8 8 8

APOLLO DEVELOPMENT I VLF-EM RAIJ DATA

100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 100 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 2 3 0 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 200 s 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S 300 S

40 E 80 E 120 E 160 E 200 E 240 E 280 E 320 E 340 E 360 E 380 E 400 E

-1000 w -360 il’ -920 w - 8 6 0 I,J -840 W -800 h’ - 7 G 0 W -720 w -680 \I -6.10 i\‘ -500 i i -560 I.: ~ 5 2 0 i\’ -380 :i -440 I: -:00 Ii - 3 G O W -320 w -280 P I -240 w -200 W -lGO W -120 W -80 w -40 W 0 w

-1064 W -1040 W -1000 W -960 W -920 W -880 W -840 W -800 w -760 W -720 w -680 W -640 W -600 W -560 W -520 W

8 6 8 3 7 5 4 2 2 3

4 -11 -8 -6 -6 -4 -2 -2 -3 -2 -4 - 2 -7 -7

-10 - a -8 -G -9

-11 -6 -7 -7 -9 -6 2

-7 -8 -4 -3 -1

0 1 1 4 2 1 3

-1 -2 -2 -1

-


300 s 300 s 300 s 300 s 300 S 300 s 300 s 300 s 300 S 300 s 30'3 s 300 s 300 s ,100 s ~:00 s 400 s 3 0 0 s ,400 s .:00 s 400 s 400 s -400 s ,400 s 400 s 400 s ,100 s 400 s 400 s 400 s -100 s 3 0 0 s 400 s 3 0 0 s 400 s 400 S 4 0 0 s 400 s 400 s 400 s 4 0 0 s 4 0 0 s 500 S 500 S 500 S 500 S 500 S 500 S 5 0 0 S 500 S 5 0 0 S 500 S 5 0 0 S 5 0 0 S

-480 W - 4 4 0 w -400 w -360 W -320 w -280 W -240 w -200 w -160 W -120 W -80 W - 3 0 w

o w -1200 E -1160 E -1120 E -1080 E - 1 0 4 0 E -1000 E -9G0 E -920 E -880 E -840 E

-7GO E -720 E -680 E -640 E -600 E -560 W -520 w -480 W - 4 4 0 w -400 W -360 W -320 w -280 W -240 W -200 w -160 W -120 w

-1200 w -1160 W -1120 w -1080 W -1040 W -1000 E

-960 E -920 E -880 E -840 E -800 E -760 E

- a 0 0 E

2 -3 -5 -4 -5 -5 -4 1

- 4 -3 0 8

14 -1 0 10 8 5 2 0 -2 -2 -2 - G - 3 -9 -9 -8 - G -3 0

-1 0 2 5 3 1 2 1 1 0

-1 -2 -1 1 3 2

-1 -1 -3 -3 -6 -8

APOLLO DEVELOPMENT I VLF-EM !+A\$ DATA

5 0 0 S 5 0 0 S 500 S 500 S 500 S 500 S 500 S 500 S 500 S 500 S G O O S G O O S 600 S G O O S GOO s 600 s G O O s GOO S G O 0 S G O O S G O 0 s GO0 S GOO S GOO S G O O s G O O S 600 S G O O S G O O S G O O S G O O S 7 0 0 S 700 S 700 S 700 S 700 S 7 0 0 S 700 S 700 S 700 S 700 S 7 0 0 S 7 0 0 S 7 0 0 S 7 0 0 S 7 0 0 S 7 0 0 S 7 0 0 S 7 0 0 S 7 0 0 S 8 0 0 S 8 0 0 S 8 0 0 S

-720 E -680 E -G40 E - G O O E -560 E -520 E -480 E -440 E - 4 0 0 E -360 E

-1200 E -1160 E --1120 E -1060 E - i ' ) 4 0 E -1000 il -960 E -320 E -880 E -840 z -800 E -7G0 E -720 E -660 F -640 L - G O O E -560 E -520 E -480 E -4G0 E -420 E

-1200 E -1160 E -1120 E -1080 E -1040 E -1000 E

- 9 6 0 E -920 E -880 E -840 E -800 E -760 E -720 E - 6 8 0 E -640 E - G O O E -560 E -520 E -480 E

-1200 E -1160 E -1120 E

-10 -11 -7 -6 -2 0

-1 -1 0 1

-2 -2 -1 1 2

-1 -2 -2 - 2 -6 - 7 -3

-10 -5 , -7 -3 -1 0

-1 -2 -1 0 1 2 0 3

-1 -2 -1 -2 - 3 -7 - 7 -10 -9 - 3 -1 - 2

0 - 3 - 2

0

7 i

APOLLO DEVELOPMENT 1 VJ>,F-EM RAW D A T A

a o o s a o o s a 0 0 s a 0 0 s a 0 0 s a 0 0 s 800 s 800 s 800 S 800 S 800 S a 0 0 s 800 s 800 s

a o o s a o o s

180 rJ 180 N 180 N 180 N 180 N

180 N 180 N 130 N 180 N 180 N 180 N

120 N 120 N 120 N 120 N 120 N 120 N 120 N 120 N 120 N 120 N 120 N 120 N 120 N 120 N

-120 s -100 s

- 8 0 S - G O S -40 s -20 s

0 s 20 N 40 N

i a o N

i a o N

-1080 E -1040 E -1000 E

- 9 6 0 E -920 E -880 E - 8 4 0 E - 8 0 0 E - 7 6 0 E -720 E - 6 8 0 E - 6 4 0 E -600 E -560 E -520 E -480 E

-100 I\’ -80 t i -60 15 -40 bi - 2 0 w -10 w

O E 10 E 20 E 40 E G O E 80 E 100 E

-100 w -80 W -GO W -40 w -20 w -10 w 0 w 10 E 2 0 E 4 0 E G O E 80 E 100 E 120 E

o w o w o w o w o w o w o w o w o w

2 0 I

- :I - 3

-6 - 5 - 9 -5 - 5

-1 0

- 3

-I_

- 2 ~

- 7 ..

~

3

3

2 -

i 0 2

- 3 - 1

i J

-i 3 2 2

-1 2 1 2 2 0 1

15 2 0 1 2 1

- 3 -2 0 1 4 5 G

G O 60 100 120 1'10 160 1 8 0 200 ?. '2 0 240 2G0

APOLLO DEVELOPMENT I V L F - E M RAI? DATA

N o w 2 N o w 2 N 0 w 0 N 0 w 0 I: 0 I? 1 N !> PI 1 I.) 0 w 2 N 0 I S 2 1J 0 w 4 N o w 2 N 0 w 3 :J !J 0 GI 1

o w -2

\

.

\ \

'%

P 8 UY

8 i m

W z 8 UY

100 S( -

200 SE -

300 SE -

400 SE -

\ I I I I l l I I 1 I I I I I I I I t I 1 1 . 1 I

trench 1

' I \

r l 5 * 5

. s .7 . 8 +(I . 7

+ 3 + 2 7 + l .13 > , 18

15 + 1 4 * 1 2 * 1 0 * -.1 - 1300 SE

l S & * 8 * 1 5 r l l * I 3 - 1 2 -1400 SE

t l l l - 1000 f4E

X

\

'A

13 r 1 4

+Adi t yII w r u

Trench

x Outcrop

Winze

Law 1650s Old grid flag

Road ._ . .

A Swamp

f - - Creek

cz

\

\

\

\ . 00'- r 7 8

\ 100 SE -

200 SE -

300 SE -

460 SE -

' 8 0

( 0 vl 9-

trench "\

\ "n 8 8 9

0

c

m

+ 7 4 *63 * 5 4 * 5 5 +SO + 5 6

700 SE

800 SE

800 SE

1060 SE

I100 SE

1200 SE

1500 SE

1400 SE

.33 *a

.6% .n

* 6 5 r 7 3

.78 *61

\ '

681 +60 t 9 4 + 9 3 + 6 2 +51 *A r170

- 000 NE +36 -69 r k 8 r 6 b r37 +68 +36 XU2 r47 a62 *7a

~

*06 *70 r77 +35 *47 *32 . *45 653 r53' a41 171 -700 NE

3 5 0 NE

. l a a ,

.- \ I U

*60 *63 .83 .92 .so .79 . I02

I 1 I I I l / f , l

- 100 SE

- 200 SE

Sub Anomalous Threshold Value 188 pprn Background Value: 112 ppm

4 Adit

Trench

x Outcrop

61 Winze

Law 1650s Old arid flaa

8 5 m

I l l l l l - 1000 NE *OJ .a1 .0.1 .a1 1.0.1 r0.1 *0.1 .OJ +0.1

I I I I _I I I I I 1 I I I I I I I I 1000 N L t 0.1 *&I .OJ Yo2 .a1 02 + 0.1 Yo.2 +a! + 0.1 + 0.1

\ \ \ \ \ \ \ \ \ \ \ \ \ I I I I I I I \ I I I

I I \ I \ I \ I 1 I \ I \ I \

\ I I &/

. ".- ",. ".. . w 0.1

. 0.1 0.2

A

a\

900 NE - f0.2 r0.2 r0.1 .O.l r0.1 * 0.1 . 0.1 I0.1 *0.2 .a1

n

-650 NE

-550 NE

1 1 1 1 1 1

1.3 - 100 SE

,,I - 200 SE

\

!L!a!a Anomalous Threshold Value: .5 ppm

Sub Anomalous Threshold Value .3 ppm Background Volue: .2 ppm

J,2 .J - 1300 SE

A x 0

i OJ . o.M.2 *02\ 0.2 \ 0.2 I05 - 1400 SE

+ Adit

g Trench

x Outcrop

61 Winze

LBW 1650s Old grid

,& Camp

Road

a Swamp

t--- Creek

Scale 15000 0 100 200 300 400

metres

I APOLLO DEVELOPMENT INC. Y CLAIM GROUP

GEOCHEMICAL SURVEY ,

Ag P P m Date PLAN No. FIGURE Originator Orawn

LS Geo-Comp OCT.'90 Original

Revision . 82E/6 Revision N.T.S. ' 9

&-Canna -s SOOKOCHOFF CONSULTANTS INC.

\ s 0 0 v)

0 0

i m

w z 0 0 In

I I 1 I I I I I I I I I I I I 1 1 . 1 I I - 1000 I NE I I 1000 N L - 2 + s - 2 I r 3 .4 .3 .3 .4 .. .2 . E .2 .4 .s .2 r , .2 ., .2 .2 .2 .2

x \ trench

, .2 .3 .2 .2 ., ' .2 .2.3 .2 .2 .2 - 900 NE

-

* 2 .2 .2 r 2 .2 r 2 .2 x3 .2 .4 .Z, - aoo NE

900 NE - 900 NE -

800 NE -

700 NE -

600 NE-

560 NE-

40 NE-

.3

.5

.2

800 NE -

700 NE -

600 NE-

560 NE-

40 NE-

,

- 700 NE .2 + 2 .2 .2 .2 .2 .2 .2 . 2 ' .2 .2

-650 .2 * 2 .2 .2 .2 .2 + 2 ., .z .3 NE

. .- .2 .3 + 2 +3 1.3 <f13

. .ll.11.10 Q2 .9 -I

- 7 8

.3 .2 .2 .2 .2 .2 . .2

* 2 @ . s .s .P 1 7

-s I

r 2 .3' r 3 r 3 I .4

.3 3 ,, R

0 , o v) c

I I I ' 1 1 - 1 00'- r 3 r 2 ~ . 3 r 2 r 5 .Z r 3 * 2 t 2 r 2 .3 .2 r , .2 3 . 2 .3 .2 r 3 6 3 i t .s

, .

' : I I 1 I I I 1 I I I I .

. ' ' GATE -

100 SE -

.2 .3 + 2 .2 t 2 .2 .2 .3 . s * 2 .2 .2 .2 .2 + 2 + 5 2

* 4 4 5 r 3 *3 + 5 + 2 1 2 .2 * 2 - 2 4 2 i 6 * 2 a 4

n /* .

200 SE -

300 SE -

400 SE -

'A . L .2 .3 ., .2 .2 *3 - 00 NE

- 100 SE

- 200 SE

Anomalous Threshold Value: 10 pprn

Background Value: 5 ppm Sub Anomalous Threshold Value 7 ppm $ w 4 800 SE

900 SE

1600 SE

1100 SE

1200 SE

1500 SE

1400 SE

-..+ Adlt

Trench

x Outcrop

61 Winze

L 8 W 16505 Old grid

Camp

Road

Swamp

Creek

._ . - * . - .

0 400

I APOLLO DEVELOPMENT INC.

I Y CLAIM GROUP

GEOCH EM1 CAL SURVEY

A s PP- I I ,

4N No. FIGURE

J.T.S.

ANTS INC.

Originator Drawn Date P L Original I LS 1 Gee-Camp I OCT.'90

Rsvision b Revision a

SO 0 KO CH 0 F F CONS U LT

W z 0 0

0 0 In

i m 8 v)

0.2 0.2 + 0.2 f 0.21 * 0.2 * 0.3 + 0.2 + 02 0.2 + 0 f 0.2 + 0.2 - 1000 NE I f 0.2 0.2 + 0.3 + 0.2

I

900 NE - . 0.3 + 0. . 0.2 . 0.2

\ \ \ \ \ \ \ \ \ \ \ \ I \ I \ \ I \ \ I \ \ \ I \ \

\ \ \ 0

\ \

500 NE -

J

. 02 . .5 . 0.2 . 0.3 . 0.2 . 0.2 h.4 8 -550 NE

.OJ + 0.2 . a 3

.0.3 r02 .0.2 .0.2 0.2 . 0.2 .0.2

. 0.2 . 0.2 . 0.2 * 0.2 f 0.3

.0.2 X fO.2 .02 .0.2 a0.2

/ f0.3 . a 3 + 02 +J.2 / + 0

/ /

1

\ \ \ \

/' /

f 0.4 f O# + 0.2 f 0.4 * 0.3

/ t 0.2 + 0.3 . a2 + 0.4 + 0.2 + 0.2 + 0.2

\ I \ . I \ \ i I R 1 5 \ \ I 0 \ \ \ 8

I - I I

\ '\ \\

\

R

9 m

(y$-jQ 0

1.2 * 0. . .s . 1 0

> I I

).2 ,d fl' '' '\ . ,,/ f 0.2 + 0.2 * 02 f 0.2 * 0.2 + 0.2 + 0 1 + 0.2 0.2 + 0.2A.O.2 + 0.3 / i /

,,5 - 200 SE

. ' L 7 SE I I I 0 . . A

I 0 . 2 10.2 t0.s .0.2 * 0.3 t I ur 3.4

LEGEND Anomalous Threshold Value: 1 .O ppm

Sub Anomalous Threshold Value 0.7 pprn Background Value: 0.4 ppm

-.+ Adit

Trench

x Outcrop

ig Winze

D w 1650s Old grid flog

2i Camp

Road

* Swamp

+------ Creek

I * 0.2 . 0.2 0.2 . 0.2 . 0.2 . 0.2 L0.2 * 0.2 t 1000 SE -

1100 SE

1200 SE

1300 SE

1400 SE

Scale 1:5000 0 100 200 300 400

metres

I APOLLO DEVELOPMENT INC. - 1300 SE

Y CLAIM GROUP

GEOCHEMICAL SURVEY - 1400 SE

' I I I I CD pn- t 1 Oriainatorl Drawn I Date .. I " I I

Original LS Ceo-Camp OCT.'90 " - Revision

9 Revision m

SOOKOCHOFF CON m-camp * b m S

I Revision 1 Revision I

N.T.S. 82E/6

///// I

GRID A

J? .-

8 c -I m

W z

I 1000 N L

I

900 NE

800 NE-

700 NE - ,650 NE

- 5 5 0 NE

- 200 SE

600 NE -.

500 NE

400 NE-

i

\ 100 NE, ..

I l l

200 SE -1 \,

U I W 1650s

X /

,' & . +-

900 8ooj SE - \ I / t i L U L U b 1 L ~ U " 1 . I r r . - - - A S S E S S M E N T R E P O R T

---( nu,<

g Tmnch

x Outcrop

61

LBW 1650s

Wlnzs

Old grid flag

Camp

Road

Swamp

Creek

1000 SE - i I - 1100 SE i

I

cove 3- \ 1100 SE -

1200 SE -

1300 SE -

7 - 1200 SE - 1200 SE 0 100 200 300 400 -. . - .___

metres

- 1300 SE

- 14-00 SE

APOLLO DEVELOPMENT INC; , I Y CLAIM GROUP

GEOPHYSICAL SURVEY 1400 SE - I I ' I I

I 1 VLF-EM I FRASER FILTERED

1 /Origiitori Drown 1 Date I P U N No. I Oriainal Ceo-Comp OCT.'90

I SOOKOCHOFF CONSULTANTS INC.

apollo development inc. assessment report

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