A Geol Evaluation & Work Proposal for the Mckee

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4IJI1SW8807 2.14316 CASSON 010

A GEOLOGICAL EVALUATION AND WORK PROPOSAL FOR THE MCKEE COPPER COMPANY CLAIM GROUP THESSALON AREA, ONTARIO FOR N.S.A.I. HOLDINGS LTD.

January, 1991 by J.P. Mills SUMMARY

The geological investigation of the Mckee property was done on behalf of N.S.A.I. Holdings Ltd. of Wawa, Ontario. The property consists of eleven claims and is located in eastern Otter Township, Ontario(Fig. l and 2). Access is easily attained from highway 129. Milling facilities are available about 12 km(7.5 mi) to the south at the Gould Copper Mine site in Gould Township.

Quartz veining with copper sulfide mineralization occurs in several places on the property. However,work to date has been concentrated on the main showing. Previous work includes local geological and geophysical surveys, diamond drilling, test pitting and an adit driven for about 85 m(260 ft) along the veining. The drilling totaled about 373 m(1224 ft) plus two short holes. assays from veining in drill core gave a maximum value of 10.39 percent copper over 0.46 m(1.5 ft). Assaying from a test pit gave a value of 7.28 percent copper over 1.53 m(5 ft).

About 13 to 15 hundred tons of mineralized vein rock from drifting were stockpiled near the adit. Five hundred tons of the material was sent to Tribag Mines in 1973 for custom milling. According to Mckee Copper and Exploration Company officials(personal communication), the material assayed 4.5 percent copper. Recent sampling(1990) and assaying of the stockpiled material and several locations along the exposed veining shows copper values ranging to 22.6 percent.

Structure and mineralization features observed on the property are similar to those recorded from other parts of the region. Numerous mineralized vein showings exist in areas near the property. For example, the Fano showing in the western part of Otter Township and the Cheney and Gould showings(former mines) in Gould Township to the south.

To fully evaluate the economic potential of the property, a varied work program is strongly recommended. The program should include geological surveys and prospecting, geophysics, road construction, stripping, trenching and sampling, soil sampling and diamond drilling.

Toronto, Ontario v" ^ Respectfully submitted,

January, 1991

/J.P. Mills(Ph.D. Geology) QucL v H coJ2ufr-**-[ vH\x-"] ^Q^p-err-*^ 1 * l ~ TABLE OF CONTENTS

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INRODUCTION...... l

PROPERTY STATUS...... l

LOCATION AND ACCESS...... 4

TOPOGRAPHY AND VEGETATION...... 4

EXPLORATION HISTORY...... 6

REGIONAL GEOLOGY AND COPPER MINERALIZATION...... 7

LITHOLOGY AND STRUCTURE...... 7

COPPER MINERALIZATION AND QUARTZ VEINING...... 8

LOCAL AND PROPERTY GEOLOGY...... 11

SAMPLING...... 13

DISCUSSION...... 18

CONCLUSIONS AND RECOMMENDATIONS...... 19

WORK PROPOSAL...... 20

REFERENCES...... 22

STATEMENT OF QUALIFICATIONS...... 24

ILLUSTRATIONS

FIGURE l, Location Map...... 2

FIGURE 2 , C laim Map...... 3

FIGURE 3, Local Access Map...... 5

FIGURE 4, Regional Geology...... 10 FIGURE 5, Local Geology...... 15

FIGURE 6, Vein Exposure Locations Sketch Map...... 16

FIGURE 7, Main Showing Area Sketch Map...... 17

TABLE l, Copper Assay Values...... 13

APPENDIXES

APPENDIX l, Certificate of Analysis.

APPENDIX 2, Report on Investigations, Reuben Mckee Option, Otter Township, Ontario, 1968 By: Rio Tinto Canadian Exploration(Riocanex)

APPENDIX 3, Report on Geophysics and Drilling, Macpherson Option, 1971 By: Selco Exploration Co. Ltd.

APPENDIX 4, Mineral Deposit Inventory Record(MDI) with a brief description of the deposit and of the history of exploration and development: Mines Library, Geoscience Centre, Ontario Geological Survey, Toronto. INTRODUCTION

This evaluation of the Mckee Property, Otter Township, Ontario has been prepaired for N.S.A.I. Holdings Ltd. P.O. Box 2021, Wawa, Ontario POS 1KO. The report contents are based on the author©s experience in the area over the past two years, two days(October 17 and 18, 1990) of geological investigation and prospecting on the property, consultation with officials of the Mckee Copper and Exploration Co., a review of the assessment files at the Mines Library, Geoscience Centre, Ministry of Natural Resources, Toronto and a study of geological maps and reports on the region published by the Ontario Geological Survey and the Geological Survey of Canada.

PROPERTY STATUS

The Mckee Copper Company property consists of 10 crown claims and one leased claim. The claims are located in the east-central region of Otter Township(Fig. 2) in the Sault Ste. Marie Mining Division of Algoma District(Ministry of Natural Resources map: Index to Land Disposition Plan G-3309, Otter Township, May 1990 issue). The claim numbers are as follows:

1. Leased claim - SSM 282633 2. Crown claim - SSM 609010 3. Crown claim - SSM 609011 4. Crown claim - SSM 609012 5. Crown claim - SSM 609013 6. Crown claim - SSM 699924 7. Crown claim - SSM 699925 8. Crown claim - SSM 699926 9. Crown claim - SSM 699927 10. Crown claim - SSM 699928 11. Crown claim - SSM 699929

The claims are in good standing under the Mckee Copper Exploration Company of Thessalon, Ontario. N.S.A.I. Holdings of Wawa, Ontario has a ten year option on the claims beginning in 1990. 75"

FIGURE 1, Location Map. A general outline of Ontario showing the McKee property Location.

75" ^ FIGURE 2, Claim map showing ^" ©vT the 10 Crown claims and 1 "~^\\ leased claim. t "3 LOCATION AND ACCESS

The property(Fig. 2) is located in the east-central part of Otter Township, Ontario. The region is in the Sault Ste. Marie mining Division, Algoma District. The N.T.S. number is 41J/11SW. The coordinates of the main showing area are about Lat: 46 34© 02" and long: 83 27© 56"(see Appendix 4). The claim group can be reached by traveling north from Thessalon, Ontario for about 40 km(25 mi) on highway 129 to the Snowshoe Creek crossing(see Fig. 3). Immediately north of the crossing, a gravel road leads off to the west and the property is about 6.8 km(4.2 mi) northwest across the Mississagi River. The river is about 100 m(328 ft) to 200 m(656 ft) wide and requires an amphibious vehicle or a canoe for safe crossing.

The terrain along the gravel road is mainly well drained sand and gravel and forms a good road bed. Aggregate for road repair and construction could easily be taken from several places along the route. Bridging the river for general traffic and transport is quite feasible. Previously, Mckee Copper and Exploration Co. officials(personal communication) had recommended constructing a baily bridge upstream from the site generally used now.

Milling facilities exist in the area. The mill at the Gould Copper Mine site, which closed operations in 1986, is essentially intact and could be made operational if required(personal communication with N.S.A.I. Holdings personnel). The mill is about 12 km(7.5 mi) south of the Mckee property and about 1.5 km(0.93 mi) west of highway 129 in Gould Township. The mill is capable of processing about 200 tons of ore per day. Smelter facilities exist at INCO in Sudbury, Ontario.

TOPOGRAPHY AND VEGETATION

The property is part of the glaciated southern Shield region. Maximum relief is about 135 m(443 ft). The lower area is to the east where the south flowing Mississagi River serves as the main drainage for the region(see Fig. 3). Local drainage is eastward along generally straight valleys that are cliff faced in places with angular scree covered slopes in some locations.

The regolith is mainly well drained poorly sorted sandy gravel. Vegetation is thick in places with large trees and clusters of underbrush. The larger tree types include maple, birch, poplar, pine and spruce. The underbrush is mainly willow and maple.

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The property was staked in 1967 by Reuben Mckee of Thessalon, Ontario. Eight claims were staked in Otter Township and three adjoining claims in Casson Township immediately to the east.

Trenching was done and in 1968 an option was taken on the claims by Rio Tinto Canadian Exploration Limited(Riocanex). Riocanex did some geological investigations and had ground level magnetometer and electromagnetic surveys done. Company personnel completed a report in Septmber, 1968(see Appendix 2) in which an assay value of 7.28 percent copper over 1.53 m(5 ft) of mineralized veining was indicated. The vein thickness was estimated to be 1.53 m(5 ft) to 2.14 m(7 ft) based on pits. A vein strike length of 153 m(500 ft) to 183 m(600 ft) was indicated based on interpretation of the geophysics. Diamond drilling was recommended and two holes were drilled. The original drill core logs are not available. However, reporting by Selco Exploration in 1971(see Appendix 3) states that an intersection in the first of the two holes(H-l and H-2) showed an assay value of 2.7 percent copper over a true thickness of seven feet. Results from hole H-2 were not given.

In the fall of 1970, Selco Exploration took an option on the property which was called the Macpherson Option(see Appendix 3) although the property had been transfered to Mckee Copper Incorporated. Ground level magnetometer and electromagnetic surveys were done and four holes were drilled totaling 373 m(1224 ft) intersecting mineralized veining in some intervals(see Appendix 3, drill logs). Copper assay values ranged to a maximum of 10.39 percent over 0.46 m(1.5 ft).

In 1973, Mr. W. Doughty of Sault Ste. Marie, Ontario, representing Otter Mining and Exploration, drove and adit for about 85 m(280 ft) along the veining at the main showing. According to Mckee Company officials(personal communication), a 50 ton bulk sample was taken and assayed by Noranda and Copper Corporation. Noranda reported 12 percent copper and Copper Corporation 22 percent. Ore from the adit was stockpiled near the portal(Fig.7^). A 500 ton bulk sample of the stockpile was sent to Tribag Mines for custom mill ing(Appendix 4) and according to Mckee company officials(personal communication) the material assayed 4.5 percent copper.

Operations were stopped in 1974. However, the claims were retained by Mckee Copper Incorporated. REGIONAL GEOLOGY AND COPPER MINERALIZATION

The property is in the east-west trending contact zone between Early Precambrian felsic intrusive rocks of the Superior Province to the north and unconformably overlying Huronian sedimentary rocks of the Southern Province(Fig. 4; Stockwell, 1982, Fig. 20)to the south. The felsic intrusive and sedimentary rocks are cut by Early and Middle-to-Late Precambrian intermediate-to- mafic intrusive rocks(Ontario Geological Survey Map 2419). the Middle-to-Late Precambrian intrusive rocks include the widespread Nipissing Diabase dikes. Quartz veining occurs widely, commonly in association with Nipissing Diabase exposures, and many vein sections contain copper sulfide mineralization of economic significance.

LITHOLOGY AND STRUCTURE

The Early Precambrian intrusive rocks form a highly folded and faulted complex consisting of layered gneiss and massive granite (Frarey, 1977, p. 15-16). The gneiss is pink to gray and ranges in composition from granite to granodiorite and diorite. The massive granite is pink to red and shows variations to syenite and quartz monzonite.

The Huronian sedimentary rocks are part of the Penokean Fold Belt(Stockwell, 1982 Fig. 20) of the Southern Province. Exposures consist mainly of clastic rocks of the Huronian Cobalt Group in which the Gowganda Formation is the upper unit(Ontario Geological Survey Map 2419). The Gowganda Formation, consisting of conglomerates, sandstones and mudstones, is widespread and includes the sedimentary rocks in the property area(Chandler, 1976).

Lineaments occur widely in the region(Ontario Geological Survey Map 2419). Lineament trends are mainly northwest and northeast. Some lineaments represent faults of regional extent, such as the Flack Lake and Little White River faults. Thrust faulting, striking generally west to northwest, is prominent in several locations south and southwest of the property area(Frarey, 1977, p. 65).

Folding in the sedimentary rocks occurs mainly along north- northwest striking axes. In some places, axes trend northeast(Fig. 3). The folds are mainly broad open structures in contrast to the more complexly folded Early Precambrian intrusive 8 rocks. The Quirke Lake Syncline( Ontario Geological Survey Map 2419) is a prominent feature in the eastern region. The syncline opens westward and trends generally towards the Otter Township area.

COPPER MINERALIZATION AND QUARTZ VEINING

The copper sulfide mineralization occurs in various settings throughout the region(0ntario Geological Survey Map 2419; Pearson, 1980). Quartz vein deposits are the most extensive(Frarey, 1977, p. 71) and several varieties occur showing different ranges of mineralization. However, the quartz- carbonate-chalcopyrite-pyrite hematite type(qz-cb-cp-hm) is the most widespread, forming about 70 percent of the mineralized veining occurrences(Pearson, 1980, p. 236). The Bruce Mines site is the best known example of the qz-cb-cp-hm variety. Knight(1915), Collins(1925) and Moore(1929) describe several sites of past economic activity including showings in Gould, McMahon, Morin and Otter Townships.

The mineralized veining is commonly associated with Nipissing Diabase units. However, exposures of the diabase does not necessarily denote veining in the immediate vicinity(Pearson, 1980, p. 271). The qz-cb-cp-hm vein type is most commonly hosted by rocks of the Gowganda Formation, Nipissing Diabase, Early Precambrian rocks and, to a lesser extent, the Mississauga Formation. Both pre-Gowganda and post-Gowganda Formation units of the Huronian, with the exception of the Mississauga Formation, host relatively few qz-cb-cp-hm vein type(Pearson, 1980, p. 241, 242).

The veining strikes generally eastwest with some variation. Individual veins range from a few millimeters to over four meters in width. Single veins tend to pinch out within a few score meters. However, vein zones consisting of two or more units may be traceable for several kilometers and tend to follow faults or shear zones(Frarey, 1977, p. 71). The pinch and swell structure is well documented at Blind River where the veining pinches out for several hundred meters in places between mineralized sections(Knight, 1915, p. 233). Contacts of veining with wall rock are sharp and irregular and show little or no alteration (moore, 1929, p. 9). Wall rock inclusions are angular and, in many places, are elongate units generally paralleling the contact(personal observations). Quartz/the main component of the veining, is light gray to white except where red and specular hematite has given the rock a red to purplish coloring. In places, the veining is vuggy with well formed quartz crystals lining the vugs. The sulfide, mainly chalcopyrite, occurs as irregular disseminations randomly scattered in the vein rock(Frarey, 1977, p. 71) and ranges in size from small flecks to blebs two to three centimeters across. The sulfide is massive in places. Knight(1915, p. 235) noted a massive chalcopyrite unit about 30 cm(0.98 ft) wide at the Cheney showing in Gould Township. The chalcopyrite is accompanied by bornite, pyrite and malachite in some locations and less commonly by chalcocite, galena, sphalerite, pitchblende, smalite and tetrahedrite(Frarey, 1977, p. 71).

Several earlier workers attributed the mineralization and veining to hydrothermal solutions derived from gabbroic magma(Pearson, 1980, p. 272). Knight(1915), Collins(1925) and Moore(1929) noted the close association of mineralized veining and Nipissing Diabase and stipulated a genetic relationship with the veining being a later phase of the magma differentiation. According to Coll i os(1925, p. 128), diabase trending through central Otter Township has pegmatitic phases that have minor copper mineralization in some instances. A genetic relationship of the veining and diabase is further suggested by field relations in the Quirke Lake Syncline. The syncline is cored with Gowganda Formation rocks(0ntario Geological Survey Map 2419) and an increasing amount of veining westward coincides with more Nipissing Diabase(Pearson, 1980, p. 238, 244). boundary

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LOCAL AND PROPERTY GEOLOGY

The claim group straddles the contact zone between Early Precambrian massive granite to the south and an eastwest trending belt of Nipissing Diabase intrusive rocks to the north(Fig. 5; Chandler, 1976). Outliers of Gowganda Formation clastic rocks overlay the massive granite in some places. (Chandler, 1976).

Mineralized quartz veining exists in several locations on the property(Fig. 6). At the Main showing in claim number SSM 282633, copper assay values from samples taken in 1990 range to 22.6 percent(see Table l, samples: 4714 - 4720, 4722, 4723).

The local host rocks consist of diabase, granite and paraconglomerate. The diabase is dark gray, fine to medium grained, massive and generally slightly magnetic. The granite is red massive, coarse grained, and contains 20 to 40 percent quartz, the dark mineral content is generally less than two percent. The paraconglomerate is massive with a dark grayish green mudstone matrix. Clasts are mainly red granite fragments which form generally about five to 25 percent of the rock.

The main showing is in the west end of an eastward draining valley(Fig. 2). The veining, on a general strike of 090 to 100 degrees, cuts across the diabase and granite which comprise the host rock locally. Veining is most extensively exposed at the adit site(Fig. 7). West of the adit, about 150 m(492 ft) along strike, mineralized veining is exposed in several places. About 416 m(1365 ft) to the east of the adit, mineralized quartz veining is exposed in a creek bed.

At the adit site, the veining is 1.2 m(3.5 ft) to 1.5 m(5.0 ft) wide and dips 80 to 85 degrees north, wall rock contacts are sharp and lack alteration. The veining is highly sheared and generally parallel to or subparallel to wall rock contacts and is brecciated in places. The veining consists of interlensing quartz, carbonate and host rock units with widely occurring grains, clots and lenses of chalcopyrite. Limonite and malachite alteration are widespread.

The stockpiled material taken from the adit consists mainly of pieces showing various amounts of sulfide mineralization. The 12 chalcopyrite content ranges to about 50 percent occurring as random grains, irregular clots and lenses. Bluish coloring in some specimens suggests bornite or altered chalcopyrite. Red and specular hematite, limonite and malachite are widespread. The carbonate occurs as light brown lenses, veins and clots of generally well formed, fine to coarse grained chrystals. Weathered carbonate surfaces are more dark brown. The quartz is light gray to whitish and translucent and is generally highly fractured.

The two pits located a few meters east of the adit portal(Fig. 7) show weathered veining about 1.5 m( 5 ft) wide and hosted in massive red granite. The contacts dip vertically to 80 degrees north and are sharp with alteration lacking. Limonite and malachite are widespread and the vein rock is pitted and friable in places. The main veining consists of quartz and carbonate lenses with irregular, massive clots of chalcopyrite with minor pyrite. The sulfide is generally pervasive ranging from random grains to about 80 percent. Random bluish coloring occurs in places suggesting bornite or altered chalcopyrite.

About 416 m(1365 ft) along strike to the east of the adit, quartz veining hosted in paraconglomerate is exposed in a creek bed. The veining shows random traces of chalcopyrite(Table l, sample 4724) with limonite and hematite. Three old pits, now filled in, are located a few meters southwest of the of the exposure.

West of the adit site, about 150 m(492 ft) along strike, mineralized veining 0.6m(2 ft.) to 0.9 m(3 ft) wide occurs as several exposures(Fig. 7) along a strike length of about 34 m(112 ft). The veining consists of interlensing quartz and carbonate with fractured paraconglomerate units and is hosted in granite and paraconglomerate. The veining is moderately magnetic in places. Mineralization(Table l, sample 4721) occurs as minor, random chalcopyrite clots and grains and limonite is widespread. Offshoots from the main veining occur in some places and trend in various directions. Exposures near the veining show minor quartz veins paralleling the main zone.

Mineralized quartz veining is exposed in claim number SSM 699929 southwest of the adit area. The veining, about 1.2 m(3.9 ft) wide, is exposed in a wooded area on the north shoulder of the eastwest trending valley and about 30 m(100 ft) south of the bush road. The veining is highly fractured and sheared and shows 13 widespread malachite alteration with minor, random chalcopyrite. Assaying(Table l, sample: 4713) shows copper values of 2.01 percent over 1.2m. According to Mckee Company of ficials(personal communication), quartz veining is also exposed in places north of this location towards the pond(Fig. 2 and 6).

SAMPLING

A total of twelve samples were taken at several vein locations and from mineralized material stockpiled during previous(1973) work at the main showing area. Assay results, sample type, claim number and a brief description are given in Table l following.

Table l

Sample no. % Cu Claim no.

(1) 4713 2.01 699929

A chip sample taken across a 1.2 m(3.9 ft) wide, highly sheared zone containing quartz stringers with malachite and minor chalcopyrite.

(2) 4714 0.23 282633

A chip sample taken across a 0.9 m(3 ft) wide, highly weathered vein zone consisting of carbonate with specular hematite.

(3) 4715 16.32 282633

A chip sample across 0.5 m(1.6 ft) of highly mineralized vein material in an old trench(No. 1), prominent malachite and chalcopyrite.

(4) 4716 0.57 282633

A chip sample across 0.5 m(1.6 ft) of highly weathered quartz- carbonate vein material in an old trench(No. 1).

(5) 4717 22.64 282633 14

A chip sample across 0.7 m(2.3 ft) of vein material(trench No. 2) showing strong chalcopyrite mineralization.

(6) 4718 10.92 282633

A chip sample across 0.7 m(2.3 ft) of highly mineralized vein material at the west end of the zone, between the adit portal and the rise, where a 50 ton bulk sample was taken in 1973 for analysis by Copper Corporation and Noranda.

(7) 4719 10.30 282633

A grab sample from the muck pile beside the rise.

(8) 4720 0.12 609013

A chip sample across l m(3.3 ft) of highly weathered quartz- carbonate veining showing some specular hematite and chalcopyrite.

(9) 4721 1.40 282633

A grab sample from the muck pile beside an old trench west of the road, about 150 m(492 ft west of the adit site.

(10) 4722 13.87 282633

A hand-cobbed grab sample from stockpiled ore from the adit

(11) 4723 2.67 282633

A random grab sample from the stockpile as in 10. above.

(12) 4724 0.08 699925

A grab sample of quartz-carbonate vein material, showing minor specular hematite and traces of chalcopyrite, taken from the muck pile at an old pit near exposed veining in the creek bed about 416 m(1365 ft) east of the adit site. un-

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mineralized mineralized

6, 6,

shown shown

some some FIGURE FIGURE 18

DISCUSSION Quartz veining with Chalcopyrite mineralization is exposed at several places on the property. In addition, mineralized veining occurs in neighboring areas such as the Fano occurrence(shklanka, 1969; chandler, 1976) in western Otter Township, in Morin and McMahon Townships(shklanka, 1969) farther west and at the Cheney and Gould copper showings(former mines) in Gould Township to the south. The existence of the numerous exposures in the area tends to support Pearson©s view(Pearson, 1980) that quartz veining and diabase tend to increase in amount westward along the axial trend of the Quirke Syncline axis(Fig. 4).

Vein features including mineralogy, the general eastwest strike, variation in width along strike and the close association with diabase coincides with features occurring in other quartz vein zones in the region(see regional geology such as the Cheney and Gould mine sites and Bruce Mines(Knight, 1915, p. 233).

To date work on the Mckee property has been concentrated on the most extensive exposure site located in claim number SSM 282633. Veining, generallly about 0. 9m(3 ft) to 1.5 m(5 ft) wide, has been exposed over a strike length of about 85 m(280 ft). Assay values range from traces to 22.6 percent copper have been obtained. However, several other exposures of quartz and mineralized quartz veining exist on the property and have had relatively little investigation. A similar situation existed at the Gould Copper Mine site until recent work disclosed more extensive veining than was previously known. Assay results from these locations show copper values of economic significance.

Selco Exploration(see Appendix 3) concluded that the response to geophysical signals was from the diabase(called andesite and volcanic rock in their report) which is moderately magnetic. The mineralized veining was considered to lack any response to the signals. This conclusion coincides with mapping results(see maps in Appendix 2) where the trend of the geophysical anomaly parallels the trend of diabase exposures and not the veining trend. However, magnetic sections of mineralized veining have been noted(see local and property geology) and these sections are not hosted in diabase. Consequently, geophysics may help to locate some mineralized vein zones as well as diabase units.

In view of these several factors, more widespread and varied work on the Mckee property is definitely warranted. 19

CONCLUSIONS AND RECOMMENDATIONS

Significant economic potential for the property is strongly suggested by several factors:

(1) At the main exposure, where veining has been exposed for about 85 m{280 ft), vein width ranges from about 0.9 m(3 ft) to 1.5 m(5 ft) and assay values obtained to date range to a maximun of 22.6 percent copper.

(2) The property is located near several other showings of copper sulfide mineralization of economic significance including the Cheney and Gould copper mining sites.

(3) Mineralized veining is exposed along strike from the zone mentioned in (1) above and in other parts of the claim group.

(4) The property is well situated in respect to access and milling facilities which exist at the Gould Copper Mine site about 12 km(7.5 mi) to the south in Gould Township.

In view of the results to date a work program is recommended to fully evaluate the economic potential of the propery. The program should include line cutting, geological mapping and prospecting, geophysics, road construction, soil sampling, stripping, trenching and sampling, and diamond drilling. 20

WORK PROPOSAL

A work program designed to fully evaluate the Mckee Copper property should involve the following activities:

1. Line cutting. Estimate: 40 km at S500.00/kilometer...... S20,000.00 To include a baseline, tielines, crosslines at 50 m intervals and surveying of the baseline and tielines.

2. Prospecting. Estimate: Two men for 30 days at S150.00/day.....^10,000.00 To include a thorough search for mineralized bedrock exposure, grubhoeing in promising areas and stripping locally to enlarge on exposed surfaces, sampling and assaying.

3. Geological mapping. Estimate: One geologist, S 25Q. 00/day, 2 km/day....S20,000.00 To include complete mapping of the grid at 1:2,500 scale, detailed mapping of stripped zones and trenches at 1:200 scale.

4. Geophysical surveys. Estimate:...... S30,000.00 To include ground magnetometer and VLF surveys over the entire grid, close spacing in some areas based on bedrock exposure interpretations, compilations and report writing.

5. Geochemical surveys. Estimate: About 1500 samples at S 2Q .00/sample.....S20.000.00 To include soil sampling in selected areas based on bedrock exposure interpretations, topography and geophysical survey interpretations; assaying, compilations and report writing.

6. Road construction. Estimate: including backhoe work,...... S25,000.00 To include expanding and opening up of old roads and making new roads. 21

7. Clearing and stripping of veined zones. Estimate: including backhoe with operator...... S75,000.00 To include clearing and stripping of bedrock along the strike trend of known mineralized exposures and of new discoveries.

8. Trenching and Sampling. Estimate: using a 4 to 6 man crew...... 550,000.00 To include drilling, blasting, channel sampling and assaying.

9. Adit mapping and sampling. Estimate:...... S25,000.00 To include detailed mapping at 1:200 scale, surveying, possible ground support work in places and compilations.

10. Diamond drilling. Estimate: 10,000 ft at S25.00/ft...... S250,000 .00 To include core logging, sampling and assaying, core splitting, core boxes, supervision, compilations and report writing

11. Supervision. Estimate:...... 540,000.00 To include project supervision, surface surveying and equipment rentals.

12. Contingencies. Estimate:...... 525,000.00

TOTAL:...... 5600,000.00 II 22 l REFERENCES l Chandler, F.W., 1967; Geology of the Saunders Lake Area, District of Algoma: Geoscience Report 155: Ontario Division of Mines, Ontario Ministry of Natural Resources; Toronto; 46 p., 5 i fig., 3 tables, l map. Collins, W.H., 1925; North Shore of Lake Huron: Memoir 143, No. l 124 Geology Series: Canada Department of Mines, Geological Survey of Canada; Ottawa; 160 p., 9 figures, 27 plates, 2 l maps, References. Frarey, M.J., 1977; Geology of the Huronian Belt Between Sault Ste. Marie and Blind River Ontario, Geological Survey of l Resources Canada; Canada Memoir 383: Energy, Mines and l Ottawa, Ontario. 87p., 29 fig., 11 tables, 4 maps. Knight, C.W., 1915; The North Shore of Lake Huron; Summary Report of Geology and Mineral Industry, Annual Report Vol. 24, Part n 1: Ontario Bureau of Mines, Ontario Ministry of Natural Resources, Toronto; p. 216-242, 12 figures, references.

i^* Moore, E.S., 1929; Ore Deposits Near the North Shore of Lake Huron: Ontario Department of Mines, Volume 38, Part 7, Pages H 1-51; Ontario Ministry of Natural Resources; Toronto, Ontario.

Ontario Geological Survey, 1976; Map 2419; Sault Ste. Marie- Elliot Lake Geological Compilation Series; Scale: 1:253,440 or l inch to 4 miles: Ontario Ministry of Natural Resources, Toronto, Ontario.

Ontario Geological Survey, 1991; Mineral Deposits Files, Geoscience Information Centre, Archives Building: Ontario Minstry of Natural Resources, Toronto; The following Reports under Otter Township. (1) Report on Investigations, Reuben Mckee Option,Otter Township, Ontario, N.T.S. 41-J-ll/SW. H (2) Selco Exploration Company Limited, Macpherson Option, Final Report on Geophysics and Drilling. (3) Mineral Deposit Inventory Record for the deposit called Mckee; located in Otter Township, Algoma District. m B 23 l Ontario Ministry of Natural Resources, 1990; Index to Land Distribution Map, Plan G-3309, Otter Township, Ontario, l 1:20,000 scale, July l, 1990 issue: Algoma Land Titles Registry Division, Sault Ste. Marie, Ontario; Ontario H Ministry of Natural Resources, Toronto, Ontario. Pearson, W.N., 1980; Copper Metallogeny, North Shore Region oflake Huron, Ontario: Ph.D. Dissertation, Queen©s l University; Kingston, Ontario; 403 p., 117 fig., 24 tables, 7 appendixes, references. l Shklanka, R.,(Ed.)/ 1969; Copper, Nickel, Lead, Zinc Deposits of Ontario: Mineral Resources Circular No. 12(MRC12): Ontario l Department of Mines, Ontario Ministry of Natural Resources, Toronto; 394 p.

l Stockwell, C.H., 1982; Structural Provinces and Subprovinces of the Canadian Shield and of Adjacent Platforms and Mobile Belts of Canada: Part l, Paper 80-19, Figure 20: Geological n Survey of Canada, Department of Energy Mines and Resources, Ottawa.

Wakomata Lake Map Sheet, 1976; 41-J/ll, Edition 2, Algoma District, Scale 1:50,000: Surveys and Mapping Branch, Department of Energy Mines and Resources, Ottawa, Ontario. l l l m m 24

STATEMENT OF QUALIFICATIONS

I, John Peter Mills, of Toronto, Ontario, do cirtify that:

(1) I am a self employed consulting geologist with present address at: l University Ave., Suite 502, Toronto, Ontario M5J 2P1.

(2) I Have a Ph.D. degree in geology from the University of Kansas, Lawrence, Kansas, U.S.A.

(3) I have been practicing geology continuously since 1960.

(4) I am a fellow of the Geological Association of Canada.

(5) I have not received, nor do I expect to receive any interest, direct or indirect in the property of Mckee Copper and Exploration or in any affiliate of the company.

(6) Permission is hereby granted to N.S.A.I. Holdings Ltd. for the use of this report in a prospectus or in a statement of fact relating to the raising of funds.

Respectfully Submitted,

J. P. Mills (Ph.D. geology)

502 - l University Ave. Toronto, Ontario M5J 2P1

January, 1991 B l l H l l l l APPENDIX l

Certificate of Analysis

V m , ^ J^.JI.^AJE-. r^-B Vtf MVVM '

& , .. "JF ' -: P.O. Box 1998 - Wawa. Ontario POS 1KQ - 705-856-4^-3 ^— ^- . . -. 1 27 Mission Road Fsx - 705-856-2902 I wo nQ^Ti CERTIFICATE OF ANALYSIS ^ uy^ fj 1 No. 6151 DATE: November 7, 1990 CLIENT: NSAI HOLDINGS LID.

Cu Au Ag SAMPLE Cu r. •OtSm SS UT^b "DT3IB

20140 2.01 . 4713 2260 0.23 1 4714 163200 16.32 4715 0.57 4716 5720 1 226400 22.64 14 2.7 4717 n 109200 10.92 4718 103000 10.30 B 4719 1230 0.12 ' 4720 13930 1.40 1 4721 138700 13.87 1 4722 4722 check no ehrg 140300 14. C3

^^t 26680 2.67 840 0.08 l 4724

1 1 1 1

Samples, Pulps and rejects discarded after two maaths. II l l H l APPENDIX 2 l Report on Investigations,

Reuben Mckee Option,

^ Otter Township, Ontario, 1968 l n Rio Tinto Canadian Exploration(Riocanex) i i i m m m m o l l l l r

l McKEE OPTION REUBEN l OTTER TOWNSHIP, ONTARIO l N.T.S. l |R. A. Benkis H. Bec"kmann i M REPORT ON INVESTIGATIONS REUBEN McKEE OPTION OTTER TOWNSHIP, ONTARIO N.T.S. 41-J-ll

TABLE OF CONTENTS PAGE NUMBER

SUMMARY

PART I - GEOLOGY AND GENERAL©

...... ; ; One. . INTRODUCTION , * One PROPERTY ......

...... Two HISTORY AND PREVIOUS WORK . . . © . Three - WORK BY RIOCANEX .,...... ," Four REFERENCES ...... Four GEOLOGY © . . . , ...... Seven CONCLUSIONS ...... © ...... Seven RECOMMENDATIONS . . . . ^...... - PART II - GEOPHYSICAL SURVEYS One SUMMARY ...... One CONCLUSIONS ...... One RECOMMENDATIONS ...... One DISCUSSION OF GEOPHYSICAL RESULTS . . . Two PERSONNEL ...... APPENDIX . MAPS IN POCKET l" ^SO© G-2474 GEOLOGY OF McKEE SHOWING (D.. SPRAGUE) l" ^ 100© G-326l GEOLOGICAL MAP (R. BENKIS) - l" ** 1 00 D M-3262 MAGNETIC S E.M. PROFILES (H. BECKMANN) REPORT ON INVESTIGATIONS

REUBEN McKEE OPTION

OTTER TOWNSHIP, ONTARIP

N.T.S. 41-J-ll

SUMMARY . © .- ;;

© . t the last week of September, a team comprised During . © i a copper of H.©Beckmann, D. Sexsmith and R. Benkis investigated l . . occurrence in Otter Township, Ontario. occurs Apparently heavy chalcopyrite mineralization into Archaean in a quartz vein within a basic dike intruded copper content as high granite. Chemical assays have indicated a content in the vein as 7 . 2856 Cu; visual estimates of the copper average width of are between 20?6 to 40^ chalcopyrite. The true have shown it to the mineralized vein is unknown, but test pits of the magnetometer and be between 5 and.7 feet wide. The results of 500 to 600 feet E.M. surveys suggests a possible strike length *. for the mineralized vein. © recommended, To test the structure, diamond drilling is REPORT ON INVESTIGATIONS

REUBEN McKEE OPTION

OTTER TOWNSHIP, ONTARIO

N.T.S. 41-J-ll

INTRODUCTION

Based on a recommendation by Doug Sprague, Riocanex has agreed to option a copper prospect in Otter Township, Ontario. t . - This report describes the exploration of the prospect that has-been

* ** completed to date.

PROPERTY .

The owner of the claims is Reuben McKee, c/o Demers Bay

Inn, R. R. 3, Thessalon, Ontario. The eight claims which the company has agreed to option are contiguous and occupy Lot l, Concession III in Otter Township, Sault Ste. Marie Mining Division. The numbers and the respective locations of the claims are:

SSM 89471 .Lot l, Concession III SSM 89472 M n II II n© II II SSM 89473 i SSM 89474 i n II It n II II SSM 89475 n SSM 89476 M II II II SSM 89477 II II II II SSM 89478 ti n II M

Theoretically the eastern boundary of the claims© block should lie at the boundary between Otter Township to the west, and

Township 188 to the east. However, there is some doubt whether the claim lines have baen "correctly located; the township originally was surveyed many years ago, and since then the survey lines have become obliterated by the bush.

The claims were staked last fall, and were recorded on October 3, 1967. By paying the prescribed fee to the Ontario Depart ment of Mines, Doug Sprague last month arranged an extension till April 30, 1969 to file the necessary assessment work against the claims; at the same time 40 days of work (trenching, etc.) were filed i against four of the eight claims.

To have protection eastwards, McKee has staked three additional claims in the adjoining Township 188; the claims join©.the© three * ** "" northern claims in the original block of eight. During our visit to the property these newly staked claims had not yet * been tagged.

The showing is located on claim SSM 89475; geographically it is at 830 28© west longitude, 46 O 34© north latitude, NTS 41-J-ll. The claims are near the Thessalon-Chapleau Highway (Provincial Highway 129), approximately 30 miles north of Thessalon. To reach the showing one must cross the Mississagi River, and walk approximately one mile westwards to the property. Along bush roads from north and south, vehicles can be driven to within four miles of the showing.

HISTORY AND PREVIOUS WORK

Doug Sprague first examined the showing in October of 1967. A sample across the best ©looking part of the vein assayed 7.28^ Cu, arid it was recommended to McKee that more of the structure be exposed by additional , trenching. During August of this year Sprague made a second visit to the property to examine some^ new pits opened by McKee. - - ...... - - The pits are narrow slits dug in 2 to 4 feet, of sandy rains had overburden.. At the time of our visit to the claims heavy and very little caused the pits to become partially filled with mud/ the circum of the mineralized rock could be seen in place. Under showing as stances, J will quote Doug Sprague©s description of the seen during his August visit: "Since then two more locations of the vein or structure were made by test pitting. The © © " . first of these (Pit 2), located about 40 © SW ©-. of Pit l shows heavy cpy estimated to avera-ge ; © between 205^ and 3C^ across a true width of at \ least 1*2 feet, with the south wall not exposed. . ; Another mineralized area was located 70 feet t west of Pit 2 and this exposed 3^ Cpy/1.5© and ! * 40^ Cpy/1.9© on the east wall and 20?4 Cpy/3.5© l- plus heavy gossan and 40^ Cpy/0.4 1 for follow ing 2 feet. North wall is heavily oxidized, and is altered dike, south wall appears to be granite. 2lO feet west of this pit there is a shallow trench exposing .granite which has "3" of heavy rust on top - supposedly from the nearby vein? This is upstream from the above mentioned pits.

Due to the heavy overburden encountered in the pits and elsewhere, it is obvious that further trenching by this method is not feasible, and that other methods should be employed." .

WORK BY RIOCANEX

grid consists of a 1,000-foot long baseline, situated

RIO TlriTO CANADIAN EXPLORATION LIMITED at 100O , and five 800-foot long cross lines at 200-foot intervals. Three of the cross lines run N-S, while the eastern two lines are at right angles to the baseline, i.e. at 010 . © Geological mapping of the picket line grid, and along a north-south claim line. - 3. Magnetometer and vertical loop E.M. surveys over the picket line grid. © - The packet line grid has * © * © - been tied-in .to two claim" posts. . - REFERENCES

Echo-Lake Geological Survey of l" = l mile. Canada Map 23-1959; Blind River-Elliot Lake Sheet Mines preliminary Ontario Department of geological nfap l" - 2 miles. No. P. 304, 1967;© Sault Ste. Marie Sheet Ontario preliminary Department of Mines geological map No. P.303, 1965; l" ©s 2 miles Sault Ste. Marie-Elliot Lake Sheet Ontario of Mines geological Map Department 2100, 1967; l" = 4 miles. Echo Lake Geological Survey No. of Canada aeromagnetic 2123G, 1963; l" = l mile. map Wakomata Lake Geological Survey map No. of Canada aeromagnetic 2227G, 1963; l" = l mile. GEOLOGY

As mentioned previously, because of cave-ins in pits, very"©little of the mineralized vein could be seen during our visit to Otter Township. V Mineralized .floats that have been excavated from

RIO TldTO CANADIAN EXPLORATION LIMITED jLncij.cate that heavy massive and disseminated chalco pyrite mineralization occurs in a quartz vein, which in turn, © apparently is confined to a basic dike intruded in Archean granite. In places the chalcopyrite mineralization is associated with specular hematite. © On a broader scale the outcrop pattern in the surveyed area suggests that the mineralized dike has been intruded into a more or less east-west situated mass of Archean granite which to the north, east and south is overlain by flat lying younger Gowganda© sediments - - of Huronian age. To the north of the picket line grid the sediments, in turn, are overlain by Nipissing diabase (Post-Huronian in age)©. The granite outcropping in the vicinity of Post l, Claim SSM 89475 suggest a rugged Pre-Huronian topography, and the Huronian sediments now found in the area probably were laid down in©valleys occurring in the Archean basement complex. The following is a brief description of the rock found types in the surveyed area: GRANITE is a medium grained, reddish to pink colored rock, containing 30?6 to 50% quartz, flesh to dark colored K-feldspar, and minor amount-of mafic minerals. The rock is massive; the outcrops are well t jointed, and form ledges along the more prominent joints. In one outcrop (L6E, 1+80S) the granite contained some greenstone inclusions.

HURONIAN SEDIMENTS occurring in the mapped area belong to the Gowganda formation. Within the mapped area the majority of

HIO TlrtTO CAUAblAN EXPLOnATIOH LIMITED which consist of le sedimentary outcrops are conglomerate, 9 to 6 inches in diameter set abundant subrounded granite pebbles up the pebbles appear to be into^a greywacke matrix. In composition elsewhere in the area. In very similar to the granite outcropping 4E and 6E there are two the southern part of the grid near Lines fine grained, greenish grey small outcrops of greywacke; the rock is feldspar and v/hite quartz in color, with angular and subangular pink the rock is flesh colored. clastic grains. The weathered surface of © * * * in an-outcrop DIABASE occurs, within the mapped area, elsewhere north of the 70 feet south of Post l, Claim SSM 89475; but they have not been grid area diabase outcrops are numerous, probably belongs tied in with the surveyed lines. This formation known as Nipissing diabase. to the intrusive sills and dikes commonly green in color, and has The rock is medium to coarse grained, dark The diabase consists diabasic texture; it weathers rusty brown. with lesser amounts of mainly of calcic plagioclase, chlorite,

hornblende, quartz, pyrite, sphene, etc. into rocks of BASIC DIKES apparently have been intruded the Nipissing diabase. . The all ages with the possible exception of very fine to fine grained dike within the mapped area is dark green, the rock contains small rock. In the outcrops between L-0 and L2W of. chalcopyrite up to euhedral grains of pink feldspar, and specks small quartz.veinlets 1/16" in diameter. The dike contains numerous i * - pit 120 feet west of with grains of pyrite. Floats near a filled-in with quartz and pyrite. L2W, 0+70S had specular hematite associated the MINERALIZED QUARTZ VEIN of unknown width occurs in t * the test "basic dike at and near 0+00 on L-0. Floats removed from occurs in pits -suggest that massive and disseminated chalcopyrite In quartz near the contact between granite and basic dike. azurite and addition to the sulphides the vein contains malachite, complimentary some specular hematite. A weak E.M. conductor with a pits. The magnetic anomaly coincides with the mineralized test i length of some 500©to 600 feet; most of it conductor has a strike - - - . . that westwards is obscured by overburden. It is interesting to note i floats the conductor does not extend to the pit near which the

containing the specular hematite are found.

CONCLUSIONS . - t Heavy chalcopyrite mineralization occurs in a quartz where it had vein in a basic dike cutting pink granite. The vein, a weak E.M. been exposed in test pits, had a width of 5 to 7 feet; strike length conductor suggests that mineralization extends for a

of 500 to 600 feet. © ~

RECOMMENDATIONS © It is recommended that the E.M. conductor should be along a tested by short diamond drill holes. The base line runs of it. A few side of a hill, with the height of land to the south provide a negatively inclined holes drilled towards the south would

maximum of information with a minimum of drilling.

A. Benkis October 8, 1968 Rolands PART II REPORT ON GEOPHYSICAL SURVEYS REUBEN MG KEE OPTION OTTER TOWNSHIP, ONTARIO

N.T.S. 41-J-ll JUMMARY

Reconnaissance investigation of the McKee showing Township indicated in Otter minor electromagnetic and magnetic irid lines correlation. at 200-foot spacings were cut to cover tensions. the -east-west The survey ex of these lines outlined a minor (4-5 pp.) conductor zone 500-600 feet long with positive magnetic to correlation 2000 gammas. . of up . - .©ONCLUSIONS . © " . © © Indications are that a mineralized west zone extends 100 and 400 feet east feet of the McKee showing. RECOMMENDATIONS © © . It is recommended to .test the extensions geophysical outlined by the survey to determine if the copper mineralization pyrite) of "the showing (chalco continues along the indicated zone. DISCUSSION OF GEOPHYSICAL RESULTS A test line of horizontal loop E.M. over inconclusive the showing was partly due to elevation differences of the stations. Vertical loop E.M. indica©ted . : minor conduction. The lines were surveyed i by the detail vertical by placing the loop method transmitter over a previously located crossover while une adjacent lines. A conductor of 600 feet strike length .was outlined with deflections of 4-5O pp. The magnetometer survey indicated positive magnetic correlation of up to 2000 gammas, with the chalcopyrite zone (at the showing) falling on the south flank of the magnetic high. PERSONNEL © - . © - " R. A. Benkis, Geologist 394 Goldenwood Rd.,- Willowdale, Ontario. H. Be:ckmann, Geophysical Instrument Operator 1086 Albertson Crs., © " Port Credit, Ontario. D. N. Sexsmith, Geophysical Instrument Operator 85 Hollyrood Hts. Dr., Port Credit, Ontario.

s , R. McKee, Prospector . . © c/o Demers Bay Hotel, . R. R. #3, /- . Thessalon, Ontario. © . Line Cutting 4 Man days © l Mapping M i 2 II l Geophysical Surveys ; 4 "

m \ . Reports li n l i, o l l l October 7 , 1968 H. Beckmann i l RIO TlriTO k. CANADIAN EXPLOr.ATIOH LIMITED APPENDIX

.OPI-IYSICAL SURVEYS

MODEL SE 600 ELECTROMAGNETIC . / UNIT The SE 600 is a moving source electromagnetic unit capable of measuring In-Phase and Out-of-Phase components at coil separations up to 300 feat.

Readings are recorded at 100-foot stations with the reference point midway between the two coils. 1 - -- . . .© . ~ . A typical anomaly due to © a sub-surface conductor will consist of a decrease in -the In-Phase reading and a negative Out-of- Phase reading.

As a horizontal loop unit, both coils are moved along a line, preferably cut across the strike of the formation. Penetration is approximately one half of the coil separation.

A simple conversion enables the operator to employ the SE 600 as a vertical loop unit. With this method the receiver and transmitter can be run (a) in line (b) on parallel lines 400 feet apart and (c) with the transmitter stationary and the receiver moving on adjacent lines and up to 800 feet away. This increases the depth penetration considerably. Readings are recorded in degrees of de flection and interpretation is comparable to other vertical loop units. The SE 600 is battery powered and operates on 1600 cps. © - Horizontal loop data are plotted in per cent (56) In-Phase and Out-of-Phase signal while the vertical loop results are plotted in degree (o ) of deflection resulting in crossovers over electro magnetic conduction. © © APPENDIX

GEOPHYSICAL SUKVEY Magnetometer Survey No. An AsXania torsion magnetometer, Serial has a range of 250,000 was employed during the survey. It and can be read to an gammas, a scale constant of 250 gammas has been tied in about accuracy of *- 5 gammas. The survey to day variations, and . every hour to check stations and day The zero point is arbi diurnal drifts have been corrected. illustration of the data trary and has been chosen for better form of contours. which is plotted in profile or in the APPENDIX 3

Report on Geophysics and Drilling,

Macpherson Option, 1971

Selco Exploration Co. Ltd. EXPLORATION COMPANY LIMITED

"W. J- Anderson June 10, 1971. INTRODUCTION prospect in is a vein-type copper The Macpherson Option Township The property is in Otter Thessalon, Ontario area. north of the 4L-J-11, some 22 miles in N.T.S. reference area Thessalon. surveys the results of geophysical This report describes and spring of out by Selco in the winter and drilling carried 1971.

PREVIOUS WORK Macpherson in the optioned from Mr. M. The property was work done on the time of acquisition the fall of 1970. At the a combined some trenching and sampling, property included and two short drill magnetometer survey, vertical loop EM and holes.

GENERAL GEOLOGY and an by an intrusive granite The property is underlain is shown on andesite. The latter of massive carbonated lithology of inlier as diabase or a similar regional government maps in earlier work is the terminology used unknown age, and this on the property. are all in the showings on the property The exposed veins containing and consist of quartz-dolomite discontinuous andesite and massive irregular specular hematite sampling of accessory In the old pit No. l of chalcopyrite. across aggregates yielded up to 2.28*54, Cu the vein material apparently 4.5 feet.

GEOPHYSICAL WORK 1968 by survey carried out in The EM and magnetometer cross 600 feet long, with broad yielded a conductor a direct mag others amplitudes of 10O and overs having peak-to-peak up to 1500 gammas. netic correlation of performed a this work a Selco crew In order to confirm grid trending of this year across a similar survey in February axis. along the old conductor at 12Oo and centered toy broadside The previous conductor was not detected coil separation, and vertical loop traverses using a 2OO ft. in plan and the resulting magnetic anomaly, while similar to the north. dimensions to the old anomaly, was displaced be the Sufficient magnetite occurs in the volcanics to has a better source of the anomaly and as the later anomaly this survey was correlation with the extent of the volcanics, accepted as more reliable. from The significant result of the surveys, as is evident is that the the location of the vein on the accompanying plan, or magnetic mineralization does not produce an electromagnetic response.

DRILL RESULTS drill In the fall of 1970, Macpherson put down two short the accompany- holes to the west of the best surface showing.(see feet of quartz- int drill hole plan). Hole H-l intersected ten 2.70/6 cu (one carbonate veining and yielded values of at least in this assay result is missing but the footage is included H-2 apparently calculation) over a true width of 7.0 feet. Hole hole were not intersected the vein but values obtained in the received by SeLco. the con In May 1971, three holes were spotted to test a final check on tinuity of the mineralization and also provide the old conductor. of pit No. l, The first hole S-l, was collared 100 feet east directly beneath and did not intersect the vein. Hole S-2 passed quartz - carbona the original pit and intersected one foot of barren quartz-carbonate from veining. The third hole picked up mineralized pending assay 126.5 to 132.5. A visual estimate of the grade feet. results is 2.5-3*^, Cu over a true width of 4.5 hole to The latter intersection necessitated an additional a barren quartz- check any westerly extension. Hole S-4 intersected carbonate vein at 134.5-136.5 the old Nothing was observed in the core which could explain conductor. SIGNS AND^RECOMMEIMiJrt.ij.v-.i.^ The five holes completed on the showing demonstrate the erratic nature of the mineralization. Holes S-l, S-4, and presumably H-2 limit any strike extensions and hole S-2 precludes any depth extension. The results define a very limited narrow pocket of moderate mineralization, upon which no further work is

warranted.

W. J. Anderson. II 8 e t ^ 0 .s ^ ^ DD DD 0 ri \ Vi o M tPHc/r * (- R ^ ^ S ^5 I t A h 0 J: 5 .x i l i; * Ui r V}

\ i

352

1971

19, 19,

REMARKS

DEPTH

May May

..W. ..W.

ELEVATION ELEVATION

TOTAL TOTAL

SIGNED

COMPLETED COMPLETED

No.

1971 1971

CI. CI.

16, 16,

5AYS

May May

STARTED STARTED

ERED

CORE CORE

RECOV RECOV

ONTARIO

LIMITED

CORE CORE

LENGTH

RECORD

AREA. AREA.

0 0

COMPANY COMPANY

210

DRILL DRILL

FROM

THESSALON THESSALON

COLLAR COLLAR

- -

NO.

EXPLORATION EXPLORATION

SAMPLE SAMPLE

DIP DIP

BEARING BEARING

SELCO SELCO

OPTION OPTION

DIAMOND DIAMOND

and

pyrite

cent

dark

coarse coarse

Approx.

and

axis

section.

some

and and

to to

and

per per

Composition

PHERSON PHERSON

pyrite pyrite

intervals

flecks flecks

and and

core core

over over

fractures fractures

grey grey

to to

fractures fractures

chlorite.

feldspar feldspar

feldspar feldspar 0 0

Several Several

chlorite chlorite

flecks flecks

dark dark

occasionally occasionally

thick thick

throughout. throughout.

calcite calcite

pink pink thin thin

with with

J.0% J.0%

to to

scattered scattered

at at

1mm 1mm

with with

of of

PROPERTYJIAC

equigranular. equigranular.

zone.

chalcopyrite chalcopyrite

DESCRIPTION

with with

vein vein

coarser-grained coarser-grained

filled filled

massive. massive.

vein vein

magnetite magnetite

Scattered Scattered

subhedral subhedral

minor minor

present.

Altered Altered

hematite.

grey, grey,

massive, massive,

angles angles

Occasional Occasional

quartz quartz

aggregates aggregates hematite-stained hematite-stained

angles angles

medium-grained, medium-grained,

(lS-20%) (lS-20%)

quartz quartz

ORISSETTE

medium-grained medium-grained

3" 3"

to to

2" 2"

occasional occasional

UUIN UUIN

tiny tiny

+OOE

142-146 142-146

chalcopyrite chalcopyrite

varying varying

specular specular 99-104 99-104

57.6 57.6 chalcopyrite.

96 96

showing showing containing containing

5% 5%

and and carbonate carbonate

BY..^ BY..^

Fine Fine

greenish greenish disseminated disseminated

varying varying

Pink, Pink,

essentially essentially quartz quartz muscovite. muscovite.

grained, grained,

l l

s-l s-l

ANDESITE:

GRANITE:

CASING

No No

No. No.

DRILLED DRILLED

148

LOCATION LOCATION

HOLE HOLE

SHEET SHEET

FP-IM

i i

1 j

: : © © j

REMARKS

DEPTH

SIZE

ELEVATION ELEVATION

CORE CORE

TOTAL TOTAL

PLETED

SIGNED

COM

No.

——

" "

CI. CI.

——————————

— —

3 3

4 4

ASSAYS

STARTED

EHto

CORE CORE

nccov- nccov-

LIMITED

CORE CORE

LENGTH

RECORD

COMPANY COMPANY

DRILL DRILL

FROM

COLLAR

NO.

EXPLORATION EXPLORATION

SAMPLE SAMPLE

DIP DIP

BEARING BEARING

SELCO SELCO

and

DIAMOND DIAMOND

textures

material.

and

quartz quartz

round round

of of

internal internal

to to

within within

fine-grained fine-grained

consists consists

PROPERTY.

veins veins

spherical spherical

- -

subrounded subrounded

grey grey

DESCRIPTION

and and

is is

shows shows

dark dark

sediment sediment

blebs blebs

and and

which which

HOLE HOLE

of of

-i

OON

above above

places.

+ +

5 +OOE

l l OF OF

—

in in

surrounding surrounding

some some Possible Possible

As As

outline outline

hematite hematite BY

END END

GRANITE:

No No

No. No.

DRILLED DRILLED

352 352

HOLE HOLE LOCATION LOCATION

SHEET SHEET

VOM

' '

148

[ [

j f

353'

1971

ANDERSON-

J. J.

REMARKS

23, 23,

W. W.

DEPTH DEPTH

SIZE

May May

CORE CORE ELEVATION

TOTAL TOTAL

SIGNED

COMPLETED COMPLETED

No.

1971 1971

CI. CI.

nil

21, 21,

ASSAYS

May May

trace

3.11

STARTED STARTED

tfiED

CORE CORE

RCCOV- RCCOV-

ONTARIO.

1.0

350© 350©

LIMITED

d* d*

1.0

CORE

LENGTH

AREA, AREA,

RECORD

0 0

23.1

COMPANY COMPANY

DRILL DRILL

22.1

FROM

THESSALQN THESSALQN

COLLAR COLLAR

- -

NO.

EXPLORATION EXPLORATION

SAMPLE SAMPLE

0310

DIP DIP

BEARING BEARING

SELCO SELCO

OPTION OPTION

5©

patche

quartz

core

DIAMOND DIAMOND

and

frag frag

lcm lcm

Fine

grey,

to to

clusters

and

quartz

with with

O O

lower lower

pinkish

present present

PHERSOJL PHERSOJL

content.

metacrysts.

and and

equigranular.

hematite hematite

axis. axis.

at at

Over Over

patches patches

calcite calcite subangular subangular

greenish greenish

and and

pyrite pyrite

chalcopyrite chalcopyrite

interval interval

disseminated

muscovite.

slightly slightly

pyrite pyrite

core core

vein vein

calcite calcite

of of

tiny tiny

feldspar feldspar dark dark

chalcopyrite chalcopyrite

massive, massive,

eldspar-quartz-calcite

to to

and and

f f Minor Minor

and and

O O

to to

PROPERTY^.MAC

section. section.

calcite calcite

visible visible

recrystallization recrystallization

subrounded subrounded

quartz quartz

DESCRIPTION

separating separating

flecks flecks

of of

pink pink

euhedral euhedral

assive assive

to to

brecciated brecciated

at at

grey grey

more more

Scattered Scattered

cent cent

of of

A A

subhedral subhedral

chlorite chlorite

thick thick

Rare Rare

hematite hematite

veins veins due due

tiny tiny

aggregates.

andesite. andesite.

dark dark

per per

Coarser-grained Coarser-grained

Partly Partly

Scattered Scattered

of of

1.6" 1.6"

contact contact

medium-grained, medium-grained,

ORISSETTE

remainder remainder

ID-15% ID-15%

across across

with with

DW DW

. .

cm cm

L L

O+IOE

S-2

present. present.

increased increased

Several Several

interval, interval, over over

considerably considerably

70-118 70-118

magnetite. magnetite. 59-67 59-67

scattered scattered

carbonate carbonate

irregular irregular

quartz. 61-62 61-62

2 2

ments ments

26.1 26.1 Pink, Pink,

blebs.

axis axis

grained, grained,

BY. BY.

Upper Upper

Composition Composition

with with

ANDESITE:

CASING

GRANITE:

NO NO

NO. NO.

DRILLED DRILLED

37.1

156.5

LOCATION LOCATION

HOLE HOLE

SHEET SHEET

37.1

FROM

1 1

;

l s

1 1 t P

REMARKS

DEPTH DEPTH

SIZE SIZE

CORE CORE

ELEVATION ELEVATION

TOTAL TOTAL

SIGNED SIGNED

COMPLETED

No.

CI. CI.

ASSAYS

STARTED

ERED

CORE CORE

RECOV RECOV

LIMITED

CORE CORE

LENGTH

RECORD

COMPANY COMPANY

DRILL DRILL

FROM

COLLAR

NO.

EXPLORATION EXPLORATION

SAMPLE SAMPLE

DIP DIP

BEARING BEARING

SELCO SELCO

DIAMOND DIAMOND

seams.

chlorite chlorite

thin thin

DESCRIPTION

Occasional Occasional

HOLE.

IOE IOE

+ +

above. above.

1+25N

O O

S-2

OF OF

BY,

As As

pyrite.

END END

GRANITE GRANITE

No No

No. No.

DRILLED DRILLED

353

LOCATION

HOLE HOLE

SHEET SHEET

FROM

" " 1.56.5

1971

AXT

REMARKS

28, 28,

DEPTH DEPTH

SIZE

May May

ELEVATION

CORE CORE

TOTAL TOTAL

SIGNED__W. SIGNED__W.

COMPLETED COMPLETED

No.

1971 1971

CI. CI.

nil nil

nil

25, 25,

ASSAYS

0.03

0.02

0.07

May May

4.23

0.76

10.39

- -

STARTED STARTED

1.5

ERED

ONTARIO.

CORE CORE

RECOV RECOV

350' 350'

LIMITED

1.5

CORE CORE

LENOTH

AREA, AREA,

RECORD

L27.5

L29.0

132.5

COMPANY COMPANY

2lo

DRILL DRILL

FROM

131.0

127.5

126

THF.SSAT.ON THF.SSAT.ON

COLLAR50

- -

NO.

EXPLORATION EXPLORATION

0313

0312

0311

SAMPLE SAMPLE

DIP DIP

BEARING BEARING

OPTION OPTION

SELCO SELCO

DIAMOND DIAMOND

and

coarse

and

at at

Occasion Occasion

grained

anhedral

to to

stringers

several

halcopyrite/

with

axis axis

fine

PHF.R.qoN PHF.R.qoN

to to

chalcopyrite,

vein vein

A A

and and

chalcopyrite chalcopyrite.

MAC MAC

visible visible

vein vein

core core

veins veins

coarser coarser

muscovite muscovite

medium medium

of of

grey, grey,

inclusions inclusions

to to

rarer rarer

RTY RTY

flecks flecks

aggregates.

throughout. throughout. E E

subhedral subhedral

P P

minor minor

fleck fleck

45 45

quartz quartz

approx. approx.

aggregates aggregates

and and

feldspar feldspar

R.O R.O

@ @

Somewhat Somewhat

P P

angular angular

..^...... ^

greenish greenish

odd odd

with with

and and

DESCRIPTION

to to

pink pink

calcite calcite

carrying carrying

quartz-carbonate quartz-carbonate

equigranular, equigranular,

the the

thick thick

pyrite pyrite

magnetite magnetite

dark dark

Averages Averages

Quartz-carbonate Quartz-carbonate

r- r- present.

blebs blebs

cm cm

of of

occasional occasional

to to

with with

Composition Composition

small small

massive. massive.

axis, axis,

thick thick

with with

1.5 1.5

1" 1"

grey grey

.MORISSEIIE^ .MORISSEIIE^

Massive, Massive,

subangular subangular

j j

f f pyrite pyrite

core core

flecks flecks

to to

places places

10N

+ +

1.5©.

126-127.5 126-127.5

andesite. andesite.

scattered scattered

123 123

and and

to to

chalcopyrite chalcopyrite

or or

usually usually

al al

Scattered Scattered

in in

mm mm

numerous numerous

Disseminated Disseminated

feldspar-quartz, feldspar-quartz,

Pink Pink

grained, grained,

Dark Dark

chlorite chlorite

1 1 grained. grained.

o+gow

s-3

BY___

ANDESITE:

GRANITE GRANITE

CASING

No No

No. No.

DRILLED DRILLED

33.3

151.5

LOCATION LOCATION

HOLE HOLE

SHEET SHEET

33.3

F"OM

[ [ i i

f © © ; ;

REMARKS

DEPTH

SIZE

ELEVATION ELEVATION

CORE CORE

TOTAL TOTAL

SIGNED___. SIGNED___.

COMPLETED

No.

CI. CI.

4 4

ASSAYS

STARTED

ERED

CORE CORE

RECOV RECOV

LIMITED

CORE CORE

LENGTH

RECORD

COMPANY COMPANY

DRILL DRILL

FROM

COLLAR

NO.

EXPLORATION EXPLORATION

SAMPLE SAMPLE

DIP DIP

BEARING BEARING

SELCO SELCO

5mm

than

DIAMOND DIAMOND

rare

to to

carbonate

carbon carbon

vein vein

quartz

less less

up up

quartz

Only Only

of of

quartz quartz

with with

minor minor

approximately

flecks flecks

carbonate carbonate

axis. axis.

breccia breccia

some some

thick thick

present.

core core

andesite andesite

brownish brownish

lcm lcm

PROPERTY

Averages Averages

quartz quartz

discrete discrete

with with

in in

to to

DESCRIPTION

chalcopyrite.

as as

130.5, 130.5,

Massive Massive

Replacement Replacement

axis. axis.

45-50 45-50

Massive Massive

flecks flecks

At At

Andesite Andesite

chalcopyrite chalcopyrite

veining veining

(3 (3

core core

of of

HOLE HOLE

with with

chalcopyrite/1.5 chalcopyrite/1.5

to to

vein vein 2

halcopyrite halcopyrite

above.

10N

OF OF

+90W

+ +

1 1

s-3

BY_,..

50 50

129.0-130.0 129.0-130.0

35©^ 35©^

130-131. 130-131.

131-132.5 131-132.5

ild ild

flecks flecks

ate ate

127.5-129.0 127.5-129.0

As As

across.

vein vein

veining. veining.

carbonate carbonate

END END

GRANITE GRANITE

No No

No. No.

DRILLED DRILLED

354

LOCATION LOCATION HOLE HOLE

SHEET SHEET

r^oM 151.5

165'

6/71

AXT AXT

REMARKS

Anderson.. Anderson..

J. J.

DEPTH

SIZE SIZE

June June

,-W. ,-W.

. .

CORE CORE

ELEVATION ELEVATION

TOTAL TOTAL

SIGNED SIGNED

COMPLETED COMPLETED

No.

CI. CI.

5/71

ASSAYS

STARTED

ERED

CORE CORE

RECOV RECOV

-ONTARIO,

LIMITED

CORE CORE

LENGTH

ARF.A ARF.A

RECORD

leo

COMPANY COMPANY

DRILL DRILL

FROM

TJESSAT.ON TJESSAT.ON

COLLAR COLLAR

- -

NO.

EXPLORATION EXPLORATION

SAMPLE SAMPLE

DIP DIP

BEARING BEARING

some

SELCO SELCO

OPTION OPTION

DIAMOND DIAMOND

axis,

felds felds

with

at at

with with

rare

at at

muscovite

of of

and

core core

equigranular,

grey

vein vein

and and

inclusions inclusions

subhedral subhedral

to to

veins veins

minor minor

pyrite pyrite

_MACPHERSON _MACPHERSON

O O

across across

dark dark

of of

carbonate.

quartz-carbonate

with with

non-uniform, non-uniform,

icm icm

massive, massive,

carbonate carbonate

at at

in in

quartz quartz

hematite hematite

127 127

places places

subangular subangular

PROPERTY

essentially essentially

set set

thin thin

In In

blebs blebs

thick thick

DESCRIPTION

119, 119,

quartz-dolomite quartz-dolomite

metacrysts metacrysts

Some Some

VEIN:

grained, grained,

Icm Icm

specular specular

introduced introduced

136.

fine-grained, fine-grained,

patches patches

to to

small small

rounded rounded

at at

116.5, 116.5,

barren barren

feldspar-quartz feldspar-quartz

axis. axis.

scattered scattered

axis.

with with

medium medium

chalcopyrite.

Composition Composition

material. material.

5mrn 5mrn

- -

chalcopyrite.

ANDESITE:

Morissette

to to

grey, grey,

-CARBONATE -CARBONATE

114, 114,

chlorite.

5W 5W

core core

+ +

S-4

BY^ BY^

1 1

0450N

andesite andesite

to to flecks flecks

usually usually

Massive, Massive,

to to

86, 86,

and and

veins veins

72-73 72-73

pink. pink.

anhedral anhedral

Fine Fine

scattered scattered

spheroidal spheroidal

Scattered Scattered

pathic pathic

minor minor

considerable considerable

Dark Dark

QUARTZ QUARTZ

GRANITE GRANITE

ALTERED ALTERED

CASING

No. No.

DRILLED DRILLED

136.5

134.5

LOCATION LOCATION

HOLE HOLE

SHEET SHEET

rnow 134.5

UEMARKS

DEPTH DEPTH

SIZE

CORE CORE

ELEVATION

TOTAL TOTAL

SIGNED SIGNED

COMPLETED

No.

CI. CI.

—

,AY

AS?

STARTED

FRCD

CORE CORE

RECOV- RECOV-

LIMITED

CORE CORE

LENGTH

RECORD

COMPANY COMPANY

DRILL DRILL

FROM

COLLAR

NO.

EXPLORATION EXPLORATION

SAMPLE SAMPLE

DIP DIP

BEARING BEARING

SELCO SELCO

DIAMOND DIAMOND

5-10 5-10

veins veins

quartz quartz

PROPERTY

DESCRIPTION

scattered scattered

- -

HOLE HOLE

above above

2 2

4 4

OF OF

s s

136.5-140 136.5-140

thick.

As As

END END

GRANITE:

o. o.

DN DN

No No

DRILLED

165

LOCATI

HOLE HOLE

SHEET

FROM

136.5

j r

t t

l l i i f APPENDIX 4

Mineral Deposit Inventory Record(MDI)

with a brief description of the deposit and of the history of exploration and development

The Geoscience Centre,

Ontario Geological Survey, Toronto

RECORD

|::t63'i36a^,:.:

;

(MDI) (MDI)

JiiiWaviSSpK: JiiiWaviSSpK:

DEPOSIT DEPOSIT

- -

|l^Mi:;:iii|^^:|iis;y

^^•^i^M'ti-itiiSiV^ipJ:

ss:-:;.:.:|::Ml:;:|

......

1983

INVENTORY INVENTORY

;;

MINERAL MINERAL

22. 22.

t t

0 0

6 6 o o

0 0

NAMES

o o

0 0

6 6

AR AR

j j

, ,

i i t t

o o

0 0

rv.-.

P P

0 0

B B

- -

1 1

i i

A A

:e :e

M M

i i

STATUS

::.si ::.si

S S

ffi ffi

EXTENSION

/-^ /-^

is is

;'.*il-iB ;'.*il-iB

-M -M

." ."

ATE: ATE:

0 0

o o

0 0

6 6

0 0

o o

q q

0 0 0 0

Q Q

0 0

0 0 {j {j

; ;

* *

| |

...,

LALTERNATt LALTERNATt

-; -;

0. 0. ciw ciw

0 0

g g

6 6

5 5

J;.si J;.si

;*:i ;*:i

RECORD RECORD

; ;

ifbWNSHip ifbWNSHip

QUALIFIER QUALIFIER

;:|:;

S: S:

.:-;:S

?vS

: :

::::;:?s

;H;

; ;

vi vi

E E o o

f;:-::;:;::: f;:-::;:;:::

D D

; ;

i- i-

; ;

"OTTER

IN IN

COMMODITY

"R" "R"

LEGEND

OF OF

155

;

.||.

.;;

.v .v

'.;-; '.;-;

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: :

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; ;

0446

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i-..

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311041

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5159805

A A

- -

" "

;- ;-

from from

. .

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- -

: :

eCOflilj.

:-'\':'-:S

IN IN

KM KM

moris::

: f

- -

frbrti frbrti

ongitudes; ongitudes;

; ;

: :

2 2 |- |-

oil oil

;

ai,--:-^^-

: :

erred erred

fii fii

;y- ;y-

? ?

:V: :V:

ZONE ZONE . .

:|^''.^^|.

" "

LAKE LAKE

*wo *wo

-':- -':-

: :

trarisf trarisf

XliitBrred XliitBrred

'-:: '-::

: :

ABOUT ABOUT

EASTING EASTING

SMDR SMDR

'-- '--

NORTHING NORTHING

UTM UTM

.s^'i .s^'i

: :

::;

under under

: :

;-;.; ;-;.;

.was .was

::;

liriltudes liriltudes

7. 7.

l l

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locoiibii locoiibii

lonjjiiOdei; lonjjiiOdei;

SAUNDERS SAUNDERS

iVo iVo

pplni pplni

: :

Itickt Itickt

PROP PROP

:irid :irid

: :

STATUS

sjSect sjSect

id;:.or.'

e e

2331 2331 OCCURRENCE

AT AT r r

: :

flr flr

: :

tudei tudei

:d^pbslt:;br :d^pbslt:;br

:r*W--0r"6ipi'efi:

bi)t:;Vhiji bi)t:;Vhiji

SURVEY SURVEY

RESOURCES

:'66dyv-6f;'ihinw*ili*tloiiri^

:m*p:

: :

MAP MAP

ilstl ilstl

DDH DDH

ifiii ifiii

irid irid

CENTRE

'''' '''' iif iif

*tk)Vi

OF OF

gJEôgf.epîc gJEôgf.epîc

*i *i

riilt riilt

another another

MAJOR MAJOR

tfi*iV:t)h* tfi*iV:t)h*

; ;

1976, 1976,

DATA DATA

.shewing .shewing

QUALIFIER QUALIFIER

10 10

NATURAL NATURAL

r:ieft

P35-36 P35-36

GEOLOGICAL GEOLOGICAL

^:sln9le:tibdy::6fnltnerii|ilM ^:sln9le:tibdy::6fnltnerii|ilM

P77 P77

CU CU

either either

GS GS

or or CCURRENCE

OLLAR OLLAR

More More

:n-HJif( :n-HJif(

. .

"SafTi*; "SafTi*;

: :

,: ,:

PRECISE

SIMPLE

C r:A

.,'A .,'A

: :

OF OF

MCKEE

:-'^ :-'^ : :

:;i

::*; ::*;

27©56"

34©CO 34©CO

155, 155,

- - 49, 49,

L L

iSlli'^^-IT'SnBB iSlli'^^-IT'SnBB

REFERENCES

l l

ONTARIO ONTARIO

GEOSCIENCE GEOSCIENCE

BS© BS©

46* 46*

OTTER OTTER ALGOMA ALGOMA

41J/11SW 41J/11SW

GR GR

410/11 410/11

MP MP

. .

:: ::

STATUS STATUS

MINISTRY MINISTRY

;:cpOEb::S ;:cpOEb::S

CbMPbuNb::

LOCATED LOCATED

;

1971. 1971.

1976, 1976,

FILE, FILE,

LOCATEJ3:;, LOCATEJ3:;, COMMODITY

REFERENCE REFERENCE

1 1

OGS OGS

NMI NMI

OGS OGS

LONGITUDE

HOV? HOV?

MAT* MAT*

DEPOSIT DEPOSIT

DISTRICT

LATItUDE LATItUDE

TOliitf TOliitf Ontario

Ottawa. Ottawa.

ore ore

four four

was was

CU CU

8 8

the the

cptioned cptioned

in in

built built

Resources. Resources.

custoi custoi

hand- hand-

addi addi

an an

Also Also

Township Township

VcKee VcKee

and and

REF. REF.

explore explore

1971, 1971,

was was

and and

into into

of of

for for

L©arie L©arie

to to

of of

property property

Mines Mines

Three Three

magnetometer magnetometer

adit adit

Exploration Exploration

Reuben Reuben

Ste. Ste.

1974.

the the

nine nine

showing showing

Energy. Energy.

section section

tonnage tonnage

adjoining adjoining

material material hy hy

summer summer

of of

bin. bin.

material. material.

J/ll

a a

drilled drilled

ILE

srr.all srr.all

tbe tbe

Sault Sault

the the

by by

41 41

a a the the

in in

1967 1967

Tribag Tribag

siall siall

Canadian Canadian

on on

January January

in in

of of

grade grade

were were

in in

is is

In In

A A

geological, geological,

DEVELOPMENT

Department Department

in in

the the

Apparently Apparently

owned owned

a a

It It

drive drive

him him

hand-cobbed hand-cobbed

to to Incorporated.

feet feet

Tir.to Tir.to

high high

AREA AREA

AND AND

Sector. Sector.

to to

did did

by by

was was

502011

staked staked

of of

road. road.

Doughty Doughty

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were were

EXPLORATION EXPLORATION

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(Riocanex). (Riocanex).

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1573, 1573,

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Thessalon, Thessalon,

HISTORY HISTORY

the the

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the the

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Thessalon-Chapleau Thessalon-Chapleau 1963 1963

Limited Limited

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PROVINCE PROVINCE

TERRITORY

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province province

Algoma

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ADDRESS

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DESCRIPTION DESCRIPTION

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Associated Associated

PRODUCT PRODUCT

OWNER OWNER

UNCERTAINTY UNCERTAINTY

OBJECT OBJECT YHB-12* . 77 .

More recent exploration for copper was hy diamond drilling. In 1956, Fano Mining and Exploration Incorporated drilled six holes totalling 1,003 feet to test a chalcopyrite-bearing shear zone in Archean granitic rocks in southwestern Otter Township. The best recorded analyses were 1.71 percent copper over a width of 2 feet and 3.51 percent copper over a width of 5 feet (Shklanka 1969, p.26). In 1966 to 1967, G. Poirier drilled 80 feet on the chalcopyrite-bearing quartz vein on the Huston Lake Prospect or Gould Mine (Shklanka 1969, p.26) in northwest Gould Township (Shklanka 1969, p.28). A drift is being driven at present along the vein by Gould Copper Mines Limited. In the summer of 1971, four holes totalling about 1,220 feet were drilled on the Reuben McKee Property in east Otter Township into a chalcopyrite-bearing quartz vein associated with a diabase intrusive in Archean granitic rocks (Assessment work files, ODMNA, Resident Geologist©s office, Sault Ste. Marie).

In 1956, Pluton Uranium Mines Limited drilled three holes, totalling 546 feet, into a chalcopyrite-bearing quartz vein in sandstone of the Gowganda Formation. The site is 1/4 mile west of the outlet of Wakomata Lake in Township 188 (Assessment work files, ODMNA, Resident Geologist©s office, Sault Ste. Marie) .

Ground.geophysical surveys were carried out as follows: in 1966, on the north shore of Jobammageeshig Lake by the Mississagi Mining Company Limited and on the west shore of Wakomata Lake by Jubilant Creek Mines Limited, and in 1968. on the Reuben MrKpp property by Rio Tinto Canadian Exploration Limited (Assessment work files. ODMNA, RpgiH^nt geologist©s office. Sault Ste. Mariet. Since 1968, minor staking and development work has been carried out on copper prospects in the area by R.J. Jowsey Mining Company Limited (now Open End Mines Limited) and others.

As a result of discovery of the Blind River uranium deposits, exploration for this metal has been carried out to test the Huronian rocks in the south western part of the area. To date, however, no deposits have been found. In 1966, Kerr Addison Mines Limited drilled 529 feet in four holes to test quartz pebble conglomerate in the Matinenda Formation near the centre of the south boundary of Otter Township (Assessment work files, ODMNA, Resident Geologist©s office, Sault Ste. Marie). In 1968, Imperial Oil Enterprises Limited drilled two deep holes. The first, at the southwest end of Skookum Lake in Galbraith Township, passed through Huronian sedimentary rocks to reach Archean granitic rocks at 2,443 feet. The second, on the north shore of Cooper Lake in Haughton Township, passed through 1,100 feet of basalt and 1,450 feet of Huronian sedimentary rocks before reaching Archean granitic rocks (Assessment work files, ODMNA, Resident Geologist©s office, Sault Ste.Marie).

Aerial geophysical surveys to search for radioactive anomalies were flown in 1968 by Subeo Limited and by W.D. Sutherland and associates (Assessment work files, ODMNA, Resident Geologist©s office, Sault Ste. Marie).

General Geology: Parts of the area have been mapped by Collins (1925) , Emmons (1926, Map 194A), and Frarey (1959). Granitic Archean rocks underlie the northern half of the area as well as a salient, the Haughton High, in the northeastern part of Haughton Township. The granitic rocks are dominantly pink, massive, and granular. Small pockets of porphyritic and gneissic a quartz vein about a mile (1.6 km) west on Urquhart Lake. In lot 11 and the north half of lot 12, concession VI, Gould Township, and in the north half of lot l, concession VI, Haughton Township, many other small chalcopyrite-bearing quart/, veins have been uncovered. Observations on some of the trenched and pitted veins were recorded in 1971 by R.J. Rupert, formerly the Resident Geolo gist at Sault Ste. Marie (see Regional Geologist's Files, Ontario Ministry of Nat ural Resources, Sault Ste. Marie). The Gould Mine adit lies in an east-facing cliff about 25 feet (7.6 m) high consisting of Gowganda paraconglomerate and sandstone. Mineralization occurs in a shear /one that strikes N660W, dips south at 60CS, and is probably a reverse fault. The shear zone is quartz veined, hematite stained, and is 40 feet (12 m) wide. The 10-foot (3 m) square opening of the adit mouth lies on a 6-foot (1.8 m) wide zone of the best mineralization, the southern part and northern 3 feet (0.9 m) of which contain abundant specularite. According to Shklanka, (1969) in 1967 a test pit exposed the vein for a length of 10 feet (3 m) and a width of Wt feet (l m) including a l foot (0.3 m) of massive chalcopyrite and specularite. In 1966-1967, trenching and 80 feet (24 m) of dia mond drilling in one hole was done by G. Poirier. In 1968, trenching was carried out by Gould Coppermine Limited. A general account of the work is given in the Elliot Lake Standard (1969). R.J. Rupert selected grab samples from the ore dump near the drift for assay in 1971; the results of the assays are not known (Regional Geologist's Files, Sault Ste. Marie, Ontario Ministry of Natural Resources).

Reuben McKee (7)

The mineralized quartz vein is located at the centre of lot l, concession III, Otter Township, and may be reached by crossing the Mlssissagi River with an amphibious four-wheel-drive vehicle. This mineralized quartz vein lies in an area where Early Precambrian grani tic rocks are cut by Nipissing Diabase. To the south, an outlier of Gowganda par aconglomerate partly surrounds the mineralized quartz vein at a distance of about 300 feet (90 m). An east-striking Nipissing-type diabase dike lies about 300 feet (90 m) to the north of the deposit. In 1968, R.A. Benkis and H. Beckman,(see files in Assessment Files Re search Office, Ontario Division of Mines, Toronto) noted chalcopyrite minerali zation in a 5- to 7-foot (1.5 to 2 m) wide quartz vein in a basic dike intruded into Early Precambrian granite. A magnetic and electromagnetic survey described by Benkis and Beckman indicated a 500- to 600-foot (150 to 180 m) long vein (Assessment Files Research Office, Ontario Division of Mines, Toronto). Four diamond-drill holes that were drilled in 1971 and a pit were located on the property by the writer in the summer of 1971 relative to a survey picket l -t- 00 south 6 + 00 west as follows [ according to the author]: Diamond-drill hole number l, bearing S220 E, distance 260 feet (80 m). Diamond-drill hole number 2, bearing S120 E, distance 180 feet (55 m). Diamond-drill hole number .1, tearing S220W, distance 135 feet (41.1 m). The drill hole dips 60 0 toward S34 0 . 35 Saunders Lake Area

Diamond-drill number 4, due west, distance l!)(l I'rct (.r)H m). The diamond-drill hole dips 7()0 due south. The pit [not shown on Map 2331, hack pocket | was located 'I'M feet (70 m) onabearingof SI20 W In 1971, the writer examined the diamond-drill core from the four holes that was left at the diamond-drill hole sites. Diamond-drill holes one to three were at)out .'150 feet (110 m) long, and drill hole number four about l(i.r) feel (50 m) long. They penetrated diabase and granite. Minerali/aliori in the core is as fol lows: None was observed in diamond-drill core left at hole one. Hole number two contains a ,'i-fool (0.9 m), (apparent) thickness of a quartz- carbonate vein at a length of 20'/z feet ((5.2 m) in the hole with a l inch (2..r) cm) width of 50 percent chalcopyrite Hole three contains 50 percent chalcopyrite in diabase at a length between 129 and 131 feet (39.3 and 39.9 m) and .'10 percent chalcopyrite in a quart /.-carbo nate vein between the lengths of l 34 and l 36 feet (40.H and 41 At m ). In hole four, a barren quart/.-carhonate vein was found between the lengths of 135 and 137 feet (41.1 and 41.7 m) and ata length of 162 feet (49.4 m) there oc curred '/2 inch (13 mm) of chalcopyrite. The pit covers l square yard (0.8 m-), and in it is exposed a 2Vi-foot (0.7fi m) wide vein striking northeast (63") and dipping N750 W. The vein contains two /ones l inch (25 mm) and '/2 inch (13 mm) wide respectively consisting of chalco pyrite. Many angular blocks (i inches (15 cm) to l foot (0.3 m) in maximum di mension, and which contain 50 to 75 percent chalcopyrite with minor quartz, were scattered around the pit. In 1967, the vein was exposed by R. McKee (Regional Geologist's Files, Min istry of Natural Resources, Sault Ste. Marie). From the condition of the dia mond-drill core the author considers that the four diamond-drill holes described above were drilled in 1971.

Resource Exploration and Development Company Limited (6)

Resource Exploration and Development Company of Toronto hold several claims in northwestern Gould Township that include the Cheney Mine. The Cheney Mine is located in lot 7, concession V, Gould Township '/z mile (0.8 km) south of Chub Lake. The head frame is located within 300 feet (90 m) of Highway 129 on the west side of the road. The mine lies within a Gowganda paraconglomerate member, which in cludes subordinate sandstone and orthoconglomerate dipping 100S and N. A quartz vein about 100 feet (30 m) east of the mine strikes east and dips 500S. A quartz vein 700 feet (210 m) southwest of the mine strikes N800 W and dips fK+i 65"S. The mineralized vein in the mine is reported by Shklanka (1969) to strike if ?v?. east and dip 45" to 600S. It is cut by later diabase dikes. Chalcopyrite, pyrite, specularite, siderite or ankerite, barite, and calcite occur in the veins. The following account is condensed from Shklanka 1969, p.26-27: The zone has been traced by diamond drilling to a depth of 460 feet (140 m) and on the surface it has been traced 4,000 feet (1,200 m) along strike. The width 36 -t- /-^S-:" , i*" -' -~ - -- - . .r —J5,f—— -V^. X V . f.A, 1^; few -J ...- ^ '•i\ •~SV' ^ .r- ^? ^^v,. * W 'j •S",^. 3-^ c?' " - — -* %^/^/i -;: , * \'*\ •v* Îf y -"( " \ l " - c*. ./r •v/ ? ^ ^1^ m*.V 505sf ?^:s- .v -q J ,-^P^ l '--i * T* -— *y Qg y i- a,'/! L_i i"-** v/y- :/ '.r! Of - r, u 'ea W-V .; 5s"* *7/ VI -dS !** L ^V/ ^"^*/ ^ ^"'Jy o vi .- fiV' ^-7^? 'f*// ,, ^. v A-vv,^- sor ! A /i l* •' s-', ^^^"•^ sf/s {•vr/ i.1 C 'J **w^.. '* ^//X A r* ?,.? s; i V ^ 1' cf) S* ...-A- v/ ^t / *-iv , ^? ..?^' ."^ "r ^ -^M^T-^ *.# ^ ^ r y®* c N^ t/ /\9 t h -?\ ^- ^ s \VV fi'J ? ' •' "^ '.A'.s\ —-V \\ T---,r— H" ' "'-f&ftl f-*^ :( . ^ ' --' ,V ^ (^---- J f v'' V. o^ y \ 3 -gx-;^"~'- ^ N Sk/ M'^ I J) JsTjMl 7V t\: i* S i fT^l \ /fr V\ !\*- *u *.i,i ^5X^ iff 5 :\ Â'^3"*S "*-5 'OS "Y' S?^,"tys ^^ r-'- •l'imi ,.^ •w -*" ^*" \ ?s/?-* ( U/ 3 to il ^ \ -r- ™ ^ •O. S? L2^?^ ^ *4 -* l' ^ 05* X i^ fs 99 K WA S /& m !?/ i'*? v'S^ fr/ ^lî SO ///^ o T#sy y \ r*?* j xa. i^ i^* o- '^V \ V-1. •xi&r a * i/ os- vi *Z~ ^ *J.j f /frvw A ^ > ir (S Ci'.f ss? J& Ssv -c:.* ^ ?t*i -^-r\, ^^* i t Î^f^ v ^ 00 sS- * ^ Jr tv It N. /O t. ? V^-J:U 1 •Li- \^- V X 00 •®5 ^ •'-A l r, : -'J Ministry of Report of Work Conducted Transaction Number Northern Development ~~ Mines After Recording Claim Ontaric Mining Act

Personal information collected on this form is obtained under the authority of the l this collection should be directed to the Provincial Manager, Mining Lands, Mi Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264. 41JllSWee07 2.14316 CASSON 900 Instructions: - Please type or print and submit in duplicate. - Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining Recorder. - A separate copy of this form must be completed for each Work Group. - Technical reports and maps-must accompany this form in duplicate. - A sketch, showing the claims the work is assigned to, must accompany this form.

Recorded Holders) ~ Client No.

Address ^ ~ . ^ — ^-j - Telephone No. ll.K'#3t ItiBSShLdAJ. ff/lSt- Ut K iJLo Mining Division Township/Area M or G Plan No. X- X. M fyRjE CASSON * a-ffBfc Dates /O / l i Work From: W *T~ \ 1 Gt ~ To: /^/*~T" c* J 'ft, Performed (7* (X^ J f jO CsCsC' X O f Work Performed (Check One Work Group Only) RECEIVED , Work Group Type V Geotechnical Survey fl/ q&sft*;*^- J2^J^tl^^ SEP 0 6 1991 Physical Work, Including Drilling ^ ' u ' MINING LANDS btuFiON ' Rehabilitation •*t)ther Authorized S Work ^ P * -fi jJ?^^Er~ ^~ '

_J f- Assays F 3 ( ^ Assignment from Reserve

Total Assessment Work Claimed on the Attached Statement of Costs $ o( of oCP - Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report) Name Address /IJ'S-Q-T. WoMWGZ ^TD tp.8-fcoiSn92L- 1 WfivJ*. 0/isr. PtoU^

RECORDED. .

SEP - 4 1991 (attach a schedule If necessary) RecelDt -, Certification of Beneficial interest * See Note No. 1 on reverse side i——— . Date RecoW e^ Holder or(AoentTSignaturel l certify that at the time the work-was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder. ^&3L ^^k

Certification of Work Report l certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report Is true. Name and Address of Pereon Certifying

Date Notice for Amendments Sent

0241 (03/81) m

s* J g S1 -s i! SU)

onthisClaim Assessment WorkDone Valueof 00 c* QQ OS CXJ * * * * Gs*

(K Od 00 f O-

I Q! S.-

I su t* K . fe te **

Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priprize the deletion of credits. Please mark ( s) one of the following: 1. D Credits are to be cut back starting with the claim listed last, working backwards. 2. [Ruredits are-to be cut back equally over all claims contained in this report of work.. 3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented.

Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following: Signature Date l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed. Ministry of Statement of Costs Northern Development Transaction No./N 0 de transaction -"l Mines for Assessment Credit Ontario . 50 /f ^iere du Etat des couts aux fins Developpement du Nord et des mines du credit devaluation Mining Act/Loi sur les mines

Personal information collected on this form is obtained under the authority Les renseignements personnels contenus dans la presente formule sont of the Mining Act. This information will be used to maintain a record and recueillis en vertu de la Lol sur les mines et serviront 4 tenir d jour un registre ongoing status of the mining claim(s). Questions about this collection should des concessions minieres. Adresser toute quesiton sur la collece de ces be directed to the Provincial Manager, Minings Lands, Ministry of Northern renseignements au chef provincial des terrains miniers, ministere du Development and Mines, 4th Floor, 159 Cedar Street. Sudbury, Ontario Developpement du Nord et des Mines, 159, rue Cedar, 4e etage. Sudbury P3E 6A5, telephone (705) 670-7264. (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/Couts directs 2. Indirect Costs/Couts indirects * * Note: When claiming Rehabilitation work Indirect costs are not Amount Totals allowable as assessment work. Type Description Montan! Total global Pour le remboursement des travaux de rehabilitation, les admissibles en tant que travaux Wages Labour couts indirects ne sont pas Salaires Main-d'oeuvre devaluation. Field Supervision Amount Totals Supervision sur le terrain Type Description Montan! Total global Type Type Contractor's f /ea-* Transportation *3W* and Consultant's ytesdys Transport ffe.H.-up Fees Drolts de ('entrepreneur CotisujL-rAiM FEB& 3.VK-* feti-TAL- et de l 'expert - consell &177-* Type Supplies Used Fournltures utllisees *#j:* Food and Lodging Nourriture et hebergement Mobilization and Type Demobilization Equipment Mobilisation et Rental demobilisation Location de Sub Total of Indirect Costs *SK~ materiel Total partiel des couts indirects Amount Allowable (not greater than 2(W of Direct Costs) 3K~ Montan! admissible (n'excedant pas 20 H des couts directs) Total Direct Costs Total Value of Assessment Credit Valeur totale du credit *4W* |Total of Direct and Allowable devaluation Total des couts directs Indirect costsl (Total de* cotits directs teff? et Indirect* admissible* (TC?

Note: The recorded holder will be required to verify expenditures claimed in Note : Le titulaire enregistre sera tenu de verifier les depenses demadd6es oaos this statement of costs within 30 days of a request for verification. If le present etat des couts dans les 30 jours suivant une demande d cet verification is not made, the Minister may reject for assessment Y*uJV-^N — II eflel.-Si la verification n'est pas effectuee, le ministre peut rejeter tout all or part of the assessment work submitted. RECEIVGrQrjejpartie des travaux devaluation presentes.

Filing Discounts SEP depot

1 . Work filed within two years of completion is claimed aV V i travaux deposes dans les deux ans suivant leur achevement sont the above Total Value of Assessment Credit. ' Tembotrse's'a! lin) "/o de la valeur totale susmentionnee du credit devaluation.

2. Work filed three, four or five years after completion is claimed at 2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement 500Xo of the above Total Value of Assessment Credit. See sont rembourses a 50 Vo de la valeur totale du credit devaluation calculations below: susmentionne. Voir les calculs ci-dessous.

Total Value of Assessment Credit Total Assessment Claimed Valeur totale du credit devaluation Evaluation totale demandee x 0.50 = x 0,50 =

Certification Verifying Statement of Costs Attestation de l'etat des couts l hereby certify: J'atteste par la presente : that the amounts shown are as accurate as possible and these costs que les montants indiques sont le plus exact possible et que ces were incurred while conducting assessment work on the lands shown depenses ont ete engagees pour effectuer les travaux devaluation on the nrrnmr sur les terrains indiques dans la formule de rapport de travail ci-joint. je suis autorise that as authorized Et qu'a litre de ( (Recoiled HolderTAgentAPosition irf Company) (titulaire enregistre, representant, poste occupA dans la compagnie) to make this certification a faire cette attestation. Ministry of Report of Work Conducted Transaction Number Northern Development and Mines After Recording Claim Ontaric Mining Act /c* ne Co/0 y

Personal i. 'ion collected on this form is obtained under the authority of the Mining Act. This information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street. Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264. ' ^ , * o l f

Instructions: - Please type or print and submit in duplicate. - Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining Recorder. - A separate copy of this form must be completed for each Work Group. - Technical reports and maps must accompany this form in duplicate. - A sketch, showing the claims the work is assigned to, must accompany this form.

Recorded Holders) . Client No. /f/ C. do WE R. Address Telephone No.

Mining Division Township/Area M or Q Plan No. tS. 3366 V- Dates Work From: To: Performed i h olie Work Performed (Check One Work Group Only) Work Group Type Geotechnical Survey Physical Work, RECEIVED Including Drilling x RECORDED. ^ Rehabilitation SEP 03 1991 1 1 ir o o iqqi Other Authorized nwU fa u UsJ 1 Work MIMING LANDS SECTION ,/ pereipf Assays V sV-tjm&U-KSt Assignment from Reserve 'J ff Total Assessment Work Claimed on the Attached Statement of Costs S Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report) Name Address /V/u.ru ^SS/^M/ft ITJI/CL- /^7 /tf/ss/'/u; ^^. ll^uM , ^x/r-

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

1 certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder.

Certification of Work Report 1 certify that 1 have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after its completion and annexed report is true. Name and Address of Person Certifying dlAOOE f.- Telepone No. Date - 8V/-. h

SrC- V X/v C& Total Value Cr. Recorded Date Recorded Mining Recorder , 7 """•T&STStE. MAPE MINING DIVISION L&teZ- - 4*?3/*?/ RECEIVED Deemed Approval Date Date Approved /f

Date Notice for Amendments Sent AH 23AOU1991 pM 7,8,9,10,111121112,3,4,5,6

0241 (03W1) ISJj

-Q •-Si -O si H

3 in 2.3 5)3" S

a*IStn ^ to c i -o 05*1* Ci. 2-1 S 2- Vi •^ (D ^

l — 3** C 3 S.*

B?il? 53*8 "&S2 ga? 9 (D

indicate from to minimize the adverse effects of such deletions, please you are claiming in this report may be cut back. In order Credits Please mark (s) one of the following: which claims you wish to priorize the deletion of credits. listed last, working backwards. 1. D Credits are to be cut back starting with the claim contained in this report of work. 2. B uredits are to be cut back equally over all claims appendix. 3. G Credits are to be cut back as priorized on the attached priority, option one will be implemented. In the event that you have not specified your choice of etc., with respect transfers, option agreements, memorandum of agreements, Note 1: Examples of beneficial interest are unrecorded to the mining claims.

leased land, please complete the following: Note 2: If work has been performed on patented or Signature Date in the patented l certify that the recorded holder had a beneficial interest or leased land at the time the work was performed. ^Ministry of Statement of Costs orthern Development Transaction No./N 0 de transaction nri Mines for Assessment Credit Ontario ..stere du Etat des couts aux fins D6veloppement du Nord et des mines du credit devaluation

Mining Act/Loi sur les mines

Personal information collected on this form is obtained under the authority Les renseignements personnels contenus dans la pr6sente formule sont of the Mining Act. This information will be used to maintain a record and recueillis en vertu de la Loi sur les mines et serviront a tenir a jour un registre ongoing status of the mining claim(s). Questions about this collection should des concessions minieres. Adresser toute quesiton sur la collece de ces be directed to the Provincial Manager, Minings Lands, Ministry of Northern renseignements au chef provincial des terrains miniers, ministere du Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario D6veloppement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury P3E 6A5, telephone (705) 670-7264. (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/Gouts directs 2. Indirect Costs/Gouts indirects

Amount Totals * * Note: When claiming Rehabilitation work Indirect costs are not Type Description Montant Total global allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les Wages Labour couts indirects ne sont pas admissibles en tant que travaux Salaires Main-d'oeuvre devaluation. Field Supervision Amount Totals Type Supervision sur le terrain Description Montant Total global ————— - •^ Type Contractor's ^^. Transportation and ConsuH^jFs /fc5 -S/) 'y'S Transport Fees x^ —~— —— ———— - zzr^ Drolls de ('entrepreneur ^o/Vsiut, T/ffsr /~^cs 3 *8 f 3 -6^ et de 1 'expert ~ consell 397700 Type 7 Supplies Used Fournitures utlllsees -=^====- ^

Food and Lodging Nourriture et hebergement Mobilization and Type Demobilization Equipment Mobilisation et Rental ^ TtfjC/t /ffrff/9 L . ••aa* 75 demobilisation Location de materiel Sub Total of Indirect Costs Total partial des couts indirects Amount Allowable (not greater than 2044 of Direct Costs) 3&M Montant admissible (n'excedant pas 20 Vt des couts directs) Total Direct Costs Total Value of Assessment Credit Valeur totale du credit Total Total of Direct and Allowable devaluation des couts directs rzsz.4* ndirect costs) (Total des codls directs et Indlrects admlsslbles

Note: The recorded holder will be required to verify expenditures claimed in Note : Le titulaire enregistr6 sera tenu de verifier les defenses demandees dans this statement of costs within 30 days of a request for verification. If le present etat des couts dans les 30 jours suivant une demande a cet verification is not made, the Minister may reject for assessment work effet. Si la verification n'est pas effective, le ministre peut rejeter tout all or part of the assessment work submitted. ou une partie des travaux devaluation presentes.

Filing Discounts Remises pour depdt

1. Work filed within two years of completion is claimed at 10007o of 1. Les travaux deposes dans les deux ans suivant leu r achievement sont the above Total Value of Assessment Credit. remboursgs a 100 "/o de la valeur totals susmentionnee du credit devaluation.

2. Work filed three, four or five years after completion is claimed at 2. Les travaux deposes trois, quatre ou cinq ans apres leur achievement SQo/o of the above Total Value of Assessment Credit. See sont rembourses a 50 Vo de la valeur totale du credit devaluation calculations below: susmentionne'. Voir les calculs ci-dessous.

Total Value of Assessment Credit Total Assessment Claimed Valeur totale du credit devaluation Evaluation totale demandee x 0.50 x 0,50 =

Certification Verifying Statement of Costs Attestation de l'etat des couts l hereby certify: J'atteste par la presente : that the amounts shown are as accurate as possible and these costs que les montants indiques sont le plus exact possible et que ces were incurred while conducting assessment work on the lands shown depenses ont ete engagees pour effectuer les travaux devaluation on the accompanying Report oLWork form. sur les terrains indiques dans la formule de rapport de travail ci-joint. that ... ^ ^ , am authorized Et qu'a litre de je suis autorise (flee6rdSd Hi (titulaire enregistre, representant, poste occupd dans la compagnie) to make this certification faire cette attestation.

0212 (04/91) Nota : Dans cette formule ines, le masculin est utilise au sens neutre. Mining Lands Branch Geoscience Approvals Section 159 Cedar Street, 4th Floor Sudbury, Ontario P3E 6A5 Telephone: (705) 670-7264 Fax: (705) 670-7262 File: 2. 14316

Mr. Bob Owen Ontario Geological Survey 77 Grenville Street Room 812 Toronto, Ontario M7A 1W4

Dear Sir:

Re: Work submitted on mining claims SSM 609013 et al. in Casson and Otter Townships.

As per your request, we are highlighting this file as the work falls under the category of ASSAYS.

For further information, please contact Clive Stephenson at (705) 670-7251. Yours sincerely,

Ron C. Gashinski Senior Manager, Mining Lands Branch Mines Se Minerals Division CDS Ontario Ministry of Ministere du Geoscience Approvals Section Northern Development Developpement du Nord Mining Lands Branch 159 Cedar Street, 4th Floor and Mines et des Mines Sudbury, Ontario P3E 6A5 Toll Free: 1-800-465-3880 Telephone: (705) 670-7264 Fax: (705) 670-7262 Our File: 2. 14316 Transaction #: W9150.5009 January 10, 1992 Mining Recorder Ministry of Northern Development and Mines 875 Queen Street East P. O. Box 669 Sault Ste. Marie, Ontario P6A 2B3 Dear Sir/Madam: RE: APPROVAL OF ASSAY COSTS FOR SAMPLING ON MINING CLAIMS SSM 609013 ET AL. IN CASSON AND OTTER TOWNSHIPS.

The assessment work credits for Assaying, section 17 of the Mining Act Regulations, listed on the attached Assessment Work Credit form, have been approved as of January 6, 1992. The attached credit form replaces the one filed as part of the original submission. If you have any questions please contact Clive Stephenson at (705) 670-7251. Yours sincerely,

Ron C. Gashinski Senior Manager, Mining Lands Branch Mines and Minerals Division CM CDS/jl Enclosures: cc: Assessment Files Office Resident Geologist Toronto, Ontario Sault Ste. Marie, Ontario ASSESSMENT WORK CREDIT FORM FILE NUMBER: 2. 14316 DATE: January 6, 1992 RECORDER© 8 REPORT NUMBER: W9150.5009

RECORDED HOLDER: McKee Copper Inc. CLIENT NUMBER: 168120 TOWNSHIP OR AREA: Casson and Otter

VALUE OF ASSESSMENT VALUE APPLIED VALUE ASSIGNED CLAIM NUMBER WORK DONE ON THIS CLAIM TO THIfl CLAIM FROM THIS CLAIM

SSM 609013 O 8. 50 O $ 8. 50 SSM 699925 g 8. 50 $ 4. 25 $ 4. 25 SSM 699929 $ 8. 50 $ 4. 25 $ 4. 25

SSM 699924 O O 4. 25 O SSM 699926 O O 4. 25 O SSM 699927 O $ 4. 25 O SSM 699928 O S 4. 25 O

Totals S25. 50 $25. 50 . 00 - y L--A/

P.O. Box 2Q21 7Q5-889-2133 (Wawa) V/awa, 705-889-2247 (Fax) POS IKO 705-841-1091 (Thessalon)

July 1991

of Expenses for Kge Copper Report

1 Report by J.P- Mills 3,200.00 --

2 In. 101-B - by S. Babcock - services 675.00 V

~3 In. 625 - by G.M,S. for vehicles, etc. 375.00 y

4 Invoice - Wawa Assaying - 12 samples _ 1 02.00* TOTAL 4.352.QO

Maureen Babcock LJ'i T 3 O 19 i A :eived from ud9 H-Strf H t. f. 4 t The sum of _. . La somme de ' L-'1- RECEIPT/REQURENTLOYERDE 100 Renl of Pour le lover da tJ '•"f., ? ic.

Month ending No. Mois terminant

-•fw,

(^~p eceivedfrm P.O. Box 1998 - Wawa, Ontario POS 1KO - 705-856-4443 127 Mission Road Fax - 705-856-2902

RECEIPT

December l, 1990

RECEIVED FROM: NSAI Holdings $ 102.00 ------One Hundred and Two Dollars------xx

For the analysis of 12 McKee copper samples, sample #©s 4713 to 4724, @ $8.50 each. Ontario Ministry of Ministere du Geoscience Approvals Section Northern Development Developpement du Nord Mining Lands Branch 159 Cedar Street, 4th Floor and Mines et des Mines Sudbury, Ontario P3E 6A5 Toll Free: 1-800-465-3880 Telephone: (705) 670-7264 Fax: (705) 670-7262 Our File: 2. 14316 Transaction #: W9150. 5011 January 10, 1992 Mining Recorder Ministry of Northern Development and Mines 875 Queen Street East P. O. Box 669 Sault Ste. Marie, Ontario P6A 2B3 Dear Sir/Madam: RE: APPROVAL OF A GEOLOGICAL EVALUATION SURVEY ON MINING CLAIMS SSM 609010 ET AL. IN CASSON AND OTTER TOWNSHIPS.

The assessment work credits, subsection 18(6) of the-Mining Act Regulations, listed on the attached Assessment Work Credit form, have been approved as of January 9, 1992. The attached credit form replaces the one filed as part of the original submission. If you have any questions please contact Clive Stephenson at (705) 670-7251. Yours ^incerely,

Ron C. Gas hi ne ki Senior Manager, Mining Lands Branch Mines and Minerals Division CDS/DS/ j l Enclosures: cc: Assessment Files Office Resident Geologist Toronto, Ontario Sault Ste. Marie, Ontario ASSESSMENT WORK CREDIT FORM FILE NUMBER: 2. 14316 DATE: January 10, 1992 RECORDER© S REPORT NUMBER: W9150.5011

RECORDED HOLDER: Me Ree Copper Inc. CLIENT NUMBER: 168120 TOWNSHIP OR AREA: Casson and Otter

VALUE OF ASSESSMENT VALUE APPLIED VALUE ASSIGNED CLAIM NUMBER WORK DONE ON THIS CLAIM TO THIS CLAIM PROM THIS CLAIM SSM 609010 $ 212. 50 O $ 212. 50 SSM 609011 $ 212. 50 O $ 212. 50 SSM 609012 $ 212. 50 O $ 212. 50 SSM 609013 s 212. 50 O ^ 212. 50 SSM 699924 $ 212. 50 $ 354. 16 O SSM 699925 $ 212. 50 $ 354. 16 O SSM 699926 ^ 212. 50 $ 354. 17 O SSM 699927 $ 212. 50 $ 354. 17 O SSM 699928 g 212. 50 ^ 354. 17 O SSM 699929 S 212. 50 fi 354. 17 O

Totals $2125.00 $2125. 00 S 850. 00

TOTAL ASSESSMENT WORK CREDIT IS S 2,125.00 IVIII llvlll J ut Natural Northern Development Resources and Mines Ontario •O'j jrrj

INDEX TO LAND DISPOSITION

MN R. ADMINISTRATIVE DISTRICT PUN .iV^1 - BLIND R;VFR G-3266 MINING DIVISION TOWNSHIP SAULT STE. MARIE LAND TITLES/REGISTRY DIVISION CASSON ALGOMA

^^LJ;) -- fr - -'~ Scale 1:20 000 '^ -; * 1000

1000 1000 MOO 4000 5000 MMM TOM (00* 101

Contour Interval 10 Metre*

AREAS WITHDRAWN FROM DISPOSITION MRO- Mining Rights Only SRO - Surface Rights Only M ^ S - Mining and Surface Rights

b/MBOLS OntorNo DM* FHv (".l 3tC 16IH SO is/t/r* SRO Boundary CVsEL 3biRsoi*aoi i/2/ao SRO Township. Meridian. Baseline ("l) StC JblR S f)'l*|OI WIO/60 10/T/ao SRO IMS09 IFIOOOINS TO CONTOUR CLtVATIOM IIIO*) Road allowance, survnyet. shoreline Lot/Concession, surveyed . tinsiirveyed Parcel, surveyed . . unsurveyod .... . - i '} WJL r l - v^ Right-of-way, road . i ' ' i ^**,0\T V railway . . I'tihty Reservation ...... Cliff. li* Pile ...... *- - —— T l "i i* l i-^'c&s' S- Contour ...... g. ^"* H. Interpolated ...... i 1FT\\S Approximate .. . •: - , tdf^k—L- Depre- sion . 03: l Control point (horizontal) ...... A f\f vVr* lad'4

Mine head frame Pipeline (above r round) l 102437ft ' 'J Railway, single track double .rack NOTES FLOODING RIGHTS ON wlUSISSAGI RIVER RESERVED TO CONTOUR 903* abandonee1 W PL A N* 35 FILE 593? vol 4 y ' / ~f~ Road, highway, coun'y. township i i ; x c,- Jio ,'xii :Y - access .. . trail, bush ...... Shoreline (original) ... . . Iransmips.on line ...... Wooded~,^......

DISPOSITION OF CROWN LANDS

Patent Surface A Mining Rights ...... 9 THE INFORMATION THAT Surface Rights Only ...... O APPEARS ON THIS MAP HAS BEEN COMPILED Mining Rights Only ...... Q FROM VARIOUS SOURCES, AND ACCURACY IS NOT Lease GUARANTEED THOSE Surface A Mining Rights ...... WISHING TO STAKE MIN Surface Rights Only ...... S ING CLAIMS SHOULD CON SUIT WITH THE MINING Mining Rights Only ...... B RECORDER, MINISTRY OF NORTHERN DEVELOP Licence of Occupation ...... T MENT AND MINES, FOR AD Order-in Council...... ,...... OC DITIONAL INFORMATION ON THE STATUS OF THE Cancelled ...... ® LANDS SHOWN HEREON Reservation... SandAGravesl 1^ ^ - .' t A *:.— "r "* " 7^""

i) -'l-'l; i --

Map base and land disposition drafting by Surveys and Map,nng The disposition ol land, location of tot fabric and pare* boundmn on Branch, Ministry of Nature l this index was compiled for adminHHrativ* purpoaOT only.

^-i —r-—rtrTTTTr————^ "J Resources * and Mines Ontario J ( } \ ,^)S )\\A i I'M t- t TOWNSHIP INDEX TO LAND DISPOSITION

M.N.R. ADMINISTRATIVE DISTRTT PUN BLIND RIVER G-3309 MINING DIVISION TOWNSHIP SAULT STE. MARIE LAND TITLES/REGISTRY DP/1SC s OTTER ALGOMA

Scale 1:20 OOC

l K

'S, - **M 7MO (• * L ~ - Contour Interval

AREAS WITHDRAW* FROM DISPOSITION

MRO - Mirwig Ricmts Only 8RO- SurTac* Rights Only M * 8 - Mmmq *nd Surface Rights

if Or**rN* Ft* " ^ \' SYMBOLS w to/an JO .'*0 S K O

Boundary "r) w 4/is M O •k 'MD *)IVJH Township Mendian. Bavahne .

Head allowance, surveyed ... shoreline ——— — l——tt—teUf"———— ^' ~~[3]~5K*—FiT-1 Lot/Concession, surveyed., unsurveyed

Parcel, surveyed ...... unsurveyed .....

Right-ot-way. road railway . . utility .. __L J Reservation . Cliff Pit. Pile

Contour Interpolated l r -xv-^ -' ; Approximate A-^A*'^"' "^ Depression ^r— NR--.V -r^— --i * -^**- Control point (honzomal) Flooded land

Mine head frame

Pipeline (above ground) .

Railway, single track .. double track.. .. abandoned Road, highway, county, township x v^I\"'|)T access ...... , --x-fc-i ((J/-1 trail, bush .. .. Shoreline (original) ..

Transmission line...... - Wooded •rea......

-l - fcctT I DISPOSITION OF CROWN LANDS i J ^98890 Patent :\.\ -M \\\U Surface A Mining Rights \V W\ Surface Rights Only...... e Mining Rights Onry e

Leasu Surface A Mining Rights Surface Rights Only B Mining Rights Only B Licence of Occupation . - - - - T oc - Order nrv-Council .. - - (S) LV j ss Cancelled ...... THE INFORMATION TH -. (D APPFARS ON THIS M^ Reservation..... - ••••- - HAS BEEN COMPIL. Sand A Gravel ...... - - .O FROM VARIOUS SOURCF AND. ACCURACY IS M' GUARANTEED THO WISHING TO STAKE ING CLAIMS SHOULD SULT WITH THE MINIKC RECORDER, MINISTRY NORTHERN DEVEU MENT AND MINES FOR A., DITIONAI INFOHMATir - ON THE STATUS OF TV-: tfGHTON-% ioWNSHIP LANDS SHOWN HEREO* -f^^-vSLfe r// ~\^^ j^T--^ ^K/N^.; i^lkX^. r^t^/i 'l -'. . ~? -^ ^0^*- Map base and land disposition drafting by Survey* and Mapping Thedtspositionof land, l tab c and pefcel oa purpoiM*onry Branch. Ministry of Natural Resources tw *ndu WM compiled tor

4.1.1 liSWft*97 e M316 CASSON 210

•i*- Post l* SSM 89475 Pott 2- SSM 89474

''•"Hi :''' "- '"' *" ' Jr* 1 '

Post l - SSM 99478 Pott 2 SSM 89475

JtlUTf Off

2 M316 CASSON 220 IN 8SM

IN r/ i -rA l

*i!~j?* io*.M^~k •ton*—-ft / Pi! l-7 .Bit ** l** -Orlfn •Mi •l **4'*l*

1 " " ' ——— 1 NT! MO TINTO CANADIAN EXPlOIATtON iTD. l LEGEND: *f-*-ll ____ - ———————* — —^R N * . "* 1 1 MCUMN MC HEE OPTION OTTCR TWr.tOJl| Minirolittd qwOf 4 f Bfltic tfyM a GEOLOGY 1 Otobott W!' of 1 MC KEE SHOWING J

OCT. M

41J118WM*/ 2.H316 CASSON Access road Stockpiled muck from the adit, most fragments General access SAMPLE 4723 show variable amounts of road, curving 2.67*^ copper "chalcopyrite, malachite, Quarts veining occurring Previously excavated random grab to the east Raise, about 6m to limonite and, possibly, in diabase host rocjj, now filled in with sampl e 6.5m deep showing bornite. The pile is the chalcopyrite mineralization, old timbers, muck and highly fractured source of the 500 ton strong limonite alteration, growth, vtin zone also \ Zone of thin overburden, Overburden mineralized Diabase host bulk sample sent Tribag highly fractured, blocky, serves as a c reek bed minor quartz veining zone, veining and diabase rock on each side \ Mines, assaying 4.5 ife some offshoots into wall in places and offshoots , omitted from wall rock of excavation copper. Pile dimensions; rock SAMPLE 4715 from the main zona Vein section sketch map containing soil P o r t a l areo^ show tag about 8.5m x 10.4m x 3m Vein attitude: 270 a \80 0 - 85 0 16 . 3^ copper s light l ^magnetic Oy e jrbu L den and vein rubble ~ mineral i zed quartz- Vein width in places ranging from over O . 5m, zone , carbonate visimnc;, chip sample E, 4722 Vein width ranging omitted from partly 11 o u 11 u 11 l. 2m to l.5m IS.87% copper, from O.6m to 1m sketch map Diabase \ hand-cobbed grab \ sample

-' - ^ —————— ^--7- - ; - Jfc-r^ SAMPLE 4714 ^ ' ' ' Overburden Q.23% copper About 416m east, quartz Overburden -^ chip sample on -H ^, veining with minor -•I - .^ /l -:r^^^- quartz-carbonate chalcopyrite and hematite vein material is exposed in the creek pile V with hematite bed. SAMPLE 4724, O . 8** SAMPLE 4720 _ 4721 fein section excavat Vein width JlrciruJjLL h o L; t rock SAMPLE 4717 copper, taken from muck Q.12% copper over Granite-diabase ^ SAMPLE 4718 SAMPLE 4716 Paraconglomerate . 4% copper, J3 AMPLER 47 L 9 :or the 50 ton bulk ranges from rock expojed along 22.67Sfe copper pile at an old trench 1m Quartz- contact, sharp 10.92* copper Q.57% copper host rock, grab sample IQ.39% copper sample analysed at l.?m to l.5m excavation sides, over O.7m, near the veining carbonate veining alteration over 0.7m over 0.5m of granite locally from muck pile grab sample jJoranda(12 ;J) copper) and red, massive, chip sample with hematite and lacking, steeply chip sample quartz- carbonate beside trenching from muck Copper Corporation coaro grained chalcopyrite Overburden dipping vein material beside raise [22!* copper)

IIIo-rv 19.1.

Magne tic FIGURE 7, Sketch map of mineralized quartz- decl illation carbonate vein exposure locations at the main showing area, claim SSM 282633. Scale(metnc) : 1:250 (vertical seal e exaggerted) .

4U11SWM97 Z M 316 CASSON 2

i*/ n* 5

41JIISWM97 2.14316 CASSON 250

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