075MNE0013,1,1,"The DOD showing occurs within the Slave Supracrustal Province, Archean in age. The Supracrustal rocks are of the Yellowknife Supergroup, dominated by a volcanic-greywacke-mudstone sequence forming various greenstone belts that cover about one third of the province. Granitoid intrusions make up the bulk of the craton and are grouped as pre-, syn-, and post- Yellowknife Supergroup. In addition, several mafic dykes have intruded the shield, orientated between 140 and 180 degrees. The DOD showing is situated on the Camsell Lake property which is approximately 20 miles north of the East Arm of Great Slave Lake. The rocks on the Camsell property are volcanics and sediments of the Yellowknife Supergroup which occur as two northeasterly trending belts. These belts have been intruded by glomeroporphyritic leucogabbro/gabbro stocks, gabbro sills and rare leucogabbro sills. Granitic intrusions include dykes and stocks of granodiorites of various compositions and pegmatites of the same phases. All rocks of the area are intruded by north-northwesterly magnetic diabase dykes. This showing is a Cu-Ni mineral occurrence from two drill holes. The mineralization is disseminated in a gabbroic volcanic and ranges from 0.23% Cu over 10 feet to 0.45% Cu over 2.2 feet and 0.11% Ni over 10 feet to 0.12% Ni over 5 feet. The showing was discovered after geophysical work in 1967 located an anomaly. The anomaly was then drilled and trenched, although no report can be located with the information. No further work on the area has since been reported. " 075MNE0014,2,1,"This showing was derived from the CANMINDEX database. No mention of this showing is located in any assessment report and is only a mineral occurrence on a map. In the GSC paper 70-70, the EGO claim group is mentioned to be owned by Shield Resources in 1966." 075MNE0015,3,1,"The CL 25 showing occurs within the Slave Supracrustal Province, Archean in age. The Supracrustal rocks are of the Yellowknife Supergroup, dominated by a volcanic-greywacke-mudstone sequence forming various greenstone belts that cover about one third of the province. Granitoid intrusions make up the bulk of the craton and are grouped as pre-, syn-, and post- Yellowknife Supergroup. In addition, several mafic dykes have intruded the shield, orientated between 140 and 180 degrees. Also present in the regional area are diamondiferous kimberlite pipes that occur along the same general strike as the dyke swarms. The CL 25 showing is situated on the Camsell Lake property which is approximately 20 miles north of the East Arm of Great Slave Lake. The rocks on the Camsell property are volcanics and sediments of the Yellowknife Supergroup which occur as two northeasterly trending belts. These belts have been intruded by glomeroporphyritic leucogabbro/gabbro stocks, gabbro sills and rare leucogabbro sills. Granitic intrusions include dykes and stocks of granodiorites of various compositions and pegmatites of the same phases. All rocks of the area are intruded by north-northwesterly magnetic diabase dykes. Although past mineral exploration was focused on the Cu-Zn potential on the Camsell Lake area, diamond exploration has been the main focus since the first discovery of kimberlites in the Slave. Winspear Resources Inc., Aber Resources, Amarado and Consolidated Newgate started work on the Camsell Lake project in 1993 with a regional airborne Mag/EM survey was completed. Following the survey, samples were collected from two major eskers in the southern portion of the property. In 1994, a ground survey and basal till sampling and diamond drilling was completed." 075MNE0015,4,2,"Results from the 1994 field season included plotting indicator minerals on maps from sample locations to trace back towards the possible source. By combining information from geophysical surveys and sampling results, four drill holes tested two geophysical anomalies. Three drill holes intersected kimberlites. From drill holes 1 and 2 a bulk sample weighing 350.4 kg contained a total of 221 diamonds; 9 were macro- (>0.5 mm) and 212 micro-sized (<0.5 mm). These intersections of kimberlite resulted in the discovery of the first kimberlite pipe on the Camsell Lake Property. " 075MNE0016,5,1,"The CL 174 showing occurs within the Slave Supracrustal Province, Archean in age. The Supracrustal rocks are of the Yellowknife Supergroup, dominated by a volcanic-greywacke-mudstone sequence forming various greenstone belts that cover about one third of the province. Granitoid intrusions make up the bulk of the craton and are grouped as pre-, syn-, and post- Yellowknife Supergroup. In addition, several mafic dykes have intruded the shield, orientated between 140 and 180 degrees. Also present in the regional area are diamondiferous kimberlite pipes that occur along the same general strike as the dyke swarms. The CL 174 showing is situated on the Camsell Lake property which is approximately 20 miles north of the East Arm of Great Slave Lake. The rocks on the Camsell property are volcanics and sediments of the Yellowknife Supergroup which occur as two northeasterly trending belts. These belts have been intruded by glomeroporphyritic leucogabbro/gabbro stocks, gabbro sills and rare leucogabbro sills. Granitic intrusions include dykes and stocks of granodiorites of various compositions and pegmatites of the same phases. All rocks of the area are intruded by north-northwesterly magnetic diabase dykes. Although past mineral exploration was focused on the Cu-Zn potential on the Camsell Lake area, diamond exploration has been the main focus since the first discovery of kimberlites in the Slave. Winspear Resources Inc., Aber Resources, Amarado and Consolidated Newgate started work on the Camsell Lake project in 1993 with a regional airborne Mag/EM survey was completed. Following the survey, samples were collected from two major eskers in the southern portion of the property. In 1994, a ground survey and basal till sampling and diamond drilling was completed." 075MNE0016,6,2,"The CL 174 kimberlite pipe is 150 metres northwest of the CL 25 kimberlite pipe. Its discovery came when drilling to find the extent of the CL 25 pipe was done. The only information on the showing to date is that from news releases stating from drill hole 174-1 a 622.2 kg sample was taken and 284 total diamonds were recovered, with 274 micro- (<0.5 mm) and 10 macro-sized (>0.5 mm)." 075MNE0017,7,1,"The CL 186 showing occurs within the Slave Supracrustal Province, Archean in age. The Supracrustal rocks are of the Yellowknife Supergroup, dominated by a volcanic-greywacke-mudstone sequence forming various greenstone belts that cover about one third of the province. Granitoid intrusions make up the bulk of the craton and are grouped as pre-, syn-, and post- Yellowknife Supergroup. In addition, several mafic dykes have intruded the shield, orientated between 140 and 180 degrees. Also present in the regional area are diamondiferous kimberlite pipes that occur along the same general strike as the dyke swarms. The CL 186 showing is situated on the Camsell Lake property which is approximately 20 miles north of the East Arm of Great Slave Lake. The rocks on the Camsell property are volcanics and sediments of the Yellowknife Supergroup which occur as two northeasterly trending belts. These belts have been intruded by glomeroporphyritic leucogabbro/gabbro stocks, gabbro sills and rare leucogabbro sills. Granitic intrusions include dykes and stocks of granodiorites of various compositions and pegmatites of the same phases. All rocks of the area are intruded by north-northwesterly magnetic diabase dykes. Although past mineral exploration was focused on the Cu-Zn potential on the Camsell Lake area, diamond exploration has been the main focus since the first discovery of kimberlites in the Slave. Winspear Resources Inc., Aber Resources, Amarado and Consolidated Newgate Resources started work on the Camsell Lake project in 1993 with a regional airborne Mag/EM survey was completed." 075MNE0017,8,2,"The CL 186 showing is a diamondiferous kimberlite pipe on the east shore of Snap Lake. Despite the presence of kimberlite boulders, the area gives a low magnetic response due to 100 metre of granite overlying (and masking) the kimberlite pipe. After drilling into kimberlite breccia in 1997, diamond analysis of two bulk samples resulted in a total of 11 diamonds from a 74.2 kg sample and 114 diamonds from a 78.2 kg sample. The two samples produced a total of 42 macro-sized diamonds. " 075MNE0018,9,1,"The Snap Lake Dyke showing occurs within the Slave Supracrustal Province, Archean in age. The Supracrustal rocks are of the Yellowknife Supergroup, dominated by a volcanic-greywacke-mudstone sequence forming various greenstone belts that cover about one third of the province. Granitoid intrusions make up the bulk of the craton and are grouped as pre-, syn-, and post- Yellowknife Supergroup. In addition, several mafic dykes have intruded the shield, orientated between 140 and 180 degrees. Also present in the regional area are diamondiferous kimberlite pipes that occur along the same general strike as the dyke swarms. The Snap Lake Dyke showing is situated on the Camsell Lake property which is approximately 20 miles north of the East Arm of Great Slave Lake. The rocks on the Camsell property are volcanics and sediments of the Yellowknife Supergroup which occur as two northeasterly trending belts. These belts have been intruded by glomeroporphyritic leucogabbro/gabbro stocks, gabbro sills and rare leucogabbro sills. Granitic intrusions include dykes and stocks of granodiorites of various compositions and pegmatites of the same phases. All rocks of the area are intruded by north-northwesterly magnetic diabase dykes. Although past mineral exploration was focused on the Cu-Zn potential on the Camsell Lake area, diamond exploration has been the main focus since the first discovery of kimberlites in the Slave. Winspear Resources Inc., Aber Resources, Amarado and Consolidated Newgate Resources started work on the Camsell Lake project in 1993 with a regional airborne Mag/EM survey was completed." 075MNE0018,10,2,"The Snap Lake Dyke has been intersected 11 times in an area of 1 square km. The dyke, with an average true thickness of 2.47 metres, was bulk sampled with a total of 137.14 kg of kimberlite recovering 401 diamonds, 149 macro- (>0.50 mm) and 252 micro-sized (<0.5 mm)." 075MNE0019,11,1,"The Snap Lake Boulder showing occurs within the Slave Supracrustal Province, Archean in age. The Supracrustal rocks are of the Yellowknife Supergroup, dominated by a volcanic-greywacke-mudstone sequence forming various greenstone belts that cover about one third of the province. Granitoid intrusions make up the bulk of the craton and are grouped as pre-, syn-, and post- Yellowknife Supergroup. In addition, several mafic dykes have intruded the shield, orientated between 140 and 180 degrees. Also present in the regional area are diamondiferous kimberlite pipes that occur along the same general strike as the dyke swarms. The Snap Lake Boulder showing is situated on the Camsell Lake property which is approximately 20 miles north of the East Arm of Great Slave Lake. The rocks on the Camsell property are volcanics and sediments of the Yellowknife Supergroup which occur as two northeasterly trending belts. These belts have been intruded by glomeroporphyritic leucogabbro/gabbro stocks, gabbro sills and rare leucogabbro sills. Granitic intrusions include dykes and stocks of granodiorites of various compositions and pegmatites of the same phases. All rocks of the area are intruded by north-northwesterly magnetic diabase dykes. Although past mineral exploration was focused on the Cu-Zn potential on the Camsell Lake area, diamond exploration has been the main focus since the first discovery of kimberlites in the Slave. Winspear Resources Inc., Aber Resources, Amarado and Consolidated Newgate Resources started work on the Camsell Lake project in 1993 with a regional airborne Mag/EM survey was completed." 075MNE0019,12,2,"The Snap Lake Boulder showing is 6 boulder samples taken on the northwest shore of Snap Lake that had diamonds in them. The total weight of the samples taken was 248.18 kg in which 637 diamonds were found, 202 macro- (>0.50 mm) and 435 micro-sized (<0.5 mm)." 075MNW0003,13,1,"Regional: The TALL claims are located on the western side of the Courageous Lake Archean Greenstone belt which is a 60 km long north south striking volcanic belt within the Yellowknife Supergroup. Property: The TALL property is composed of volcanics which are overlain to the east by Yellowknife Supergroup sediments and undermined to the west by granites. Showing: Noranda drilled six airborne electromagnetic conductors in 1980 some of which represented massive sulphide zones in felsic tuffs. One of the holes, T-4-80, tested a 300 - 400 metre EM conductor with coincident mag which contained a 1.02 metre zone at a felsic pyroclastic-mafic tuff contact. This zone contained massive pyrrhotite and pyrite as well as traces of chalcopyrite and 0.67% zinc in sphalerite. No further work was recommended." 075MNW0016,14,1,"Regional: The CAM property lies in the central, volcanic portion of the Camsell Lake Greenstone Belt of Archean aged Yellowknife Supergroup volcanic and sedimentary rocks of the Slave Province. Property: volcanic rocks in the area are composed of locally pillowed basalts and andesites with some felsic tuff beds. These units are intruded by a well-differentiated gabbro-anorthosite complex which also strikes NE-SW. The volcanic rocks are cut by fairly prominant shears which run both parallel and at acute angles to the volcanics. The entire package is underlain by Proterozoic granites. Showing: The property was originally staked in 1957 as the LIZ group and optioned to Cominco who did geophysics, trenching and drilling in 1958, finding fair copper values. The property was then re-staked in 1964 as the CAM group and more geophysical work was done. In 1966 the property was optioned by Hurley River Mines who did more geophysics and 2,607 ft. of drilling which resulted in up to 5.2 feet grading 0.47% Cu and minor zinc. In general the mineralization consists of fairly massive po. with minor associated cpy, and traces of sph. Two major types of mineralization have been observed, both occuring in shear zones in the altered volcanics, near and parallelling the volcanic-gabbro contact. Type 1 - Cpy-po-py bearing altered andesite and associated massive mineralized quartz. Type 2 - Fine grained po-mt-py disseminated along shear zones in the altered andesite. The cpy type of mineralizaion occurs at several localities on the property." 075MNW0035,15,1,"Regional: The PEP property lies in the central, volcanic portion of the Camsell Lake Greenstone Belt of Archean aged Yellowknife Supergroup volcanic and sedimentary rocks of the Slave Province. Property: volcanic rocks in the area are composed of locally pillowed basalts, andesites and dacites with some felsic tuff beds. These units are intruded by a well-differentiated gabbro-anorthosite complex which also strikes NE-SW. The volcanic rocks are cut by fairly prominant shears which run both parallel and at acute angles to the volcanics. The entire package is underlain by Proterozoic granites. Showing: The author could not find the early work done on this showing though the property was first prospected in the mid 1960s. The only other work done on the claim was in 1971 when Anglo United Development ran a ground geophysical survey over the prospect and drilled three diamond drill holes through the shear to test a coincident anomaly at depth. In general the mineralization occurs in a shear near to and parallelling the volcanic-gabbro contact and consists of fairly massive po. with minor associated py and cpy. The results were poor with copper values up to 0.27%, and zinc up to 0.22%." 075MNW0036,16,1,"During 1948, 345 feet of diamond drilling was recorded on the SECUM11 claim by J. McAvoy for Cunaxa Mining Ltd. This property is located in the Courageous Lake area of the Yellowknife Supergroup in a peninsula in McKay Lake. Some pyrite, pyrrhotite, chalcopyrite and trace galena mineralization was reported, however no further work has been recorded. Drilling was also completed on the adjacent KM12 claim." 075MNW0037,17,1,"During 1948, 500 feet of diamond drilling was recorded on the KM 12 claim by J. McAvoy for Cunaxa Mining Ltd. This property is located in the Courageous Lake area of the Yellowknife Supergroup in a peninsula in McKay Lake. Pyrite, pyrrhotite, chalcopyrite and galena were reported, however no further work has been recorded. Drilling was also completed on the adjacent SECUM 11 claim." 075MNW0046,18,1,"Known as the Roma and Jeta claims in 1945-1950, held by Homer YK mines, no assessment report found. Known as the Don claims in 1958, held by North Goldcrest mines, no assessment report found, and in 1973 (also Don claims) held by Golden Ram resources, no report found." 075MNW0047,19,1,"Regional: The Courageous-MacKay Lake Greenstone Belt is one of the twenty volcanic belts within the Slave Structural Province which make up the volcanic portion of the Yellowknife Supergroup. The greenstone belt is an eastward facing, homoclinal sequence of volcanic rocks overlain by a thick sedimentary group. The Matthews Lake Volcanic Complex is composed of pyroclastic and volcanoclastic units of rhyodacite to rhyolite composition. Mafic flows and interflow sediments make up a minor portion of this complex. All of the gold showings on the Tundra property are associated with the volcanics of this complex. Property: The Matthews Lake Volcanic Complex may be divided into two volcanic cycles characterezed by mafic flows to felsic pyroclastic successions. The top of each cycle contains localized gold mineralization within felsic ash and lapilli tuff in assiciation with blue quartz veins and arsenopyrite mineralization. Showing: The main BERTHA 5 showing is descibed as felsic lapilli tuff with 1% py., and 1% aspy., foliated at 342 degrees and dipping 85 degrees to the west. The surounding geochem samples are described as having up to 15% blue black quartz veining and up to 10 % banded aspy. Chlorite rich bands are also noted in the logs. A second, satelite showing 150 m to the NW is descrbed as wacke, near a mafic tuff contact with simmilar minerology to the main showing." 075MNW0048,20,1,"Regional: The Courageous-MacKay Lake greenstone belt is one of the twenty volcanic belts within the Archean Slave Structural Province which make up the volcanic portion of the Yellowknife Supergroup. The greenstone belt is an eastward facing, homoclinal sequence of volcanic rocks overlain by a thick sedimentary group. The Matthews Lake Volcanic Complex is composed of pyroclastic and volcanoclastic units of rhyodacite to rhyolite composition. Mafic flows and interflow sediments make up a minor portion of this complex. All of the gold showings on the Tundra property are associated with the volcanics of this complex. Property: The Matthews Lake Volcanic Complex may be divided into two volcanic cycles characterized by mafic flows to felsic pyroclastic successions. The top of each cycle contains localized gold mineralization within felsic ash and lapilli tuff in association with blue quartz veins and arsenopyrite mineralization. Showing: Assessment report 082777 describes three samples which graded over 500 ppb gold. These are of felsic and intermediate ash tuff beds with up to 20% quartz veining and up to 3% aspy., 3% py., trace cpy., and 5 % epidote. The showings all had foliation striking from 338 to 004 degrees and dipping steeply eastwards. " 075MNW0049,21,1,"Regional: The Courageous-MacKay Lake Greenstone Belt is one of the twenty volcanic belts within the Slave Structural Province which make up the volcanic portion of the Yellowknife Supergroup. The greenstone belt is an eastward facing, homoclinal sequence of volcanic rocks overlain by a thick sedimentary group. The Matthews Lake Volcanic Complex is composed of pyroclastic and volcanoclastic units of rhyodacite to rhyolite composition. Mafic flows and interflow sediments make up a minor portion of this complex. All of the gold showings on the Tundra property are associated with the volcanics of this complex. Property: The Matthews Lake Volcanic Complex may be divided into two volcanic cycles characterezed by mafic flows to felsic pyroclastic successions. The top of each cycle contains localized gold mineralization within felsic ash and lapilli tuff in assiciation with blue quartz veins and arsenopyrite mineralization. Showing: Assessment report 082777 describes one sample gradomg 1040 ppb gold. This is of a felsic lapilli tuff bed with quartz veining and up to 1% py. The zone is 1 m wide." 075MNW0050,22,1,"Regional: The Courageous-MacKay Lake Greenstone Belt is one of the twenty volcanic belts within the Slave Structural Province which make up the volcanic portion of the Yellowknife Supergroup. The greenstone belt is an eastward facing, homoclinal sequence of volcanic rocks overlain by a thick sedimentary group. The Matthews Lake Volcanic Complex is composed of pyroclastic and volcanoclastic units of rhyodacite to rhyolite composition. Mafic flows and interflow sediments make up a minor portion of this complex. All of the gold showings on the Tundra property are associated with the volcanics of this complex. Property: The Matthews Lake Volcanic Complex may be divided into two volcanic cycles characterezed by mafic flows to felsic pyroclastic successions. The top of each cycle contains localized gold mineralization within felsic ash and lapilli tuff in assiciation with blue quartz veins and arsenopyrite mineralization. Showing: The HARE 8 showing is a single chip sample taken from an in situ frost heave by Noranda in 1988 (assessment report #82777). The sample was of a felsic ash tuff with 75% aphanitic quartz, 10% sericite, 5% biotite, 5% chlorite, 2% py, and 1% po. The sample graded 1150 ppb." 075MSE0001,23,1,"Regional: The Susu Lake Cu showing is situated within the Indian Mountain greenstone belt which comprises mainly Archean Yellowknife Supergroup supracrustal rocks. The belt is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bounded on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property: The property in which this showing occurs, lies approximately 8 miles west of Susu Lake. It comprises a volcanic belt that is part of the larger Indian Mountain greenstone belt. The volcanic belt is dominated by rhyolites with quartz-biotite-cordierite schists. Deformation in the area includes shearing and brecciation. Intrusions of quartz veins are also noted. Showing: The Susu Lake Cu showing occurs in a brecciated shear zone that hosts disseminated chalcopyrite and bornite. Mineralization is largely hosted by rhyolites, but also occurs in neighboring quartz-biotite-cordierite schists. Reserves were calculated at 142,500 tons grading 0.95% Cu in 1967 from 9 diamond drill holes that were drilled by Indian Mountain Metal Mines. No other work on the showing has been recorded to date although in Canadian Mineral Deposits Not Being Mined in 1989, it was mentioned the property had been sold to Ego Resources. " 075MSE0002,24,1,"The BB prospect is one of three related volcanogenic massive sulphide occurrences situated in the Indian Mountain greenstone belt in the southern Slave structural province. All stratified rocks have been mapped as belonging to the Archean Yellowknife Supergroup. The base of the stratigraphic sequence in the vicinity of the deposits comprises a series of mafic tuffs with minor, massive and pillowed mafic flows. The bottom of this unit is migmatized. Overlying this mafic base are intermediate tuffs and flows and then a felsic unit including massive rhyolite, intermediate to felsic coarse pyroclastics, tuff, lapilli tuff and tuff breccia. Sulphide deposits are hosted by a 1 - 10 metre thick unit of carbonate-rich exhalite and pyritic cherty tuff, overlying or near the top of the felsic unit. The stratigraphic succession is completed by greywackes and argillites. All stratified rocks have been metamorphosed to middle amphibolite facies. The BB massive sulphide deposit consists of a series of closely spaced lenses interbedded with and grading into highly altered siliceous limestone which is probably a carbonate-rich exhalite. Layers of coarse grained pyrite and sphalerite are interbedded with layers of coarse grained pyrite and bands of massive, fine-grained sphalerite. Galena occurs as small grains and blebs within massive pyrite and sphalerite and as rims on host rock fragments in the latter. Small blebs of chalcopyrite are scattered throughout the deposit. Associated metallic minerals include minor amounts of chalcopyrite, pyrrhotite, marcasite, magnetite and tetrahedrite. " 075MSE0002,25,2,"Reserves were calculated for the BB showing and several values were reported, increasing in tonnage as the number of drill holes increased. By the end of 1952, over 23,000 feet total drilling on the property had been completed and reserves were calculated at 924,000 tons grading 10.3% Zn, 0.85% Pb and 3.45 oz/ton Ag. The BB Lake Copper zone is situated within a discordant alteration pipe/stringer zone underlying the BB and Kennedy Lake stratiform mineralization. Chalcopyrite and pyrrhotite occur as stringers, layers and seams in two bands 8 - 13 metres wide and up to 200 metres long. Sulphides in the higher grade portions of these bands are accompanied by a black, unidentified amphibole. The alteration pipe within which this stringer mineralization is located is zoned. An inner, intensely altered zone consists of garnet, anthophyllite, cummingtonite, cordierite, sericite and sillimanite in a less intensely altered envelope which is characterized more by biotite, quartz and chlorite. " 075MSE0002,26,3,"Work on the BB showing began in 1948 when the property of which the showing lies was discovered for McAvoy and was optioned off to Hollinger Gold Mines. Diamond drilling was started on the property the following year. Over 15,825 feet of core was drilled and reserves were calculated at 270,000 tons of ore averaging 15.68% Zn, 1.67% Pb and 5.21 oz./ton Ag to a depth of 400 feet. In 1951, under the ownership of Indian Mountain Metal Mines Ltd., reserves were re-calculated after drilling to the 800 foot horizon. Information of the drilling program done in 1951, gave good enough results for another 25,000 feet of drilling to be proposed for the following year. By the end of 1952, the BB zone had been drilled to the extent of 23,000 feet and the amount of reserves for the zone increased to 924,000 tons. Plans were under consideration for underground development and mill construction for 1953, but were not implemented. In 1965, extensive electromagnetic and magnetometer surveys were done by Indian Mountain Metals Mines Ltd. to re-examine the entire volcanic belt. In 1966, drilling was done on anomalies that were outlined the year before in the Kennedy Lake area. After 1966, no work on the BB zone has been reported. The property went to lease in 1974 and in 1979 the property was optioned to Ego Resources. The Kennedy Lake Zone which lies under Kennedy Lake is described in AR 061728 as the western extension of the BB zone although it is separated from the latter by a barren zone. The zone is not exposed at the surface although drilling outlined it to be 120 feet long with a maximum width of 21 feet. The ore is similar in all respects to that of the BB zone. Reserves for the Kennedy Lake zone were calculated at 43,000 tons grading 7.3% Zn, 1.1% Pb and 4.0 oz./ton Ag." 075MSE0005,27,1,"The COTTONGRASS Au showing lies in the Archean Slave Structural Province, in the Indian Mountain Greenstone belt. It is hosted within rhyolite rocks approximately 2 metres wide, that have been metamorphosed to granulite facies. The sample is defined by a single grab sample that assayed 680 ppb of Au." 075MSE0006,28,1,"Regional The Dawn & Gem-1 showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills from felsic to mafic in composition. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing Mineralization is within rhyolitic volcanic flows and occurs mainly as sphalerite, galena and silver. Its occurrence can be massive, disseminated or as blebs within the host rock. Some minor chalcopyrite, pyrite and arsenopyrite are also associated with the mineralization. Assay results from 3 diamond drill holes with total length of 2159 feet, range from 0.90% Pb over 2.5 feet to 0.97% Pb over 2.5 feet and 0.41% Zn over 2 feet to 6.01% Zn over 1.5 feet. The silver also had assay results but no measurements are given and thus not reported." 075MSE0006,29,2,"Exploration Work in the area began after the discovery of the BB zone in 1948, just south of the Dawn & Gem-1 showing. The area was staked in 1957 and 1958 by the McAvoy Option Group. The property was then optioned off to Mount Wright Iron Mines Company Ltd. in 1958 and in 1959 they drilled 39 holes in the showing vicinity. An EM survey was done on the showing in 1958. In 1966, more geophysical surveys were completed over the showing as well as 8 holes were drilled by Indian Mountain Metal Mines Ltd. From this drilling 3 holes intersected mineralization and the define the showing. No further work was completed on the area until 1992 when Taiga Consultants Ltd. on behalf of Royal Oak Mines, Asamera Minerals Inc. and Nebex Resources Ltd. did an EM survey over the showing." 075MSE0007,30,1,"Regional The Dawn & Gem-2 showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. It is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills from felsic to mafic in composition. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing Mineralization is found within rhyolitic volcanic flows and occurs mainly as chalcopyrite, sphalerite and silver. Its occurrence can be massive, disseminated or as blebs within the host rock. Some minor galena, pyrite and arsenopyrite are also associated with the mineralization. Diamond drilling from one hole, AR 017123, ran assay results ranging from 0.2% Cu over 4 feet to 0.88% Cu over 3 feet and 0.67% Zn over 5 feet to 1.66% Zn over 4 feet. From AR 017122, 11 holes were drilled with a total of 1791 feet, however only 8 holes intersected mineralization. Assay results from these holes ranged from 0.27% Cu over 48 inches to 3.98% Cu over 24 inches. The silver also had assay results but no measurements are given and thus not reported." 075MSE0007,31,2,"Exploration Work in the area began after the discovery of the BB zone in 1948, just south of the Dawn & Gem-2 showing. The area was staked in 1957 and 1958 by the McAvoy Option Group. The property was then optioned off to Mount Wright Iron Mines Company Ltd. in 1958 and in 1959 they drilled 8 holes on the showing. An EM survey was done on the showing in 1958. In 1966, more geophysical surveys were completed over the showing as well as more drilling in the showing vicinity by Indian Mountain Metal Mines Ltd. No further work was completed on the area until 1992 when Taiga Consultants Ltd. on behalf of Royal Oak Mines, Asamera Minerals Inc. and Nebex Resources Ltd. did an EM survey over the showing." 075MSE0008,32,1,The Plex Lake showing is a CANMINDEX showing and is found on the map 1198A as a cp occurrence. No mention of this showing is made in any assessment report. 075MSE0009,33,1,The Susu Lake North showing is a canmindex showing located on the COTTONGRASS Claims owned by BHP-Utah Mines Ltd. in the late 1980s. They are located on the maps in assessment reports 082714 and 083069 but no mention of the showing is made in the written portion of the reports. The showing is considered a reconnaissance showing and is recorded from the assessment report maps with an assay result of 2859 ppm of Cu. 075MSE0010,34,1,The 5 Mi West of Susu Lake showing is a CANMINDEX showing. It is located on the GSC 1198A map as a chalcopyrite occurrence and is covered by ground geophysics in assessment report 017125. 075MSE0017,35,1,"The Brislane Lake-1 showing is defined by five grab samples taken by Lebel Oro Mines Ltd. from the Indian Mountain Lake area. The area is within the Slave Structural Province, Archean in age. The samples returned assay results of 0.75% Cu, 0.65% Cu, 0.23% Cu, 2.35% Cu, and 0.27% Cu." 075MSE0018,36,1,"The Brislane Lake-2 showing is defined by a single grab sample from the Indian Mountain Lake area. The sample is part of the Slave Province, Archean in age. Assay results are given as 0.03 oz. Au and 0.45% Cu." 075MSE0019,37,1,"Regional The BRI 8 showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property The BRI 8 showing lies in the south-central part of the property and was prospected for copper/gold occurrences. A quartz diorite or tonalite intrusion underlies this area of the property and is usually massive, medium- to coarse-grained, creamy buff, and composed of quartz, feldspar, biotite and hornblende. The tonalite is seen to intrude the mafic volcanics of the area. Showing The mineralization of the BRI 8 showing is in well fractured, altered quartz diorite. It occurs as chalcopyrite and gold with minor pyrite and pyrrhotite. The showing was explored in the 1950s by four trenches and smaller pits which were dug and blasted on a series of parallel mineralized fracture zones. In 1992, in a joint venture between Royal Oak Mines, Asamera Minerals and Nebex Resources, 16 samples from frost-heaved boulders and the old trenches were taken. Anomalous copper values ranging from 912 ppm to 3.42% over narrow widths were reported. Two samples also returned anomalous gold values of 0.086 oz/t Au and 837 ppb Au. " 075MSE0020,38,1,"Regional The Taco Island showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property The Taco Island showing lies in the south part of Brislane Lake. The property was prospected for copper/gold occurrences. Most of the east half of the island is underlain by hornblende-cummingtonite-biotite-garnet schist while the west half is underlain by a hornblende schist. Two narrow lenses of diopside-bearing rocks occur in the centre of the island and near the north tip. Showing The mineralization of the Taco Island showing is in two different lithologies - in the diopside-garnet skarn and in the hornblende-cummingtonite-biotie-garnet schist. The mineralization occurs as disseminated blebs and fine stringers of pyrrhotite, pyrite and chalcopyrite. In 1992, in a joint venture between Royal Oak Mines, Asamera Minerals and Nebex Resources 8 chip samples from higher grade sulfide occurrences on the island were taken. The best copper values reported were 5.58% Cu over 0.6 m and 5.69% Cu over 1.0 m. Anomalous gold values also reported were 147 ppb Au and 740 ppb Au." 075MSE0021,39,1,This is a CANMINDEX showing located as an occurrence on the Mineral Occurrence Overlay Map 75M02. No mention of this showing is made in any assessment report or government report. 075MSE0022,40,1,This is a CANMINDEX showing located as an occurrence on the Mineral Occurrence Overlay Map 75M02. No mention of this showing is made in any assessment report or government report. 075MSE0023,41,1,The BRI 6 showing is represented by 11 grab samples taken from mafic volcanics south of Brislane Lake. The volcanics are part of the Indian Mountain greenstone belt and are Archean in age. The assay results for the grab samples ranged from 4274 ppm Cu over 0.60 m to 7.06% Cu over 1.10 m. 075MSE0024,42,1,The BRI 3 showing is a reconnaissance showing represented by 4 grab samples taken from mafic volcanics north of Brislane Lake. The volcanics are part of the Indian Mountain greenstone belt and are Archean in age. The assay results for the grab samples ranged from 2832 ppm Cu over 0.50 m to 2.09% Cu over 0.40 m 075MSE0025,43,1,This showing is a CANMINDEX showing and is located as an occurrence on the Mineral Occurrence Overlay Map 075M02. No mention of this showing is in any assessment report or government report. 075MSE0026,44,1,This showing is a CANMINDEX showing and is a copper occurrence on the Mineral Occurrence Overlay Map 75M02. No mention of this showing is made in any assessment report or government report. 075MSE0027,45,1,The BRI 5 showing is represented by 8 chip samples taken from mafic volcanic frost heave boulders north of Brislane Lake. The volcanics are part of the Indian Mountain greenstone belt and are Archean in age. The assay results for the grab samples ranged from 2806 ppm Cu over 0.80 m to 2.41% Cu over 0.70 m. 075MSE0028,46,1,"The JUF showing is a urainium occurrence in the Herriman Lake area. Found within a biotite schist within granitic rocks, two samples assayed 0.033% and 0.15% U3O8. The showing was discovered prior to 1952 by J. Woolgar and no further work on the showing has been recorded since." 075MSE0029,47,1,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Mackenzie. Showing is located 0.5 miles west of Susu Lake. The only records of the showing are from GSC map 1198A in which it occurs as a rusty zone with pyrite and pyrrhotite and on the Mineral Occurrence Overlay 75M/02 in which it is shown as a copper prospect. 075MSE0030,48,1,The COTTONGRASS Cu showing is defined by a single grab sample from Archean rhyolites in the Indian Mountain Greenstone belt. The rhyolites have been metamorphosed to granulite facies and are in contact with quartz-biotite schists where the mineralization is apparent. The sample assayed 2580 ppm Cu. 075MSE0031,49,1,The Susu Lake West 2 showing is a canmindex showing and is only recorded on the Mineral Occurrence Overlay map as a copper prospect showing. No mention of this showing was found in any assessment reports or papers. 075MSE0032,50,1,"Regional The HO 16 showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing This showing is defined by 3 drill holes with a combined total of 992 feet which intersected narrow bands of chalcopyrite, sphalerite and pyrite in sheared dacite-andesite volcanics. Best intersections were 1.04% Cu and 1.02 oz/ton Ag over 2 feet and 0.86% Cu over 4 feet." 075MSE0032,51,2,"Exploration The area in which the HO 16 claim lies was first staked in 1949 by the McAvoy Option Group. In 1959, three drill holes were drilled to a depth of 992 feet. No other work has been performed on the showing, however in 1992, a joint venture between Royal Oak Mines, Asamera Minerals and Nebex Resources did some reconnaissance sampling nearby." 075MSE0033,52,1,"Regional The Pb No. 5 showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing This showing is defined by 3 drill holes with a combined total of 180 feet which intersected small amounts of chalcopyrite in a rhyolite volcanic enclosed in a sediment. No assay results have been recorded. Exploration During the winter of 1950, Captain Yellowknife Gold Mines Ltd. drilled three diamond drill holes on the PB 5 claim east of Indian Mountain Lake." 075MSE0034,53,1,"Regional The FLO showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing The FLO showing is on the west of the northern part of Brislane Lake, owned by J. Herriman in 1956. In November of that year a hole was drilled to a depth of 501 feet where chalcopyrite and pyrite were observed within a narrow quartz vein. No other work has been completed on the showing although in 1992 a joint venture between Royal Oak Mines, Asamera Minerals and Nebex Resources did reconnaissance sampling in the immediate vicinity." 075MSE0039,54,1,"The Kennedy Lake West prospect is one of three related volcanogenic massive sulphide occurrences situated in the Indian Mountain greenstone belt in the southern Slave structural province. All stratified rocks have been mapped as belonging to the Archean Yellowknife Supergroup. The base of the stratigraphic sequence in the vicinity of the deposits comprises a series of mafic tuffs with minor, massive and pillowed mafic flows. The bottom of this unit is migmatized. Overlying this mafic base are intermediate tuffs and flows and then a felsic unit including massive rhyolite, intermediate to felsic coarse pyroclastics, tuff, lapilli tuff and tuff breccia. The stratigraphic succession is completed by greywackes and argillites. All stratified rocks have been metamorphosed to middle amphibolite facies. Mineralization of the Kennedy Lake West prospect occurs as chalcopyrite with minor amounts of silver and sphalerite. The chalcopyrite is associated with amphibole and garnet rich bands of the volcanics and is disseminated in nature. The mineralization can be traced discontinuously over 2,000 feet between BB Lake and Kennedy Lake. Pyrrhotite and pyrite are associated with the chalcopyrite in the low grade sections at approximately a 1:1 ratio." 075MSE0039,55,2,"The Kennedy Lake West prospect is located on the VOO claims which were first staked by James McAvoy in 1951. In 1952, 6 diamond drill holes were drilled on the VOO claims totalling 2,987 feet. In 1959, trenching was carried out and 757 feet were drilled in 10 holes. In 1965, Indian Mountain Metal Mines Ltd. located an anomaly under Kennedy Lake which they drilled into in 1966. The drilling intersected a zone of low grade disseminated chalcopyrite up to 120 feet wide. This Kennedy Lake West copper zone has been estimated to contain 1,000,000 tons grading 0.90% Cu over a length of 835 feet. In 1966, Indian Mountain Metal Mines Ltd. optioned the VOO claims and drilled 9 holes and intersected the westward extension of the copper zone. The claims subsequently lapsed and the ground was restaked by K. J. McDonald in May 1972 and later that month transferred to Indian Mountain Metal Mines Ltd. Exploration work included geological mapping and a ground EM survey. Channel samples averaged 0.5% Cu and 0.94 oz./ton Ag over a width of 25 feet. In 1974, a tonnage figure for the Kennedy Lake West zone was reported as 1,500,000 tons grading 0.62% Cu, including a higher grade core of 612,000 tons grading 1.12% Cu. In 1979, Indian Mountain Metal Mines Ltd. amalgamated to form Initiative Explorations Inc. The property was then optioned off to Domego Resources Ltd. in the early 1980s, who still held the claims in summer 1998." 075MSE0040,56,1,This VOY showing is from Mineral Occurrence Map 75M02 as a copper prospect and was converted as a CANMINDEX showing. No mention of this showing is found within any other assessment report. 075MSE0041,57,1,"Regional The Benny Bay Zone showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing The Benny Bay Zone is defined by two holes drilled by Indian Mountain Mines Ltd. in 1974 which intersected a zinc rich zone. Sphalerite with pyrite and pyrrhotite were seen within a narrow stratiform zone within the upper calcareous fragmental member of the felsic sequence. The best reported assay value from the two holes was 7.9% Zn over 37 cm. No other work on the Benny Bay Zone has been recorded since the 1974 drilling, although in AR 083129 a summary of the zone is stated. " 075MSE0042,58,1,"Regional The Northern Zinc Zone showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing Mineralization is found within quartz-carbonate stockworks in volcanic flows and occurs as sphalerite, chalcopyrite and lead. Its occurrence can be massive, disseminated or as blebs within the host rock. Garnets occur with the mineralization as well as some minor pyrrhotite, pyrite and silver. Assay results from 2 holes drilled 180 m apart along strike, intersected respectively 7.3 m averaging 7.53% Zn and 4.88 m averaging 4.83% Zn." 075MSE0042,59,2,"Exploration Work in the area began after the discovery of the BB zone in 1948, just south of the Northern Zinc Zone showing. The area was staked in 1957 and 1958 by the McAvoy Option Group. The property was then optioned off to Mount Wright Iron Mines Company Ltd. in 1958 and in 1959 they drilled 4 holes on the showing. An EM survey was done on the showing in 1958. In 1966, more geophysical surveys were completed over the showing as well as more drilling by Indian Mountain Metal Mines Ltd in 1974. No further work was completed in the area until 1992 when Taiga Consultants Ltd. on behalf of Royal Oak Mines, Asamera Minerals Inc. and Nebex Resources Ltd. reported values from two drill holes from previous work done on the claim in 1974." 075MSE0043,60,1,"Regional The No. 2 Copper Zone showing is situated within the Indian Mountain greenstone belt which is mainly Archean Supracrustal rocks. Composed of volcanic and sedimentary rocks, it is as much as 15 miles wide and extends 40 miles north from Great Slave Lake. The belt is bound on the east and west by granitic and migmatitic rocks but has a core of relatively low grade metamorphic rocks(Heywood and Davidson 1969). The belt is seen to lie on deformed granitoid rocks in some places and in others to be intruded by granitic plutons of closely related age. Property Rocks in the property area are almost entirely of volcanic origin and consist of flows, pyroclastics, and associated dykes and sills. The rocks of the property have been folded, striking approximately north-south, and are crosscut by a fault that is directly north of the showing. Showing Mineralization is found within volcanic flows and occurs mainly as chalcopyrite, sphalerite and silver. Its occurrence can be massive, disseminated or as blebs within the host rock. Garnets occur with the mineralization as well as some minor galena, pyrite and arsenopyrite. Assay results from 15 drill holes with a total of 3306 feet drilled, range from 0.30% Cu over 12 inches to 6.15% Cu over 48 inches and 0.30% Zn over 36 inches to 1.26% Zn over 48 inches. The silver also had assay results but no measurements are given and thus not reported. " 075MSE0043,61,2,"Exploration Work in the area began after the discovery of the BB zone in 1948, just south of the No. 2 Copper Zone showing. The area was staked in 1957 and 1958 by the McAvoy Option Group. The property was then optioned off to Mount Wright Iron Mines Company Ltd. in 1958 and in 1959 they drilled 15 holes on the showing. An EM survey was done on the showing in 1958. In 1966, more geophysical surveys were completed over the showing as well as more drilling by Indian Mountain Metal Mines Ltd. No further work was completed on the area until 1992 when Taiga Consultants Ltd. on behalf of Royal Oak Mines, Asamera Minerals Inc. and Nebex Resources Ltd. did an EM survey over the showing." 075MSE0044,62,1,"No claims found to be associated with this showing, quite possibly a GSC mapping find. No exploration company assessment report was found covering the showing. The showing was converted from CANMINDEX." 075MSE0045,63,1,The Brislane Lake showing is a CANMINDEX showing. No record of this showing is made in any assessment report. 075MSW0011,64,1,"In 1966, Precambrian Mining Services, on behalf of Anglo United Development Corporation and (according to NMI) Northgate Exploration Limited, conducted a regional exploration program known as Project Circle in the Camsell - Rivett Lakes greenstone belt, focussed on the volcanic-sediment contact. Reconnaisance HLEM and magnetic surveys, followed by geological mapping in areas of detected conductors, revealed a number of targets deemed worthy of follow-up. Not all surface sampling results are provided in the submitted Assessment Reports. Five drill holes in 1967 tested targets at the NW end of Lac Sans Disant, for which there is no surface information in the Reports, while the C-6, C-3 and P-2 targets, deemed the most interesting in conclusions to the final 1966 report, were not drill-tested. The Q4 occurrence is defined by one drill hole which cut 0.26% Zn over 3 feet, and a number of 3 ft and 6 ft sections which assayed 0.10 and 0.15% Zn. Another hole testing conductor O1, about 500 m to the NE, yielded a 10 ft section of 0.10 % Zn." 075MSW0012,65,1,"The Tip and Nut are possibly a restaking of the Roc claims (NMI 075M05CU 003). Regional: The property is located near the center of a narrow 70 km long NNE trending belt of Archean Yellowknife Supergroup, volcanic and sedimentary rocks within the Slave Province. The belt, known as the Camsell Lake Belt forms the eastern limb of a synclinal fold cored by Archean biotite-muscovite granites.(GSC map 738-A) Property: The property lies on a contact between meta-volcanics to the east, and meta-sediments to the west. The volcanics on the property include mafic to felsic volcanic cycles younging to the and including intervals of tuff, interflow sediments and sulphidic exhalites and rhyolite domes. Overlying the volcanics are typical Yellowknife group amphibolite grade turbidites. The showing occurs 100 feet from a shear zone near the volcanic sediment contact. " 075MSW0012,66,2,"Showing: The TIP showing on the KIM #1 claim was discovered in 1949 by prospectors for a syndicate headed by W.J. McDonough. The property was subsequently staked by a number of individuals and companies including Tailsman who drilled the showing in 1971 finding gold bearing vein up to f feet thick. In 1984 J. R. Woolgar did a soil chemistry and VLF survey over the property as well as mapping and chip sampling. The Tip gold showing is comprised of a mineralized quartz vein in a chlorite, amphibole schist striking at 35 degrees and dipping steeply. The vein which is 20 cm wide on surface and up to 1 m wide in drilling is exposed over 35 meters of trenching and has locally abundant pyrite with minor arsenopyrite, chalcopyrite, galena, and visible gold. Trench samples graded up to 9.082 oz/t Au over 15 cm, and one grab sample ran 35.55 oz/ton. The host amphibolite did not carry gold. The host rock to the east of the vein consists of meta-basalts and meta-andesites with locally well developed pillows. The host rock to the west consists of meta-sediments which are not exposed. Several other gossans, shears and quartz veins have been sampled on the property with no notable results." 075MSW0015,67,1,"Regional: The SAN property was located in the southeastern Slave Province, near the center of a narrow, 70 km long, NNE trending belt of Archean volcanic and sedimentary rocks belonging to the Yellowknife Supergroup. This belt, known as the Camsell Lake Belt, forms the eastern limb of a synclinal fold cored by Archean biotite-muscovite granites (GSC Map 738-A). Showing Area: The area is underlain by rhyolite, dacite, and slaty tuff of amphibolite facies. An EM survey was conducted in the spring of 1966 by Precambrian Mining Services for Anglo United and Northgate Exploration. Later that summer the anomolies and pre-existing trenches were drilled. The zone of interest is approximately 1 km long and 20 m wide (Northern Miner, Aug 25, 1966, p3). " 075MSW0015,68,2,"Showing: Anomoly C-3 consists of a warped sulphide lens striking ENE and dipping steeply to the north in dacite and slaty tuff. The very fine grained laminated sulphides include po and lesser sph, with py. nodules and some cpy. The C3 zone drilling assayed up to 0.4%Cu and 2.4% Zn. Anomoly C-7 contains very fine grained po., with coarse fracture fillings of po., in a rhyolite outcrop. The C7 zone drilling assayed up to 1.0% Zn and 0.5% Cu. Anomoly C-6 is located near the contact of an erregular north striking diorite dyke which dips 55 degrees east. The mineralized zone contains po., cpy. and pentlandite. The C-6 drilling assayed up to 1.03% Ni. and 0.85% Cu. " 075MSW0038,69,1,"Regional: The LEN showing is situated within the Camsell Lake Belt of volcanic and sedimentary rocks of the Archean Yellowknife Supergoup of the Slave Province. The 80 km long Camsell Lake Belt is a north east extension of the larger Campsell River belt. Property: In 1947 Burgess-Yellowknife-Kirkland Mines Ltd. drilled 8 diamond drill holes on the property for a total of 2009 feet. The results were evidently disappointing and no further work was done. No assays are available. In 1962 the property was re-staked bu A.V. Giauque and J.E. Sullivan who did geophysics and trenched the best of the conductors. Apparently visible gold was seen and one of the trench samples graded .07 oz/ton Au. Showing: Drill logs and regional mapping show the host to be a sheared, locally feldspar porphyritic, andesite with quartz veining and up to 1% pyrite, pyrrhotite and chalcopyrite. A site visit by W.R.A. Baragar however described a quartz vien in a quartz feldspar porphyry interlayered with meta-basalts of the Yellowknife group(GSC paper 63-9). The sources did agree that the main showing consisted of a less than 1 foot wide quartz vein in a massive sheared porphyritic volcanic extrusive. The showing was first drilled in 1947 but the assay results were not included in the assessment report. It may be assumed that no sygnificant gold values were detected. Geophysics and trenching on the showing in 1962 showed poor results however one sample graded .07 oz/ton Au, and another had 0.6% copper and 0.3% nickel." 075MSW0039,70,1,"Regional: The property is located near the center of a narrow 70 km long NNE trending belt of Archean Yellowknife Supergroup, volcanic and sedimentary rocks within the Slave Province. The belt, known as the Camsell Lake Belt forms the eastern limb of a synclinal fold cored by Archean biotite-muscovite granites.(GSC map 738-A) Property: The property lies on a contact between meta-volcanics to the east, and meta-sediments to the west. The volcanics on the property include mafic to felsic volcanic cycles younging to the west and including intervals of tuff, interflow sediments and sulphidic exhalites and rhyolite domes. Overlying the volcanics are typical Yellowknife group amphibolite grade turbidites. Showing: This showing was discovered by Nebex resources in 1993. The Asp Zone is a set of frost heaves near an outcrop of finely laminated mafic and felsic tuffs and wacke with minor somewhat bleached mafic volcanics. A one metre band of massive amphibolite with adjacent rusty shears crosses the centre of the outcrop. The actual gold bearing frost heaves about 40 metres SSW (along strike) of the outcrop are of a felsic or siliceous rock with quartz veining and up to 5% fine grained disseminated aspy. in rusty bands. Local lithologies suggest that this could be the sulfide facies of an iron formation." 075MSW0040,71,1,"Regional: The property is located near the center of a narrow 70 km long NNE trending belt of Archean Yellowknife Supergroup, volcanic and sedimentary rocks within the Slave Province. The belt, known as the Camsell Lake Belt forms the eastern limb of a synclinal fold cored by Archean biotite-muscovite granites.(GSC map 738-A) Property: The property lies on a contact between meta-volcanics to the east, and meta-sediments to the west. The volcanics on the property include mafic to felsic volcanic cycles younging to the west and including intervals of tuff, interflow sediments and sulphidic exhalites and rhyolite domes. Overlying the volcanics are typical Yellowknife group amphibolite grade turbidites. Showing: This polymetalic showing was discovered by Nebex Resources in 1993. Prospecting located rusty, sulphidic boulders along a 500 m long trend roughly coinciding with the upper felsic/metasediment contact near the southeast shore of Old Conoe Lake. Sample 37711 (4.8 g/t gold) was taken from a boulder of probable felsic tuff with quartz gal., sph., and cpy. Other samples of felsic float contained py. and po. mineralization. The area is covered with glacial overburden. Of the 4 samples taken the highest metal assays were 4880 ppb Au, 46 ppm Ag, 2.3% Pb, 1.17% Zn, and 0.122% Cu. Nebex took 6 more samples on the Canoe grid in 1994 with the highest gold value being 110 ppb." 075MSW0041,72,1,"Regional: The property is located near the center of a narrow 70 km long NNE trending belt of Archean Yellowknife Supergroup, volcanic and sedimentary rocks within the Slave Province. The belt, known as the Camsell Lake Belt forms the eastern limb of a synclinal fold cored by Archean biotite-muscovite granites.(GSC map 738-A) Property: The property lies on a contact between meta-volcanics to the east, and meta-sediments to the west. The volcanics on the property include mafic to felsic volcanic cycles younging to the west and including intervals of tuff, interflow sediments and sulphidic exhalites and rhyolite domes. Overlying the volcanics are typical Yellowknife group amphibolite grade turbidites. Showing: This polymetalic showing was discovered by Nebex Resources in 1993. The WK grid on the Brian 5 claim covers a package of north striking mafic volcanic flows, mafic crystal tuff and interflow sediments. Central to this package is a 20 m wide zone of intensely carbonitized mafic volcanics. The altered zone contains abundant quartz-calcite stringers and veins with local py., po. and cpy. The basalt hosted WK vein is exposed over 5 m, and up to 1 m in thickness. It consists of white quartz with traces of py., cpy. and up to 7.1 ppm silver. Five copper assays between 0.25% and 0.8% ppm were obtained from the WK vein and a gossan, also in basalt 80, m SSW of the WK vein."