64.4667,-76.15,0,036CSE0006,outcrop,Ray,036C08,Churchill - Rae,U,Resources Calculated,,,29-Sep-98,Source: Government Report,1000 Metres,,,, 69.6733,-76.8056,0,037CNE0010,outcrop,Eqe Bay,037C09,Churchill - Rae,Fe,Resources Calculated,52399,,22-Oct-97,Source: Government Report,Unknown,The iron showing occurs in strongly folded volcanics containing silicate and oxide iron formation within Eqe Bay Greenstone Belt. The magnetite-hematite iron formation occurs as zones within a 10 kilometre by 6 kilometre area.,"The showing is located 200 kilomtres east of Igloolik, 3 kilometres inland on Baffin Island.",, 73.0333,-84.3333,0,048CSE0002,outcrop,Nanisivik,048C01,Churchill,Pb-Zn-Cd-Cu,Producer,822500,,22-Oct-97,Method: Map/Airphoto,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Franklin. The MIR for 1978 of the Northwest Territories give the location of this showing. Figure or map accompanying report: LOC Fig II-1.,,, 61.98,-95.9267,0,055ENW0007,outcrop,Turquetil Lake Northwest,5.50E+14,Churchill - Hearne,Au,Resources Calculated,1088600,,22-Oct-97,Method: Map/Airphoto,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Keewatin.,Turquetil Lake is located 140 kiolmetres northwest of Arviat. Access to the property is br float or ski-equipped fixex-winged aircraft on to a suitable lake in the area.,, 62.9272,-92.1781,0,055JNW0001,outcrop,Meliadine West,055J13,Churchill - Hearne,Au,Resources Calculated,,,26-Oct-98,Source: Media/News Release,1000 Metres,"Discovery is a gold showing hosted in a banded, oxide facies iron formation and is part of the Meliadine West Gold Property. The showing is owned by WMC International Limited, Comaplex Minerals Corporation and Cumberland Resources Limited. Gold mineralization is structurally controlled and occurs in quartz veins associated with the hinges in Z-folds. Drill intercepts include 9.94 grams/tonne gold over 8 metres and 19.89 grams/tonne gold over 4.7 metres. Gold mineralized is open along strike and to a known depth of 350 metres. The location of the showing has been approximately pin pionted from several sources, most importantly DIAND assessment report 083414.",The showing is located approximately 20 kilometres north-northeast of Rankin Inlet and about 5 kilometres east of Maliadine Lake. Access to the property is by ski- or float equipped fixed-wing aircraft on to a near by lake. Rankin Inlet is close enough to be a base for supplies as it has a large air strip with regular scheduled flights.,, 62.1192,-93.8628,0,055KSW0041,outcrop,Fat Lake,055K04,Churchill - Hearne,Au,Resources Calculated,1088900,,22-Oct-97,Source: Assessment Report,15 Metres,"This showing was covered earlier by the IT and REP claims (the REP actually was covering the North Occurrence at Fat Lake (see NT MINFILE 055KSW042). Hudson Bay Mining and Smelting apparently held the ground in the 1940s. There is no evidence in the files of any work they did, however, P. Laporte made a property visit to the BM claims reportedly about 15 miles northwest of Tavane where over 2000 feet of drilling was done in 1945 (see Property Visit report for BM claims). Laporte found no evidence of work done at the latitude and longitude he visited.",The Fat Lake deposit is located approximately 70 km southwest of the community of Whale Cove and about 41 km west-northwest of the abandoned post of Tavani on Hudson Bay. Access by air.,"Park and Ralser (1990) state that there is at least two deformation phases in this area related to the Archean and a final D3 that correlated with northeast-southwest open folds in the Proterozoic Hurwitz Group sediments. They also state (with information from Thorpe and Miller, see GSC Open File 2265, page 35) that the gold-bearing veins from Fat Lake are demonstrably pre-D2 on structural criteria and therefore Archean. Model lead dates from galena in veins gave ages of 2652 Ma (Abitibi lead model) and 2694.5 Ma (Western Superior lead model). Au", 62.8167,-92.0833,0,055KNE0083,outcrop,North Rankin Nickel Mine,055K16,Churchill - Hearne,Ni-Cu-Pt-Pd-Carv,Past Producer,532500,,22-Oct-97,Source: Assessment Report,100 Metres,"The site of the mine is shown on 1:50,000 topographic maps and that is where the symbol location is taken from.",The townsite of Rankin Inlet is built up around the old minesite of the North Rankin Nickel Mine (minesite buildings were sold to the federal government for use when the mine closed in 1962). Access by regularly scheduled airline; sea access possible in summer months.,"Laporte (1975) notes that the regional metamorphic grade is greenschist facies and that contact metamorphic aureoles may be found around intrusions. Tella (1986) refutes there is any contact metamorphism. Various authors have proposed numerous structural evolutions for the area. Most commonly agreed on is that there is a major synclinal axis which follows the trend of the Kudlulik Peninsula. Some older reports indicate there may have been an earlier fold axis (isoclinal) and the syncline was actually a second generation fold (see Laporte (1975) - page 15 which shows interpretation of Hudec (1969)). Tella etal (1986) proposes only one major folding event in the area but interprets tectonic contacts (thrusts) to explain the discordance seen between the geology of the Kudlulik Peninsula and Thompson Island just to the east. As listed above, sulphide deposition is believed to occur early in the structural history of the area. Bannatyne (1958) believes the accumulation of the sulphides was contemporaneous with the intrusion of the sill which happened prior to major folding in the area.", 62.9042,-92.1197,0,055KNE0144,outcrop,F-Zone,055K16,Churchill - Hearne,Au,Resources Calculated,,,27-Oct-98,Source: Media/News Release,1000 Metres,"The F-Zone is a gold-bearing showing hosted within an Archean aged iron-formation. The iron formation is magnetite-poor and cherty. Gold and sulphide (arsenopyrite, pyrite and lesser chalcopyrite) mineralization are associated with quartz veining in the folded (hinged) portions of the exhalitive horizon. The F-Zone has a strike lenght of approximately 4,300 feet and is only one small zone making up the Wes Meg prospect. The property has been subjected to several 10s of drill holes testing the auriferous structure since at least 1994. A reserve figure of 1,800,000 tonnes grading 7.8 grams/tonne gold has been calculated for the zone. The showing location has been determined, with reasonable certainty, from both a news release (reference 19950831Comaple) and verbal conversations wih NWT DIAND district geologists.",The F-Zone is located on the southg side of Meliadine lake which is approximately 20 kilometres due north of Rankin Inlet. Access to the property is by ski- or float equipped aircraft onto one of the larger lakes in the area. There are scheduled daily commercial flights in Rankin Inlet. A road (all weathered?) from Rankin Inlet to the Meliadine River appears on a news release property map. This road appears to end at the river which is about 5 kilometres south of the F-Zone.,, 62.3686,-94.6253,0,055LSE0056,outcrop,Cache Zone,055L07,Churchill - Hearne,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,500 Metres,,"The project area (Noble Peaks Southwin) is approximately 150 km west-southwest of Rankin Inlet. Base camp was at Happy Lake, approximately 10 km northwest of Happotiyik Lake. A sand and gravel esker approximately 6 km west-southwest of the camp allowed camp to be serviced by a twin Otter with tundra tires. Helicopter was used within the project area.",, 63.6903,-95.7742,0,055MNW0002,outcrop,Apr-68,055M12,Churchill,U,Resources Calculated,931800,,22-Oct-97,Method: Map/Airphoto,100 Metres,"Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: Baker Lake Area, Keewatin District.",,, 62.9317,-92.1928,0,055NSE0001,outcrop,Tiriruniak Zone,055N01,Churchill - Hearne,Au,Resources Calculated,,,28-Oct-98,Source: Media/News Release,1000 Metres,"The Tiriruniak Zone is a gold showing hosted in shears cutting Archean aged rocks in the Churchill Structural Province. Tighter spaced (50 metres) diamond drilling was used in 1998 to better define the size and grade of the gold-bearing structure. Results from the 1998 drill program included values of 0.50 oz/ton gold over 16.4 feet (drill hole 194) and 0.83 oz/ton gold over 14.5 feet from drill hole 201 (news release reference 19980910Comaple). A resource calculation (identified resource) on the Tiriruniak Zone in 1998 resulted in an identified reserve of 8,000,000 tonnes grading 11.1 grams/tonne.",Tiriruniak is located approximately 5 kilometres northwest of the Wes Meg (F-Zone) prospect (showing 055KNE0144) and 23 kilometres north of Rankin Inlet. Access to the property is by ski- or float equipped fixed-winged aircraft onto a suitable lake near the property (possibly Meliadine Lake). Rankin Inlet has a airstrip with daily commercial flights and a road (all weather?) is indicated in a news release extending from the community to appearently Meliadine River which is about 10 kilometres south of the showing.,, 64.1694,-94.5594,0,056DSE0007,outcrop,Feb-68,056D02,Churchill,U-Mo,Resources Calculated,932300,,22-Oct-97,Method: Map/Airphoto,100 Metres,"Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: Baker Lake Area, Keewatin District.",,, 61.3067,-98.5033,0,065GSE0009,outcrop,Cullaton Lake South,065G07,Churchill,Au,Past Producer,1051700,,22-Oct-97,Source: Government Report,Unknown,,"Cullaton Lake South, also known as Shear Lake is approximately 4 km SSW of Cullaton Lake and 4 km N of Cullaton B zone. Both showings are about 230 kilometres west of Arviat. Access to the properties id by ski- or float equipped fixed-wing aircraft on to near by lakes or at a 1500 metre long air strip located 7 kilometres north of the B Zone.",, 61.2833,-98.5,0,065GSE0016,outcrop,Cullaton Mine,065G08,Churchill,Au,Past Producer,1052400,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Keewatin.,The Cullaton Mine (B-Zone) lies 8 km SSW of Cullaton Lake and is 320 km SW of Baker Lake.,, 61.7731,-96.2053,0,065HNE0001,outcrop,Heninga Lake,065H16,Churchill - Hearne,Zn-Cu-Ag-Au,Resources Calculated,159400,,22-Oct-97,Source: Assessment Report,100 Metres,,"By float or ski-equipped fixed wing aircraft or helicopter from Churchill, Manitoba, a distance of approximately 400 km. From Arviat the deposit is 130 kilometres northwest.",, 62.8733,-96.8331,0,065INE0001,outcrop,Ferguson Lake,065I15,Churchill - Hearne,Cu-Ni-Pt-Pd,Resources Calculated,1088202,,22-Oct-97,Source: Assessment Report,100 Metres,,"Located 225 km southwest of Baker Lake, NWT. Property is accessable by float or ski-equipped fixed wing aircraft or helicopter.", 62.5333,-98.6333,0,065JNE0005,outcrop,Lac Cinquante,065J10,Churchill - Hearne,U,Resources Calculated,,,1-Oct-98,Source: Government Report,1000 Metres,,, 64.2833,-97.6,0,066ASW0002,outcrop,Lone Gull,066A05,Churchill,U,Resources Calculated,959900,,22-Oct-97,Method: Map/Airphoto,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: Keewatin District.,The Lone Gull showing is approximately 72 km W of Baker lake., 65.2667,-96.3333,0,066GSE0001,outcrop,Lost Lake,066G08,Churchill - Rae,U,Resources Calculated,,,5-Oct-98,Source: Government Report,1000 Metres,,, 65.0131,-96.0469,0,066HSE0015,outcrop,Third Portage Lake,066H01,Churchill,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,"The deposit is located in the Meadowbank area, north of Tehek Lake and south of Meadowbank River. The gold showing is hosted in a 400 metre long sulphide-bearing iron formation cut by auriferous quartz veins.",The area is approximately 110 km north of Baker Lake and 930 km east-northeast of Yellowknife. Baker Lake has daily flights to Churchill (with connecting flights south) and a seasonal port facility. Wheel equipped planes can land on the ice on one of the areas lakes until June/July; float planes can then be used after break-up.,"Six deformation events were noted and described by Barham and Mudry (1990). A structural doctoral study (Ashton, 1988) is referenced and modified. See also Armitage and James, 1990. The presence of grunerite and chlorite assign the host rock to the lower amphibloite metamorphic grade. An isograd must exist north of Third Portage and south of TR 2." 65.025,-96.0489,0,066HSE0016,outcrop,Third Portage North Exten,066H01,Churchill,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,"The deposit is located in the Meadowbank area, north of Tehek Lake and south of Meadowbank River.","The area is ~110km north of Baker Lake and 930km east-northeast of Yellowknife. Baker Lake has daily flights to Churchill (with connecting flights south) and a seasonal port facility. Wheel equipped planes can land on the ice on one of the areas lakes until June/July; float planes can then be used after break-up. ","Six deformation events were noted and described by Barham and Mudry (1990). A structural doctoral study (Ashton, 1988) is referenced and modified. See also Armitage and James, 1990. The presence of grunerite and chlorite assign the host rock to the lower amphibloite metamorphic grade. An isograd must exist north of Third Portage and south of TR 2." 65.0036,-96.0544,0,066HSE0017,outcrop,Goose Island,066H01,Churchill,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,"The deposit is located in the Meadowbank area, north of Tehek Lake and south of Meadowbank River. An upper and lower auriferous iron formation makes up the showing. Drill core intersections in the iron formations include 318.5 grams/tonne gold over 2.90 metres (upper IF) and 11.66 gram/tonnes gold over 2.99 metres (lower IF). Goose Island is approximately 1 km south of the Third Portage Lake deposit.","The area is approximately 110 km north of Baker Lake and 930 km east-northeast of Yellowknife. Baker Lake has daily flights to Churchill (with connecting flights south) and a seasonal port facility. Wheel equipped planes can land on the ice on one of the areas lakes until June/July; float planes can then be used after break-up. ","Six deformation events were noted and described by Barham and Mudry (1990). A structural doctoral study (Ashton, 1988) is referenced and modified. See also Armitage and James, 1990. The presence of grunerite and chlorite assign the host rock to the lower amphibloite metamorphic grade. An isograd must exist north of Third Portage and south of TR 2." 75.3861,-96.9333,0,068HSE0003,outcrop,Polaris,068H08,Innuitian,Zn-Pb-Ag-Cd,Producer,834200,,22-Oct-97,To Be Determined,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Franklin. Location of showing determined from Pb-Zn Commodity File.,, 75.5419,-96.1675,0,068HNE0002,outcrop,Eclipse,068H09,Innuitian,Zn-Pb-Cd-Ag,Resources Calculated,36100,,22-Oct-97,Source: Assessment Report,100 Metres,,"The Eclipse showing is located on the eastern lobe of Little Cornwalis Island. The showing is accessable by air from Resolute, 104 km to the southeast.","karst dev.; Pb,Zn" 60.2578,-104.5267,0,075ASE0001,outcrop,Nickel King,075A07,Churchill - Rae,Ni-Cu-Co-Ag,Resources Calculated,1038800,,22-Oct-97,Source: Assessment Report,100 Metres,,"By float or ski-equipped fixed wing aircraft from Stony Rapids, Sask., 135 km to the southeast, or Points North, Sask.", 61.3258,-111.7922,0,075ESW0001,outcrop,OConnor Lake,7.50E+06,Churchill - Rae,Zn-Pb-Cu,Resources Calculated,819199,,22-Oct-97,Source: Assessment Report,100 Metres,,"By float plane or helicopter from Ft. Resolution or Yellowknife, NWT, distances of 100 km SSW and 175 km NW respectively. Nearest road terminus at Fort Resolution.", 61.325,-111.7789,0,075ESW0012,outcrop,OConnor Lake,7.50E+06,Churchill,Pb-Zn,Past Producer,819102,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Mackenzie.,, 61.3467,-110.24,0,075ESE0002,outcrop,Dussault,7.50E+09,Churchill - Rae,U,Resources Calculated,,,22-Oct-97,Source: Government Report,100 Metres,,"The Dussault showing is located on the west side of MacInnis Lake, 240 km SE of Yellowknife.","D0: Hudsonsian deformation heavies, precipitate D1: Hudsonsian deformation mobilization to vein" 61.4403,-109.7833,0,075FSW0001,outcrop,Salkeld Lake,075F05,Churchill - Rae,Cu-Ag-Zn-Pb-Au,Resources Calculated,656600,,22-Oct-97,Source: Assessment Report,100 Metres,,"The Salkeld Lake deposit is located 472 km northeast of Yellowknife, NWT, from which point it may be reached by float/ski-equipped fixed wing aircraft or helicopter.",Multiple phases of deformation with strong folding and faulting. 62.4097,-111.8619,0,075LSW0001,outcrop,Sachowia Lake,075L05,Slave,Ni-Co-Bi-Ag,Resources Calculated,957400,,22-Oct-97,Source: Assessment Report,100 Metres,,"The Sachowia Lake deposit is located 132 km east of Yellowknife, NWT, from which point it may be reached by float/ski-equipped fixed wing aircraft or helicopter.", 62.5825,-111.5594,0,075LNW0002,outcrop,BBX,075L12,Slave,Cu-Ag-Ni-Co-Bi-Pb-As,Resources Calculated,524200,,22-Oct-97,Source: Assessment Report,100 Metres,,147 km by float-plane or helicopter east from Yellowknife. One map shows an airstrip for the Great Slave Lodge., 63.0111,-110.8144,0,075MSE0001,outcrop,Susu Lake,075M02,Slave,Cu,Resources Calculated,657000,075M02CU 002,22-Oct-97,Source: Assessment Report,500 Metres,,"The deposit is situated approximately 185 km east northeast of Yellowknife NWT, from which it may be reached by float or ski-equipped fixed wing aircraft or helicopter. It is about 10 km north of the East Arm of Great Slave Lake.", 63.0322,-110.9483,0,075MSE0002,outcrop,BB,075M02,Slave,Zn-Pb-Ag-Cu,Resources Calculated,36203,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is situated 184 km east northeast of Yellowknife NWT, from which it may be reached by float or ski-equipped fixed wing aircraft or helicopter. It is 13 km north of the East Arm of Great Slave Lake.","D0: sulphide deposition D1: remobilization D2: remobilization All stratified rocks have been metamorphosed to middle amphibolite facies." 63.0325,-110.9633,0,075MSE0039,outcrop,Kennedy Lake West,075M02,Slave,Cu-Ag-Zn,Resources Calculated,75M02CU012,,22-Oct-97,Source: Assessment Report,100 Metres,,"The Kennedy Lake West showing is approximately 110 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft. As well, the property is only 10 miles north of the East Arm of Great Slave Lake and can be accessed this way.", 64.0017,-111.2325,0,076DSW0001,outcrop,Deb,076D03,Slave,Cu-Zn-Ag-Pb,Resources Calculated,1096300,075M14CU 003,22-Oct-97,Source: Assessment Report,100 Metres,,"The DEB showing is located on the northern shore of Mackay Lake approximately 208 km NE of Yellowknife, NWT. Mackay Lake is large enough to land planes up to a DC-3 on skis during the winter season and any aircraft on floats during the summer. The Tundra Mine airstrip is approximately 8 miles northeast of the showing.", 64.0183,-111.1683,0,076DSW0002,outcrop,Perrson,076D03,Slave,Au,Resources Calculated,,076D03AU_06,22-Oct-97,Source: Assessment Report,100 Metres,,"The showing is located approximately 235 km northeast of Yellowknife, NT and about 3 km south of the old Tundra Mine. During the summer months float planes are able to land on Don Lake. Access in the winter is possible from the winter road to the Lupin gold mine at Contwoyto Lake.", 64.1178,-111.2706,0,076DSW0003,outcrop,Tundra,076D03,Slave,Au,Resources Calculated,1058701,076D03AU007,22-Oct-97,Source: Assessment Report,100 Metres,,"Deposit is approximately 240 km northeast of Yellowknife, NWT and is accessable by float/ski-equipped aircraft or helicopter. Access during winter also via ice road off Lupin Winter road to Salmita Gold Mine. Salmita Mine airstrip, suitable for Hercules aircraft, is 5 km to southeast.", 64.0833,-111.25,0,076DSW0006,outcrop,RED 24,076D03,Slave,Au,Past Producer,660500,076D03AU001,22-Oct-97,Source: Assessment Report,1000 Metres,,"The RED claims are located at the north end of Matthews Lake and extend northward toward Courageous Lake. Access is by air in summer, 150 miles from Yellowknife by either float plane or by wheeled plane which could land on the Salmita strip 6 miles south.", 64.0597,-111.1997,0,076DSW0008,outcrop,Salmita New Discovery Vein,076D03,Slave,Au-Ag,Past Producer,1058500,076D03AU003,22-Oct-97,Source: Assessment Report,100 Metres,"The Salmita deposit includes the B, T, C zones in the north and on the South, Southeast and the Olsen showings.","The Salmita gold deposit is located 240 air kilometers NNE of Yellowknife on the east shore of Matthew Lake approximately 7 km south of Courageous Lake, NT. Access is by aircraft year round using an upgraded airstrip or by winter road.", 64.0561,-111.2061,0,076DSW0009,outcrop,Salmita South Vein,076D03,Slave,Au-Ag,Past Producer,1058600,076D03AU003,22-Oct-97,Source: Assessment Report,100 Metres,"The Salmita deposit includes the B, T, C zones in the north and on the South, Southeast and the Olsen showings.","The Salmita gold deposit is located 240 air kilometers NNE of Yellowknife on the east shore of Matthew Lake approximately 7 km south of Courageous Lake, NT. Access is by aircraft year round using an upgraded airstrip or by winter road.", 64.075,-111.2411,0,076DSW0010,outcrop,Salmita North Zone,076D03,Slave,Au-Ag,Past Producer,1058800,076D03AU003,22-Oct-97,Source: Assessment Report,100 Metres,"The Salmita deposit includes the B, T, C zones in the north and on the South, Southeast and the Olsen showings.","The Salmita gold deposit is located 240 air kilometers NNE of Yellowknife on the east shore of Matthew Lake approximately 7 km south of Courageous Lake, NT. Access is by aircraft year round using an upgraded airstrip or by winter road.", 64.0367,-111.1933,0,076DSW0019,outcrop,Tundra Mine,076D03,Slave,Au-Ag,Past Producer,,,20-May-98,Source: Government Report,500 Metres,,"The Tundra Mine is located 150 miles northeast of Yellowknife at the southern end of Matthews Lake and is accessible by float/ski-equipped airplane or helicopter. Access during winter also via ice road off Lupin Winter road to Salmita Gold Mine. Salmita Mine airstrip, suitable for Hercules aircraft, is to the northwest.", 64.0083,-111.1672,0,076DSW0020,outcrop,Saucer Zone,076D03,Slave,Au,Resources Calculated,,,7-Jun-98,Source: Assessment Report,500 Metres,The East Perrson Vein is part of the Saucer Zone and is considered a satellite showing of the Perrson Vein.,"The East Perrson Vein is located on the BS properties located 235 km northeast of Yellowknife, Northwest Territories and about 3 km south along strike from the old Tundra Mine. It is accessible during the summer months by float equipped aircraft to Don Lake. Access is possible in the winter from the winter road to the Lupin Mine at Contwoyto Lake.", 64.3081,-111.4128,0,076DSW0004,outcrop,Jax Lake,076D06,Slave,Au,Resources Calculated,1096100,,22-Oct-97,Source: Assessment Report,100 Metres,,The Jax showing lies north of Courageous Lake approximately 250 km NE of Yellowknife., 64.5614,-110.1772,0,076DNE0024,outcrop,Ekati - Misery,076D09,Slave,Diam,Resources Calculated,,,16-Oct-98,Source: Assessment Report,30 Metres,The location is derived from assessment work and was confirmed by BHP and Dia Met Minerals.,"The Fox Pipe is located in the Lac de Gras region, approximately 300 to 360 km north of Yellowknife, NT.", 64.6583,-110.6803,0,076DNE0020,outcrop,Ekati - Fox Pipe,076D10,Slave,Diam,Resources Calculated,,,16-Oct-98,Source: Assessment Report,30 Metres,The location is derived from assessment work and was confirmed by BHP and Dia Met Minerals.,"The Fox Pipe is located in the Lac de Gras region, approximately 300 to 360 km north of Yellowknife, NT.", 64.7167,-110.6064,0,076DNE0021,outcrop,Ekati - Koala,076D10,Slave,Diam,Resources Calculated,,,16-Oct-98,Source: Assessment Report,30 Metres,The location is derived from assessment work and was confirmed by BHP and Dia Met Minerals.,"The Fox Pipe is located in the Lac de Gras region, approximately 300 to 360 km north of Yellowknife, NT.", 64.7264,-110.5856,0,076DNE0023,outcrop,Ekati - Panda,076D10,Slave,Diam,Producer,,,16-Oct-98,Source: Assessment Report,30 Metres,The location is derived from assessment work and was confirmed by BHP and Dia Met Minerals.,"The Fox Pipe is located in the Lac de Gras region, approximately 300 to 360 km north of Yellowknife, NT.",, 64.7167,-110.6,0,076DNW0001,outcrop,Koala Lake Pipes,076D10,Slave,Diam,Resources Calculated,,,6-Jan-98,Source: Government Report,1000 Metres,,There is a 1950 m airstrip nearby as well as the Lupin winter road.,, 64.8606,-110.5128,0,076DNE0022,outcrop,Ekati - Sable Pipe,076D15,Slave,Diam,Resources Calculated,,,16-Oct-98,Source: Assessment Report,30 Metres,The location is derived from assessment work and was confirmed by BHP and Dia Met Minerals.,"The Fox Pipe is located in the Lac de Gras region, approximately 300 to 360 km north of Yellowknife, NT.",, 65.6083,-110.7833,0,076ENE0001,outcrop,Butterfly,7.60E+11,Slave,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,30 Metres,,"Float/ ski plane 390km NNE of Yellowknife to nearby small lakes (deposit is on one). Lupin Mine, 30km NW of the deposit, is supplied by an ice road from ~late-Jan to mid-March, and has its own full-length, all-weather airstrip with navigation aids.","King et al and Relf (GSC Papers 91-1C, 90-1C, 89-1C) recognize 3 to 4 Archean deformaton events, plutons of 6 different emplacement ages, and regional prograde and retrograde metamorphism. D1 involved isoclinal folding, cleavage development, and local faulting. D2, the main deformation event, coincided with the regional thermal peak and involved tight to isoclinal folding on a scale of mms to 100s of ms, development of the pervasive foliation, and minor faulting. D3 and possibly D4 involved two sets of open, upright cross-folds with NE- and NW-trending axial traces, and axial planar crenulation cleavages. These created kms scale structural domes defined by S2 and basins defined by biotite, cordierite and sillimanite isograds. The youngest plutons, C6, are interpreted to be contemporaneous with D3/4 cross-folding.","Age of mineralization is the subject of much debate between proponents of a syngenetic origin and of an epigenetic origin. (eg. Kerswill 1986, Gold86 Poster volume, ed. AM Chatter, Toronto, p.82-85; Lhotka and Nesbitt 1987, GAC/MAC Prog w/ Abstracts v.12 p.67)" 65.5814,-110.9686,0,076ENE0002,outcrop,Jon,7.60E+11,Slave,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,500 Metres,,"Float/ ski plane 390km NNE of Yellowknife to nearby small lakes (deposit is on one). Lupin Mine, 25km NW of the deposit, is supplied by an ice road from ~late-Jan to mid-March, and has its own full-length, all-weather airstrip with navigation aids.","King et al and Relf (GSC Papers 91-1C, 90-1C, 89-1C) recognize 3 to 4 Archean deformaton events, plutons of 6 different emplacement ages, and regional prograde and retrograde metamorphism. D1 involved isoclinal folding, cleavage development, and local faulting. D2, the main deformation event, coincided with the regional thermal peak and involved tight to isoclinal folding on a scale of mms to 100s of ms, development of the pervasive foliation, and minor faulting. D3 and possibly D4 involved two sets of open, upright cross-folds with NE- and NW-trending axial traces, and axial planar crenulation cleavages. These created kms scale structural domes defined by S2 and basins defined by biotite, cordierite and sillimanite isograds. The youngest plutons, C6, are interpreted to be contemporaneous with D3/4 cross-folding.","Age of mineralization is the subject of much debate between proponents of a syngenetic origin and of an epigenetic origin. (eg. Kerswill 1986, Gold86 Poster volume, ed. AM Chatter, Toronto, p.82-85; Lhotka and Nesbitt 1987, GAC/MAC Prog w/ Abstracts v.12 p.67)" 65.6617,-111.2056,0,076ENW0004,outcrop,Pan,7.60E+12,Slave,Au,Resources Calculated,1059900,,22-Oct-97,Source: Assessment Report,500 Metres,,"Float/ski plane 390 km NNE of Yellowknife to nearby small lakes. Lupin Mine, 10 km north of the deposit, is supplied by an ice road from approximately late January to mid-March, and has its own full-length, all-weather airstrip with navigation aids.","King et al and Relf (GSC Papers 91-1C, 90-1C, 89-1C) recognize 3 to 4 Archean deformaton events, plutons of 6 different emplacement ages, and regional prograde and retrograde metamorphism. D1 involved isoclinal folding, cleavage development, and local faulting. D2, the main deformation event, coincided with the regional thermal peak and involved tight to isoclinal folding on a scale of mms to 100s of ms, development of the pervasive foliation, and minor faulting. D3 and possibly D4 involved two sets of open, upright cross-folds with NE- and NW-trending axial traces, and axial planar crenulation cleavages. These created kms scale structural domes defined by S2 and basins defined by biotite, cordierite and sillimanite isograds. The youngest plutons, C6, are interpreted to be contemporaneous with D3/4 cross-folding. The syenite plug south of the deposit belongs to the C6 group; it generated localized hornfels metamorphism in the sediments hosting the deposit.","Age of mineralization is the subject of much debate between proponents of a syngenetic origin and of an epigenetic origin. (eg. Kerswill 1986, Gold86 Poster volume, ed. AM Chatter, Toronto, p.82-85; Lhotka and Nesbitt 1987, GAC/MAC Prog w/ Abstracts v.12 p.67)" 65.5628,-111.7969,0,076ENW0005,outcrop,Gondor,7.60E+13,Slave,Zn-Au-Ag-Cu-Pb,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,"Gondor is a base metal (copper, lead and zinc) massive sulphide showing with concentrations of silver and is operated as a joint venture between Inmet Mining Corporation and Noranda Inc. The deposit is hosted in a steeply dipping folded L-shape felsic to intermediate volcanic package (Archean Olga Lake Volcanic Belt). The ore body is traceable for 800 metres along strike and to a depth of 350 metres.","Float/ski plane 360 km NNE from Yellowknife to small lakes near the deposit. Lupin Mine, 35 km NE of Gondor, has an all-weather airstrip, and is supplied via ice road from about late January to mid-March.","D0: syngenetic sulphides King et al and Relf (GSC Papers 91-1C, 90-1C, 89-1C) recognize at least 3 Archean folding and fabric formation events, plutons of 6 different emplacement ages, and regional prograde and retrograde metamorphism. D2, the main deformation event, coincided with the regional thermal peak and involved tight to isoclinal folding on a scale of mms to 100s of ms, development of the pervasive foliation, and minor faulting. Later, two sets of open, upright cross-folds with NE- and NW-trending axial traces created kms scale structural domes and basins. The youngest plutons, C6, are interpreted to be contemporaneous with this cross-folding. Deposit according to Covello (pers. comm.) is at upper greenschist/ lower amphibolite boundary; according to AR 081676 it is lower to middle amphibolite facies. structural thickening", 65.7647,-111.225,0,076ENW0017,outcrop,Lupin Mine,7.60E+15,Slave,Au-Ag,Past Producer,1060800,,22-Oct-97,Method: Map/Airphoto,15 Metres,,Lupin mine occurs within a mile of the west shore in the northern part of Contwoyto Lake and approximately 400 km NE of Yellowknife. Access to the property is by air and winter road.,, 65.9172,-108.3631,0,076FNE0001,outcrop,Hackett River,076F16,Slave,Zn-Pb-Cu-Ag-Au,Resources Calculated,1088302,,22-Oct-97,Source: Assessment Report,100 Metres,,"By float plane or helicopter approx. 460 km northeast from Yellowknife, NWT. An esker suitable for wheeled aircraft lies about 6.5 km south of the prospect.","D0: sulphides D1: remob., thickening More deformational events highly likely.", 65.3231,-107.6208,0,076GSW0001,outcrop,Musk,076G05,Slave,Zn-Pb-Cu-Ag-Au-Ni,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,"The Musk Showing has been listed as having drill indicated reserves of 387,000 tons grading 1.2% Cu, 1.39% Pb, 10.38% Zn, 10.87 oz/ton Ag and 0.049 oz/ton Au. This is based on a total of 36 diamond drill holes totalling 3331 m.","The Musk Showing is accessable by float or ski equipped plane or helicopter. It is located approximately 460 km northeast from Yellowknife, NWT. An esker suitable for wheeled aircraft is located 6.5 km south.",The deposits are located on the limb of a steeply inclined NW trending fold which is marked by a strong S1 foliation. A crenulation cleavage is related to a second folding event., 65.5439,-106.4278,0,076GNE0017,outcrop,Goose Lake,076G09,Slave,Au,Resources Calculated,,,24-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest gold values of the showing area.,"Goose Lake is approximately 15 km south of Boot Lake Camp. THe property is approximately 500 km NE of Yellowknife, NT. Access is available by either float or ski equipped light aircraft to Goose Lake. In summer, tundra wheeled Twin Otter aircraft can utilize an undeveloped esker on the west side of Goose Lake.",The iron formation has been complexly folded and has a metamorphic grade is middle greenschist to lower amphibolite., 65.9258,-107.4764,0,076GNW0003,outcrop,George Lake,076G13,Slave,Au,Resources Calculated,,,7-Jan-98,Source: Assessment Report,30 Metres,"The NTS location is determined by selecting an approximate midpoint of the George Lake area. The George Lake Showing is comprised of 5 deposits and several occurences. The deposits include: Lone Cow Pond, Occurrence Lake (formerly Local 2), George Lake North (formerly locale 1 North, Locale 1), Esker Pond (formerly GH, GH SW, GH Central) and Slave. Occurrences include: Point, Plane, Fold Nose, Forest, Locale 3, Locale 4, Dragon Lake, and Creek. ","Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.","Chandler & Holmberg(1990)note that there are several periods of deformation in the George Lake area including ones post dating gold mineralization. NW trending brittle faults to ductile shears trend subparallel to Archean stratigraphy. Stratigraphy is offset by late N-NE conjugate brittle faults. Folding in the George Lake area is fairly extensive with tight to near isoclinal folds, steep west dipping axial planes and and subhorizontal fold axes. This fold geometry is interpretted to be the result of refolding of an earlier fold event such that fold noses exhibit variable attitudes, plunging moderately to steeply towards both the northwest and southeast. A later deformation episode has imposed a mild open warping along north to northeasterly axes with pronounced kink foliation developed in places. Chandler & Holmberg,1990 The metamorphic grade of the George Lake areas is lower to middle greenschist with chlorite being common and biotite developed in some mudstones.", 65.9258,-107.4764,0,076GNW0003,outcrop,George Lake,076G14,Slave,Au,Resources Calculated,,,7-Jan-98,Source: Assessment Report,30 Metres,"The NTS location is determined by selecting an approximate midpoint of the George Lake area. The George Lake Showing is comprised of 5 deposits and several occurences. The deposits include: Lone Cow Pond, Occurrence Lake (formerly Local 2), George Lake North (formerly locale 1 North, Locale 1), Esker Pond (formerly GH, GH SW, GH Central) and Slave. Occurrences include: Point, Plane, Fold Nose, Forest, Locale 3, Locale 4, Dragon Lake, and Creek. ","Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.","Chandler & Holmberg(1990)note that there are several periods of deformation in the George Lake area including ones post dating gold mineralization. NW trending brittle faults to ductile shears trend subparallel to Archean stratigraphy. Stratigraphy is offset by late N-NE conjugate brittle faults. Folding in the George Lake area is fairly extensive with tight to near isoclinal folds, steep west dipping axial planes and and subhorizontal fold axes. This fold geometry is interpretted to be the result of refolding of an earlier fold event such that fold noses exhibit variable attitudes, plunging moderately to steeply towards both the northwest and southeast. A later deformation episode has imposed a mild open warping along north to northeasterly axes with pronounced kink foliation developed in places. Chandler & Holmberg,1990 The metamorphic grade of the George Lake areas is lower to middle greenschist with chlorite being common and biotite developed in some mudstones.", 66.3167,-111.1944,0,076LSW0008,outcrop,Gumbo Lake Ilmenite,076L06,Slave,Ti-V-Fe,Resources Calculated,1099100,,22-Oct-97,Source: Assessment Report,500 Metres,,Float/ski plane 460 km NNE out of Yellowknife to nearby small lakes.,Archean volcanics intruded by the host complex underwent polyphase Archean deformation and metamorphism. Host complex itself is faulted (D1)., 66.9067,-110.9706,0,076LNE0023,outcrop,Ulu,076L15,Slave,Au-As-Bi-Zn-Ag-Cd,Resources Calculated,,,22-Oct-97,Source: Assessment Report,500 Metres,,Float/ski plane 520 km NNE out of Yellowknife to small lakes near showing.,"A structural history involving isoclinal folding, at least 2 generations of fabric formation, and late faulting, is not yet unravelled. According to Henderson (GSC Paper 93-1C), an early, bedding-parallel cleavage is folded by macroscale, steeply-plunging, tight to isoclinal folds (F2?), peak metamorphism was followed by development of the pervasive, NNE cleavage (S3?), and most granitic plutonism post-dated S3. In the Ulu area, S4 is developed as a vertical, NNE-striking crenulation of S3, and E & S of Ulu a vertical, NW-striking crenulation of S3 is observed. ", 67.3814,-110.85,0,076MSE0053,outcrop,High Lake AB Zone,076M07,Slave,Cu-Zn-Ag,Resources Calculated,653401,076M07CU 001,22-Oct-97,Source: Assessment Report,500 Metres,Update and entry 05/17/93.,Float/ski plane to nearby small lakes.,See GSC Open File 208. At least 2 phases of Archean folding and one of Proterozoic faulting. Contact metamorphism to Hbl-hornfels. syngenetic, 67.3758,-110.8436,0,076MSE0054,outcrop,High Lake D Zone,076M07,Slave,Zn-Cu-Ag-Pb-Au,Resources Calculated,653402,076M07CU 001,22-Oct-97,Source: Assessment Report,500 Metres,Update & entry 05/17/93.,Float/ski plane to nearby small lakes.,See GSC Open File 208. At least 2 phases of Archean folding and one of Proterozoic faulting. Contact metamorphism to Hbl-hornfels. syngenetic 67.7175,-111.3711,0,076MNW0084,outcrop,North Central Vein,076M11,Slave,Au-Ag,Resources Calculated,1063400,076M11AU 007,22-Oct-97,Source: Assessment Report,500 Metres,"The relationship of the 1980s North Central Vein to the 1960s North and No.11 Veins is not exactly defined. Numerous showings and two deposits with reserves (North Central Vein and Fred Vein) collectively go by names Arcadia, Coronation Gulf and Canuc.",Float/ski plane to nearby lakes; ship to parts of Coronation Gulf.,"Deformation according to Abraham, EGSs 1990-6 and 1991-4 and Exploration Overview 1990: Archean D1: margin-parallel S1 and local isoclinal F1, both N to NE, related to diapiric emplacement of host complex. Archean D2: S2 schistocity to ultramylonite fabric in major and minor NE-trending shear zones along margins of complex and within it; also some NNW shears; a regional translational shearing event?. Proterozoic D3: E-trending dextral and sinistral shears. If mineralization is synkinematic, as suggested (same refs; qtz injection and mineralization occurred late in D2), then its age must be bracketed by the youngest tonalite age (2682+/-2Ma U/Pb from zircon) and the age of a post-kinematic intrusion (2602+/-2Ma U/Pb from monazite in Chin Lake Stock). Note that the age of a hydrothermal alteration event in the North Central Vein hanging wall falls within this range (2670+/-2Ma Th/U from titanite) but cannot definitely be said to be related to mineralization." 67.7181,-111.3583,0,076MNW0085,outcrop,Fred Vein,076M11,Slave,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,500 Metres,"The relationship of the 1980s Fed Vein to the 1960s Northwest and Pick Veins is not exactly defined. Numerous showings and two deposits with reserves (North Central Vein and Fred Vein) collectively go by names Arcadia, Coronation Gulf and Canuc.",Float/ski plane to nearby lakes; ship to parts of Coronation Gulf.,"Deformation according to Abraham, EGSs 1990-6 & 1991-4 and Exploration Overview 1990: Archean D1: margin-parallel S1 and local isoclinal F1, both N to NE, related to diapiric emplacement of host complex. Archean D2: S2 schistocity to ultramylonite fabric in major & minor NE-trending shear zones along margins of complex and within it; also some NNW shears; a regional translational shearing event?. Proterozoic D3: E-trending dextral and sinistral shears. If mineralization is synkinematic, as suggested (same refs; qtz injection and mineralization occurred late in D2), then its age must be bracketed by the youngest tonalite age (2682 +/- 2Ma U/Pb from zircon) and the age of a post-kinematic intrusion (2602 +/- 2Ma U/Pb from monazite in Chin Lake Stock). Note that the age of a hydrothermal alteration event in the North Central Vein hanging wall falls within this range (2670 +/- 2Ma Th/U from titanite) but cannot definitely be said to be related to mineralization." 67.0494,-108.7861,0,076NSE0006,outcrop,Pistol Lake,076N02,Slave,Au-Ag-Cu,Resources Calculated,308700,076N02AU 001,22-Oct-97,Source: Assessment Report,100 Metres,,"Access is by float or ski equipped plane from Yellowknife to Pistol Lake, about 2.5 km west of the showings. A natural airstrip is located on a large esker about 5 km to the north, immediately west of Wilberforce Falls. ","At least two phases of deformation plus later faulting are evident from current mapping. Regional work by the GSC suggests that more Precambrian episodes are likely. In the silicate iron formation, auriferous sulphides are concentrated in folds with an amplitude of 50 - 150 m. Structural control on mineralization in the oxide iron formation is not clear but it is almost certainly present." 67.2169,-108.9403,0,076NSE0010,outcrop,Turner Lake Main Gold,076N02,Slave,Au,Resources Calculated,1058900,076N02AU 002,22-Oct-97,Source: Assessment Report,500 Metres,,"Float/ski plane to Turner Lake, up to C130 Hercules on ice; wheeled aircraft can land 10 km SSE on raised sand bed. Nearest major point of supply is Yellowknife, 580 km SW.","According to Clode 1987 and AR 082608, there were at least 2 phases of Archean deformation, involving tilting of strata to subvertical, development of a regional NE foliation, and localized N to NNE sinistral shearing possibly accompanied by E-W drag folding. According to Schaan (91-9), there were 2 fabric-forming and 3 folding events in the Archean. There were at least 2 Proterozoic faulting events (Clode 1987 and AR 082608). According to Clode (1987), mineralization occurred before the regional metamorphic peak, and before or during the NNE shearing event; and metamorphism peaked after the shearing event. See also Schaan (91-9)." 67.6167,-106.35,0,076ONE0010,outcrop,Boston,076O09,Slave,Au,Resources Calculated,,,15-Oct-98,Source: Government Report,Unknown,"Boston is a gold-bearing shear zone located in the southern portion of the Archean Hope Bay Greenstone belt. The pyritic quartz to quartz-carbonate shear occurs in a mafic volcanic package and is traceable for 70 kilometres along strike, obtaining a 1 kilometre width. Within the vicinity several other gold prospects (Doris Prospect, Madrid and South Patch Lake) held by BHP, occur. Boston is the most advanced prospect in the Hope Bay Belt and has been actively explored since 1991 by BHP, including over 50,700 metres of diamond drilling. An underground ramp was used to test the deposit at depth during 1996 and plans for a bulk underground sampling programme is scheduled during 1998 (reference GNWT RWED, MOG Book (1997)). The showing latitude and longitude is taken from RWEDs 1997 A guide to Mineral Deposits of the Northwest Territories.","Boston is situated approximately 170 kilometres south southeast of Cambridge Bay, along the eastern side of Bathurst Inlet and 700 kilometres northeast of Yellowknife. Access to the property is by ski- or float equipped fixed-winged aircraft onto Spyder Lake or Swan Lake. An esker strip was also established during earilier work programmes.", 60.7564,-115.1564,0,085BNE0001,outcrop,Great Slave Reef,085B10,"Arctic, Interior & Hudson Platforms",Pb-Zn-Ind1,Resources Calculated,1132203,,22-Oct-97,Source: Assessment Report,5000 Metres,,, 60.75,-115.0833,0,085BNW0006,outcrop,Great Slave Reef,085B11,"Arctic, Interior & Hudson Platforms",Pb-Zn-Cu,Resources Calculated,1132100,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Mackenzie. Showing is located 6 km southwest of Buffalo River. This showing adjoins west of Pine Points mine lease.,, 60.8514,-114.4417,0,085BNE0004,outcrop,Pine Point Mine,085B16,"Arctic, Interior & Hudson Platforms",Pb-Zn,Past Producer,808400,,22-Oct-97,Method: Map/Airphoto,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District of Mackenzie.,, 62.2281,-112.3028,0,085ISE0001,outcrop,Best Bet,085I01,Slave,Li-Be-Nb-Sn-Ta,Resources Calculated,1133100,,22-Oct-97,Source: Assessment Report,100 Metres,Previously featured in the Canmindex database where its history is described in great detail.,"The prospect is 112 km east southeast of Yellowknife, NWT and may be reached by float/ski-equipped fixed wing aircraft or helicopter from that point.",Pegmatite intrusion 62.1825,-112.2172,0,085ISE0002,outcrop,Moose #2 Dyke,085I01,Slave,Li-Nb-Be-Ta-Sn,Resources Calculated,942100,,22-Oct-97,Source: Assessment Report,100 Metres,,"The prospect is 115 km east southeast of Yellowknife, on the north shore of Drever Lake NWT, which makes it 6 km north of the East Arm of Great Slave Lake opposite Blanchet Island. The showing can be reached by float/ski-equipped fixed wing aircraft or helicopter.", 62.1958,-112.6961,0,085ISE0003,outcrop,Lens,085I02,Slave,Li-Nb-Ta-Be,Resources Calculated,1133800,,22-Oct-97,Source: Assessment Report,100 Metres,,"The prospect is 91 km southeast of Yellowknife, NWT and is accessable by helicopter and indirectly by float plane to a lake 1.6 km west.",Pegmatite intrusion 62.2253,-112.715,0,085ISE0004,outcrop,Mut,085I02,Slave,Li,Resources Calculated,1133600,,22-Oct-97,Source: Assessment Report,100 Metres,,90km,Pegmatite intrusion 62.2183,-112.7481,0,085ISE0005,outcrop,Bin,085I02,Slave,Li-Nb-Ta-Be,Resources Calculated,1133700,,22-Oct-97,Source: Assessment Report,100 Metres,,,Pegmatite intrusion 62.1181,-112.5997,0,085ISE0006,outcrop,Thor Lake,085I02,Slave,Be-Ta-Th-Y-Ga-Ce-Zr-Nb-La-Sm,Resources Calculated,1133400,,22-Oct-97,Source: Assessment Report,15 Metres,,"Thor Lake is 105 km SE of Yellowknife, NT. A 12 km tote road has been constructed between the deposit and the Hearn Channel of Great Slave Lake. The showing is also accessible by ski or float equipped fixed wing aircraft or by helicopter.", 62.4956,-113.9847,0,085ISW0007,outcrop,Big Hill East,085I05,Slave,Li,Resources Calculated,1134400,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is located 21 km east northeast of Yellowknife, NWT and is accessable by float/ski-equipped aircraft or helicopter from that point. The Ingraham Trail running east from Yellowknife passes 6 km north of the dykes.",Pegmatite intrusion 62.4189,-113.3661,0,085ISW0009,outcrop,Jake,085I06,Slave,Li-Sn-Ta-Nb,Resources Calculated,1134900,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is located 51 km east southeast of Yellowknife, NWT, from which point it may be reached by float/ski-equipped fixed wing aircraft or helicopter. The Ingraham Trail passes 10 km to the north.", 62.4133,-113.3794,0,085ISW0010,outcrop,Paint,085I06,Slave,Li-Ta-Nb,Resources Calculated,1134800,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is located 51 km east southeast of Yellowknife, NWT, from which point it may be reached by float/ski-equipped fixed wing aircraft or helicopter. The Ingraham Trail passes 10 km to the north.", 62.4756,-113.435,0,085ISW0011,outcrop,Ann,085I06,Slave,Li,Resources Calculated,1134700,,22-Oct-97,Source: Assessment Report,500 Metres,,"The prospect is 48 km east of Yellowknife, NWT, and is accessable from that point by float/ski-equipped aircraft or helicopter. The Ingraham Trail leading east from Yellowknife passes 1.1 km north of the dyke.", 62.3081,-112.8036,0,085ISE0012,outcrop,Hid,085I07,Slave,Li,Resources Calculated,1136300,,22-Oct-97,Source: Assessment Report,100 Metres,,, 62.2992,-112.7742,0,085ISE0013,outcrop,Mac,085I07,Slave,Li-Ta-Nb,Resources Calculated,1136100,,22-Oct-97,Source: Assessment Report,100 Metres,,The Mac showing is approximately 6 km W of Buckham Lake and is accessible by float or ski equipped fixed wing aircraft., 62.4178,-112.9078,0,085ISE0017,outcrop,Norma,085I07,Slave,Au,Resources Calculated,1135400,085I07AU 005,22-Oct-97,Source: Assessment Report,100 Metres,,"The Norma prospect is about 75 km east southeast of Yellowknife, NWT, and may be reached from that point by float/ski-equipped fixed wing aircraft or helicopter.", 62.4278,-112.8664,0,085ISE0018,outcrop,Joon,085I07,Slave,Au,Past Producer,1135200,085I07AU 003,22-Oct-97,Source: Assessment Report,100 Metres,"Although referred to as the June claims in GSC Memoir 261, the prospect is distinct from the June mineral leases immediately to the south.","The prospect is about 77.5 km due east of Yellowknife, NWT and is accessable from that point by float/ski-equipped fixed wing aircraft or helicopter.", 62.3414,-112.7506,0,085ISE0019,outcrop,Bullmoose,085I07,Slave,Ag-Au,Past Producer,1135000,085I07AU 001,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is 80 km east of Yellowknife, NWT, and may be reached from that point by air.", 62.4653,-112.5733,0,085ISE0020,outcrop,Ruth Mine,085I07,Slave,Au-Ag-As-W,Past Producer,1135500,085I07AU 006,22-Oct-97,Source: Assessment Report,100 Metres,,"The Ruth Mine is 96 km east of Yellowknife, NWT, and may be reached from that point by float/ski-equipped fixed wing aircraft or helicopter.", 62.4289,-112.1803,0,085ISE0021,outcrop,Thor,085I08,Slave,Li-Nb-Ta-Be,Resources Calculated,1080800,,22-Oct-97,Source: Assessment Report,100 Metres,,"The Thor pegmatites are located about 112 km east southeast of Yellowknife, NWT, and are accessable from that point by float/ski-equipped fixed wing aircraft or helicopter.", 62.7311,-112.6361,0,085INE0023,outcrop,XL,085I10,Slave,Pb-Zn-Cu-Ag,Resources Calculated,442000,,22-Oct-97,Source: Assessment Report,100 Metres,,"The prospect is approximately 91 km from Yellowknife, NWT, from which point it is accessable by float/ski-equipped aircraft.",Sulphide deposition 62.7236,-112.65,0,085INE0149,outcrop,Turnback Lake,085I10,Slave,Be-Ind3,Resources Calculated,1143700,,22-Oct-97,Method: Map/Airphoto,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 62.5925,-113.4656,0,085INW0028,outcrop,KI,085I11,Slave,Li,Resources Calculated,1160300,,22-Oct-97,Source: Assessment Report,100 Metres,,"Prospect is located approximately 50 km northeast of Yellowknife, NWT. Access is most convenient by helicopter from that point. Ground access in winter is possible via the Ingraham Trail (all weather gravel) 65 km east from Yellowknife to the Thompson Lundmark winter road which is unmaintained but generally passable, then 15 km north.",Pegmatite intrusion 62.5511,-113.4717,0,085INW0029,outcrop,Shorty,085I11,Slave,Li-Be-Sn,Resources Calculated,1136200,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is located 44 km ENE of Yellowknife, NWT, and may be reached from that point by float/ski-equipped aircraft onto Hidden Lake or directly by helicopter. The all weather Ingraham Trail road passes 5 km to the south. A winter road to the old Hidden Lake Gold Mine passes 1.5 km east of the deposit.", 62.5825,-113.4944,0,085INW0033,outcrop,FI Main Dyke,085I11,Slave,Li-Be,Resources Calculated,1160000,,22-Oct-97,Source: Assessment Report,100 Metres,"The FI Main dyke contains an estimated 2,672,000 tons to 152 m depth grading 1.54% Li2O, based on trenching and drilling.",Float/ski plane to Thompson Lake 3 km north or Hidden Lake 4 km SW; winter road passes 700 m to west. Showing is 48 km NE of Yellowknife.,"Regional metamorphism to lower amphibolite grade affected the surrounding sediments. Invasion of the pegmatites coincided with D2 cross-folding of the host sediments (Mulligan 1968, Henderson 1985)." 62.64,-113.4817,0,085INW0034,outcrop,Freda,085I11,Slave,Ta-Nb-Sn-Ti-Li-Be,Past Producer,1160600,,22-Oct-97,Source: Assessment Report,100 Metres,"3.75 tons of cobbed material from a 120 ton bulk sample was milled on-site in 1946. An estimated 500 lb of tantalite was contained in the cobbed ore and concentrates. A sample of the concentrates graded 46.19% Ta2O5, 31.18% NbO5, 1.83% SnO2 and 0.57% TiO2.",Float/ski plane to Thompson Lake 2.5 km south; or winter road to old Thompson-Lundmark Mine 4 km south.,"Regional metamorphism to lower amphibolite grade affected the surrounding sediments. Invasion of the pegmatites coincided with D2 cross-folding of the host sediments (Mulligan 1968, Henderson 1985). pegmatite intrusion?" 62.6067,-113.4656,0,085INW0037,outcrop,Thompson-Lundmark,085I11,Slave,Au-Ag,Past Producer w/ Reserves,1144000,,22-Oct-97,Source: Government Report,500 Metres,"This is a past producer as well as a deposit with reserves. It has seen production from 3 zones, has reserves remaining in at least one of these and in a new zone, and has further auriferous veins on the property. Production, from 1941 to 1949 except during war years, amounted to 70,339 oz Au and 13,782 oz Ag, mostly from the Kim and Fraser quartz vein systems. Reserves remaining are a proven 65,000 tonnes grading 6.86 gpt in the Kim, and an additional 12,428 tonnes grading 5.49 gpt in other veins.","Property is 65 km ENE of Yellowknife and lies mostly south of Thompson Lake, which is accessible by small float/ski-equipped aircraft. An approximately 15 km winter road provides direct access to the site from the all-weather Hwy 4 (Ingraham Trail).","Boyle (GSC Memoir 310, 1961) suggests auriferous quartz veining in dilatent zones during and following regional deformation. Henderson (GSC Memoir 414, 1985) discusses metamorphism and deformation. qtz veining?" 62.5414,-113.43,0,085INW0042,outcrop,Jim Lit,085I11,Slave,Li-Be,Resources Calculated,1160100,,22-Oct-97,Source: Assessment Report,100 Metres,This deposit comprises 5 separate Li-rich dykes in an area roughly 1 x 1 km.,"The dykes are 4 km east of Hidden Lake, 48 km ENE of Yellowknife, and 3.5 km NW of the Tibbitt Lake terminus of all-weather Hwy 4. A lake suitable for float/ski plane landings lies 1.5 km to the east.","Regional metamorphism to lower amphibolite grade affected the surrounding sediments. Invasion of the pegmatites coincided with D2 cross-folding of the host sediments (Mulligan 1968, Henderson 1985)." 62.7375,-113.3489,0,085INW0048,outcrop,Pensive Yellowknife Mine,085I11,Slave,Au,Past Producer,1144600,,22-Oct-97,Source: Assessment Report,100 Metres,"An 8.2m -long open cut was excavated on a grey quartz vein in 1939, and a 15m deep shaft was sunk from this in 1941. Altogether, several thousand tonnes of hand-picked ore yielded gold valued at about $7000 (NMI).","NOTE TO DATA CHECKERS; this record may not be complete. The claims are located at the northeast end of Upper Pensive Lake, about 38 Miles Northeast of Yellowknife. Lakes near the property are accessible by float or ski equipped aircraft. A winter road connecting Yellowknife and Echo Bay Mines Lupin gold mine passes within 3 km of the claims.", 62.7442,-113.1083,0,085INW0049,outcrop,Peg Tantalum,085I11,Slave,Be-Ta-Nb-Sn,Past Producer,1144100,,22-Oct-97,Method: Map/Airphoto,100 Metres,"During 1946 and 1947, 1090 tons of pegmatite rock were milled to yield tantalite-columbite concentrates of unknown grade. The first 940 tons treated yielded 3780 pounds of concentrates.","Property is near the northeast side of Upper Ross Lake, 45 miles northeast of Yellowknife. Access by aircraft to Upper Ross Lake and then along a one and a half mile rough tractor road. Alternative access in winter by a 70 mile winter tractor road via Jennejohn, Reid, Hidden, Thompson, and Ross Lake.", 62.7447,-113.5297,0,085INW0077,outcrop,Million Dollar,085I12,Slave,Au-Ag,Past Producer,1161100,,22-Oct-97,Source: Assessment Report,100 Metres,,"Float/ski plane to Parr Lake, 53 km NE of Yellowknife.","Boyle (GSC Memoir 310, 1961) suggests auriferous quartz veining in dilatent zones during and following regional deformation. Henderson (GSC Memoir 414, 1985) discusses metamorphism and deformation. qtz veining?" 62.7419,-113.5339,0,085INW0078,outcrop,Old Parr South,085I12,Slave,Au-Ag,Past Producer,1161100,,22-Oct-97,Source: Assessment Report,100 Metres,,"Float/ski plane to Parr Lake, 53 km NE of Yellowknife.","Boyle (GSC Memoir 310, 1961) suggests auriferous quartz veining in dilatent zones during and following regional deformation. Henderson (GSC Memoir 414, 1985) discusses metamorphism and deformation." 62.575,-113.5067,0,085INW0079,outcrop,FI Southwest Dyke,085I12,Slave,Li,Resources Calculated,1162000,,22-Oct-97,Source: Assessment Report,100 Metres,"This pegmatite dyke was estimated to contain 4,526,000 tons of ore grading 1.46% Li2O. Bulk sample metallurgical testwork has indicated that a spodumene concentrate containing 5-6% Li2O at an overall recovery of 80% could be produced.",Float/ski plane to Thompson Lake 4km N or Hidden Lake 2.5km SW; winter road passes 500m to west and Hwy 4 (Ingraham Trail) ~12km S. Showing is 48km NE of Yellowknife.,"Regional metamorphism to lower amphibolite grade affected the surrounding sediments. Invasion of the pegmatites coincided with D2 cross-folding of the host sediments (Mulligan 1968, Henderson 1985)." 62.8367,-113.5631,0,085INW0084,outcrop,Vo #2,085I13,Slave,Li-Be-P2O5,Resources Calculated,1162300,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposits are located about 50 km northeast of Yellowknife, NWT, from which point they may be reached by float/ski-equipped fixed wing aircraft or helicopter.", 62.8339,-113.5778,0,085INW0085,outcrop,Vo #5,085I13,Slave,Li-Be-P2O5,Resources Calculated,1162300,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposits are located about 50 km northeast of Yellowknife, NWT, from which point they may be reached by float/ski-equipped fixed wing aircraft or helicopter.", 62.8103,-113.5817,0,085INW0158,outcrop,Blaisdell Lake,085I13,Slave,Be-Li-Nb-Ta,Resources Calculated,1162200,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 62.9625,-113.3483,0,085INW0104,outcrop,Mahe,085I14,Slave,Au,Resources Calculated,1081200,,22-Oct-97,Method: Map/Airphoto,100 Metres,"The Mahe deposit consists of gold-bearing , quartz breccia zones in fold, carbonaceous, sulphide-rich siltstone. The host sediments are part of the Archean Yellowknife Supracrustral Belt. Surface and underground drilling outlined the deposit as being 305 metres long, 6 to 30 metres wide and traceable to a depth of 121 metres (reference GNWT RWED, MOG Book (1997)).",, 62.7883,-113.2381,0,085INW0105,outcrop,MYRT,085I14,Slave,Au-Pb-Zn-Cu,Resources Calculated,1081300,,22-Oct-97,Method: Map/Airphoto,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,"The showing lies approximately 72 km NE of Yellowknife, NWT.", 62.9058,-113.2328,0,085INW0132,outcrop,Gordon Lake,085I14,Slave,Au-Ag-Cu-Pb-Zn,Past Producer w/ Reserves,1141900,,22-Oct-97,Method: Map/Airphoto,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,Located at the SE shore of Gordon Lake, 62.9847,-113.2042,0,085INW0133,outcrop,Camlaren Mine,085I14,Slave,Au-Ag-Cu-Pb-Zn,Past Producer w/ Reserves,1142000,,22-Oct-97,Method: Map/Airphoto,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 62.7667,-113.4667,0,085INW0142,outcrop,Mitchell Lake,085I14,Slave,Au-Ag-Pb,Resources Calculated,1142900,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 62.7569,-113.2806,0,085INW0155,outcrop,Dome Lake (Southwest Side,085I14,Slave,Au-Ag-Pb,Resources Calculated,1161800,,22-Oct-97,Method: Map/Airphoto,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 62.8997,-112.3781,0,085INE0086,outcrop,Sunrise,085I16,Slave,Zn-Pb-Ag-Cu-Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,,"By float plane or helicopter from Yellowknife, NWT, a distance of 112 km. The right of way for the Ingraham Trail extension is surveyed and cut to within 8 km west of Sunrise Lake. A separate road runs eastwards through Victory, Weaver and Turnback Lakes and north to Sunset and Sunrise Lakes.",, 62.8928,-112.3947,0,085INE0087,outcrop,Bear,085I16,Slave,Zn-Pb-Ag-Au-Cu,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,,"By float plane or helicopter, 110 km east northeast from Yellowknife, NWT.",Prominent north/70? lineation in fragmental units parallels elongation of sulphide lenses. Possible growth faults indicated by changes in unit thickness, 62.4964,-114.3658,0,085JSE0012,outcrop,Giant Mine,085J08,Slave,Au-Ag-As,Producer,1163300,,22-Oct-97,Source: Government Report,100 Metres,"Names of mineralized zones: East, West, Creek, GB, Trough, ASD, Brock Veins, HG, WJT, Muir, Law. A separate NORMIN showing deals with the Supercrest Mine, generally regarded as part of Giant (Akaitcho and GKP zones), which is connected to the Giant workings underground.","The Giant minesite is 3 - 5 km north of Yellowknife. Yellowknife, on the west side of Yellowknife Bay, is a city of roughly 16,000 people. It is connected by road to southern cities and serviced by a modern airport with daily flights to numerous major cities.",,"The structural geology of the Yellowknife Volcanic Belt and the origin of its gold deposits is discussed by Boyle 1961 (GSC M 310) and in Henderson and Brown 1966 (GSC P 141); structure is also discussed in later works such as Fyson 1978 (JGEOL), Helmstaedt and Bailey 1987 (MDD GAC YK Field Guide), and Helmstaedt and Padgham 1986 (CIMMSVOL 38). See also Other References." 62.4664,-114.3194,0,085JSE0013,outcrop,Burwash Mine,085J08,Slave,Au,Past Producer,1163100,,22-Oct-97,Source: Assessment Report,100 Metres,Location from AR 082602 base map (1990 report on PRO claims).,"Shaft is on east shore of Yellowknife Bay, 2 km east of the City of Yellowknife and 900 m west of the road to Dettah.","Henderson 1985 (GSC M 414) discusses metamorphism and deformation. Deformation is also discussed in GSC P 141, and in Fyson 1982 (CJES v19 p878).", 62.4958,-114.425,0,085JSE0050,outcrop,Rod,085J08,Slave,Au-Ag,Resources Calculated,1163000,,22-Oct-97,Source: Government Report,100 Metres,,"The deposit is 4.1 km west of Highway 4, 2.5 km north of Highway 3, and roughly 6 km NW of downtown Yellowknife. A trail, passable by truck in the winter, connected the area to Highway 3 in 1975.","Emplacement of the host Complex probably was accompanied, in a broad temporal sense, by deformation and metamorphism of the invaded supracrustals (GSC M 414); grade is at least amphibolite in the adjacent volcanics. The host Defeat Suite of the Complex, the second from oldest suite (~2620 Ma; DIANDEO 90), is moderately to strongly deformed in its lower part and massive to foliated in its upper part. At the showing it is massive.","Age of host shearing is pre-diabase (AR 017331). According to DIANDEO 90, the latest phase of granite intrusion in the Complex (~2585 Ma) induced shearing in the earlier, marginal phases of the Complex and was associated with a major gold mineralization event in the supracrustals." 62.4394,-114.3689,0,085JSE0056,outcrop,Con-Rycon,085J08,Slave,Au-Ag-Sb-Pb-Cu-Zn,Producer,1163200,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,,, 62.5497,-114.1808,0,085JNE0002,outcrop,Cassidy Point,085J09,Slave,Au-Zn-Pb,Resources Calculated,1165400,,22-Oct-97,Source: Assessment Report,100 Metres,,"NWT Hwy 4, from Yellowknife 15 km SW, passes 2 km to the south, and a road from the highway to cottage leases on Cassidy Point is kept clear all winter.","Boyle (GSC Memoir 310, 1961) suggests auriferous quartz veining in dilatent zones during and following regional deformation. Deformation is discussed in GSC P 141, and in Fyson 1982 (CJES v19 p878). Henderson 1985 (GSC M 414) provides an overview of stratigraphy, deformation and metamorphism.", 62.5331,-114.1969,0,085JNE0009,outcrop,Tom Mine,085J09,Slave,Au-Cu-Pb-Zn,Past Producer,1165500,,22-Oct-97,Source: Government Report,100 Metres,,"The minesite, approximately 13 km NE of Yellowknife, is accessible by road. There is power to the site.","Boyle (GSC Memoir 310, 1961) suggests auriferous quartz veining in dilatent zones during and following regional deformation. Henderson 1985 (GSC M 414) discusses metamorphism and deformation. Deformation is also discussed in GSC P 141, and in Fyson 1982 (CJES v19 p878), and Fyson 1987 (YK Field Guide p89). According to Brophy 1987 (YK Field Guide p195), only 2 deformations (D1 and D3 of Fyson) are evident in the Tom/ Ptarmigan area, being large-amplitude, open F1 folds about ESE-trending axes, and small-scale F3 folds with associated axial planar S3 foliation oriented SE/subvertical. S3 is the dominant regional fabric.", 62.5192,-114.1972,0,085JNE0010,outcrop,Ptarmigan Mine,085J09,Slave,Au,Past Producer,1164200,,22-Oct-97,Source: Government Report,100 Metres,,"The minesite, approximately 12 km NE of Yellowknife, is accessible by road. There is power to the site.","Boyle (GSC Memoir 310, 1961) suggests auriferous quartz veining in dilatent zones during and following regional deformation. Henderson 1985 (GSC M 414) discusses metamorphism and deformation. Deformation is also discussed in GSC P 141, and in Fyson 1982 (CJES v19 p878), and Fyson 1987 (YK Field Guide p89). According to Brophy 1987 (YK Field Guide p195), only 2 deformations (D1 and D3 of Fyson) are evident in the Tom/ Ptarmigan area, being large-amplitude, open F1 folds about ESE-trending axes, and small-scale F3 folds with associated axial planar S3 foliation oriented SE/subvertical. S3 is the dominant regional fabric.", 62.5381,-114.1692,0,085JNE0011,outcrop,Vega,085J09,Slave,Au,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,Very little information on Vega was uncovered; it is mentioned as having small reserves of gold ore in AR 082052 (a report on a neighbouring property).,Easily accessible by road; NWT Hwy 4 passes 600m south and the road from Hwy 4 to Cassidy Point passes within 850m to the west. Prosperous Lake is also accessible to ski/float-equipped aircraft and by boat; the showing occurs on its southern shores.,"Boyle (GSC Memoir 310, 1961) suggests auriferous quartz veining in dilatent zones during and following regional deformation. Henderson 1985 (GSC M 414) discusses metamorphism and deformation. Deformation is also discussed in GSC P 141, and in Fyson 1982 (CJES v19 p878).", 62.5806,-114.3614,0,085JNE0014,outcrop,Crestaurum,085J09,Slave,Au-Ag-Sb-Pb,Past Producer w/ Reserves,1164300,,22-Oct-97,Method: Map/Airphoto,15 Metres,"A gold deposit in sheared mafic volcanics with drill-indicated reserves of 145,000 tonnes grading 7.54 g/t Au. Treminco Resources was planning to open-pit mine a bulk sample in 1989.","The deposit on Daigle Lake is 15 km north of Yellowknife. Highway 4 can be taken from the city to the Vee Lake (or Crestaurum) Road, which is a dirt road cleared as far as Vee Lake in the winter but continuing northward as a bush road to Daigle Lake and beyond. Road conditions past Vee Lake even in summer are often bad enough to require four wheel drive. Daigle Lake is roughly 4 km north of Vee Lake.",,"The structural geology of the Yellowknife Volcanic Belt and the origin of its gold deposits is discussed by Boyle 1961 (GSC M 310) and in Henderson and Brown 1966 (GSC P 141); structure is also discussed in later works such as Fyson 1978 (JGEOL), Helmstaedt and Bailey 1987 (MDD GAC YK Field Guide), and Helmstaedt and Padgham 1986 (CIMMSVOL 38). See also Other References. Metamorphic grade was not specified in references available but is likely upper greenschist to middle amphibolite (Henderson and Brown 1966)." 62.5231,-114.3481,0,085JNE0015,outcrop,Supercrest,085J09,Slave,Au-Ag-As,Past Producer w/ Reserves,1163400,,22-Oct-97,Source: Government Report,100 Metres,"This producer is generally considered part of the Giant Mine, to which it is connected underground, and which is dealt with in a separate NORMIN showing.","The Giant minesite is approximately 5 km north of downtown Yellowknife. The Akaitcho shaft is about 8 km north of the city and 3 km north of Giants C Shaft; the GKP portal is 1.6 km NW of the Akaitcho Shaft. Yellowknife, on the west side of Yellowknife Bay, is a city of roughly 16,000 people. It is connected by road to southern cities and serviced by a modern airport with daily flights to numerous major cities.",,"The structural geology of the Yellowknife Volcanic Belt and the origin of its gold deposits is discussed by Boyle 1961 (GSC M 310) and in Henderson and Brown 1966 (GSC P 141); structure is also discussed in later works such as Fyson 1978 (JGEOL), Helmstaedt and Bailey 1987 (MDD GAC YK Field Guide), and Helmstaedt and Padgham 1986 (CIMMSVOL 38). See also Other References." 62.5428,-114.36,0,085JNE0044,outcrop,Lynx,085J09,Slave,Au,Resources Calculated,1165100,,22-Oct-97,Source: Assessment Report,100 Metres,"See also NMI Au 18 (NE extension of east zone, at One Arm Lake) and Au 10 (NE extension of west zone, beneath Vee Laek). Lynx is a small, two-zone gold deposit in a fault-offset continuation of the Giant shear system. The GKP zone of NT MINFILE showing Supercrest is the southernmost part of the Lynx west zone, but falls under NT MINFILE showing Supercrest due to its inclusion in Supercrest reserve and production figures.",The Vee Lake road off NWT Highway 4 provides excellent year-round access to the site.,,The structural geology of the Yellowknife Volcanic Belt is discussed by Boyle 1961 (GSC M 310) and in Henderson and Brown 1966 (GSC P 141). 62.5003,-114.0097,0,085JNE0051,outcrop,Big Hill West,085J09,Slave,Li,Resources Calculated,1164000,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is located 21 km east northeast of Yellowknife, NWT and is accessible by float/ski-equipped aircraft or helicopter from that point. The Ingraham Trail running east from Yellowknife passes 6 km north of the dykes.",, 63.3514,-116.3042,0,085NSE0043,outcrop,Camp Lake,085N08,Slave,Au-Zn-Pb-Cu,Resources Calculated,1168500,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,"The Camp Lake Showing is located on the E side of Snare River, 131 km NW of Yellowknife, NT.",, 63.2675,-116.1106,0,085NSE0044,outcrop,Slemon Lake,085N08,Slave,Au-Ag-Cu,Resources Calculated,1168600,,22-Oct-97,Method: Map/Airphoto,1000 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,"The Slemon showing is located approximately 125 km NW of Yellowknife, NT and 4 km NE of Slemon Lake.",, 63.5453,-116.7403,0,085NNE0001,outcrop,Cab,085N10,Bear,Bi-Co-Cu-Au-As-W-Sb-Mo,Resources Calculated,1088400,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is 150 km northwest of Yellowknife, NWT and 30 km northwest of the Snare River hydro plant. In summer, access is by float-equipped fixed wing aircraft or helicopter. In winter, access is possible via the Echo Bay mine winter road which passes 4 km west of the deposit.",,Mineralization thought to be related to felsic magmatic and volcanic activity in Great Bear Magmatic Zone. 63.55,-116.7458,0,085NNE0045,outcrop,Lou Lake (Southeast of),085N10,Slave,Bi-Co-Au-Cu-W,Resources Calculated,1168700,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,,, 63.7583,-116.9167,0,085NNE0035,outcrop,SUE,085N15,Bear,Cu-Ag-U-Au-Fe,Resources Calculated,980200,,22-Oct-97,Source: Government Report,Unknown,"Sue (commonly known as Sue-Dianne) is an Olympic Dam-type mineralization containing copper, uranium, gold, silver and iron concentrations. Ore minerals occuring on the showing include chalcopyrite, bornite, chalcocite and pitchblende. The deposit occurs in a pipe-like, magnetite cemented, brecciated horizon comformable with a package of thick ash flows. These rocks are situated on the eastern side of the Bear Structural Province (Proterzoic aged rocks) within the Great Bear Magmatic Zone. The property operated through a joint venture between Fortune Minerals NWT and Noranda Inc.",,, 63.1053,-114.0539,0,085OSE0007,outcrop,Viking Yellowknife,085O01,Slave,Au,Resources Calculated,1168900,,22-Oct-97,Source: Assessment Report,100 Metres,The Viking deposit has had underground development with diamond drilling done on one level. A resource was calculated based on this development and on surface work. The inferred reserve for this deposit was calculated as 700 tons per vertical foot at an estimated grade of 0.60 oz/ton gold.,The property is southwest of Morris Lake and approximately 45 miles north-northeast of Yellowknife.,, 63.1811,-115.825,0,085OSW0001,outcrop,Bugow,085O04,Slave,Au,Resources Calculated,1169500,,22-Oct-97,Source: Assessment Report,100 Metres,"The Bugow Showing is also known by the name Andrew South. The iron formation which hosts this deposit has satellite showings, one 300 m north called the Andrew North (Showing Number 085OSW0040) and the AH 205 (Showing Number 085OSW0041) 400 m south.","The deposit is located about 130 km northwest of Yellowknife, and 45 km north of the village of Rae. Access to the claims is either by float plane and helicopter or by boat across Russell Lake.",, 63.0375,-115.5181,0,085OSW0013,outcrop,Mosher Lake,085O04,Slave,Au,Resources Calculated,1169600,,22-Oct-97,Source: Assessment Report,100 Metres,This showing has a resource calculated based on trenching and diamond drilling. It was taken to lease in 1983.,The showing is on the southwest end of Mosher Lake which is 55 miles northwest of the city of Yellowknife and 22 miles northeast of Fort Rae. Access is by float or ski equipped aircraft.,, 63.1739,-115.8239,0,085OSW0042,outcrop,Cabin Lake,085O04,Slave,Au,Resources Calculated,,,30-Jun-98,Source: Assessment Report,100 Metres,,"The deposit is located about 130 km northwest of Yellowknife, and 45 km north of the village of Rae. Access to the claims is either by float plane and helicopter or by boat across Russell Lake.",, 63.2494,-113.7694,0,085PSW0001,outcrop,Nicholas Lake,085P04,Slave,Au-Zn-Pb-As,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,,"The deposit is 88 km north of Yellowknife, NWT, and may be reached from that point by float/ski-equipped aircraft or helicopter. It is situated 8 km northeast of the old Discovery Mine. A recent study suggests the most likely route by winter road is 98 km in length.",, 63.1867,-113.8917,0,085PSW0032,outcrop,Discovery Mine,085P04,Slave,Au-Pb-Cu,Past Producer,1171300,,22-Oct-97,Method: Map/Airphoto,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,,, 63.1694,-113.9222,0,085PSW0035,outcrop,Winter Lake,085P04,Slave,Au,Resources Calculated,1171600,,22-Oct-97,Source: CANMINDEX,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,"The Winter Lake showing is approximately 85 km NNE of Yellowknife, NT.",, 63.0992,-113.5467,0,085PSW0037,outcrop,Cross Lake,085P04,Slave,Au-Pb-Zn-Cu,Resources Calculated,1171800,,22-Oct-97,Method: Map/Airphoto,1000 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,The Gab showing is approximately 19 km SE of Discovery Mine.,, 63.2847,-113.0403,0,085PSW0040,outcrop,Gordon Lake,085P06,Slave,Au,Resources Calculated,1172100,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,This showing is located NE of Gordon Lake approximately 77 km NNE of Yellowknife.,, 64.1533,-115.2183,0,086BSW0012,outcrop,Anna (Barker Vein),086B03,Slave,Au,Past Producer,1066300,,22-Oct-97,Source: Government Report,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie The Barker Vein (part of the Anna Showing) is an auriferous quartz-carbonate vein which yielded 1600 pounds of ore containing 83 fine ounces of gold in the late 1930s. During 1940 the area was re-staked and an additional 248 ounces of gold was recovered (reference no. 261 and 081785). The vein is 40 feet long and is hosted in a foliated mafic volcanic unit. Additional gold assays were obtained from near by trenches and from a quartz-feldspar dyke that ran 3560 ppb gold (reference no. 083384). The longitude and latitude of the showing is based on the location of the Barker Vein.,The Barker Vein is situated on the south eastern shore of Indin Lake. Access to the area is by ski- or float equipped fix-winged aircraft on to Indin Lake.,At least 4 deformational events were recorded by Pehrsson and Beaumont-Smith (1994-Cp91) in their study of the Indin Lake Belt., 64.1392,-115.1139,0,086BSW0050,outcrop,Horseshoe Zone,086B03,Slave,Au,Resources Calculated,,,20-Jul-98,Source: Media/News Release,100 Metres,"The majority of work preformed in the southern portion of Damoti Lake has been on the Horseshoe Zone. The Property is an auriferous iron formation which has had extensive exploration work preformed on it, including underground mining. The latitude and longitude of this showing is based on the approximate center of the zone.","The property is located 210 kilometres north-northwest of Yellowknife, NT and can be accessed with a ski- or float equipped fix-winged aircraft on to Damoti Lake or by a helicopter in to the area. It may be possible to access Indin Lake (approximately 7-10 kilometres north) via winter ice road should a road be constructed to Colomac Mine.",The area has a minimum of 4 deformational events associated with the Indin Lake Belt and the area has been metamorphosed from lower greenschist to amphibolite (reference I.D. No. 1994-Cp91)., 64.4083,-115.7583,0,086BSW0027,outcrop,Norris Lake (North End),086B05,Bear,Au,Resources Calculated,1154000,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,This showing is located 224 km NNE of Yellowknife.,, 64.3167,-115.2706,0,086BSW0002,outcrop,Kim,086B06,Slave,Au,Resources Calculated,1154600,,22-Oct-97,Source: Assessment Report,100 Metres,,,, 64.2956,-115.2667,0,086BSW0003,outcrop,Cass,086B06,Slave,Au-As,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,,,Mineralized quartz-carbonate veins and sulphides are deformed by the last deformation and thus predate it. 64.3975,-115.0856,0,086BSW0004,outcrop,Colomac,086B06,Slave,Au-Ag,Past Producer,1155000,,22-Oct-97,Source: Assessment Report,100 Metres,,"The Colomac deposit is located about 220 km northwest of Yellowknife, NWT. An airstrip allows access by fixed wing aircraft.",Mineralization is thought to have taken place between the two deformations but before the end of the second and regional metamorphism. 64.2867,-115.21,0,086BSW0019,outcrop,Leta (No. 1 Zone),086B06,Slave,Au,Resources Calculated,1069800,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 64.4931,-115.1292,0,086BSW0028,outcrop,Treasure Island,086B06,Slave,Au,Resources Calculated,1154100,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,This showing is 22 km N of Indin Lake., 64.275,-115.21,0,086BSW0029,outcrop,Indin Lake (Leta Arm) -1,086B06,Slave,Au,Resources Calculated,1154200,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 64.2633,-115.2167,0,086BSW0035,outcrop,North Inca (Indian Lake N,086B06,Slave,Au-Ag,Resources Calculated,1154901,,22-Oct-97,Method: Map/Airphoto,100 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 64.7347,-118.1861,0,086DNE0002,outcrop,CORMAC,086D09,Bear,U,Resources Calculated,926300,,22-Oct-97,Source: CANMINDEX,Unknown,"Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: Beaverlodge Lake Area Record modified according to National Mineral Inventory (NMI). Numerous occurrences, generally high grade pitchblende pods of restricted spatial extent. Numerous of these have been examined by drilling, open pits, or underground work including drifting and raising.",, 64.8167,-118.1667,0,086DNE0004,outcrop,PITCH 8,086D16,Bear,U,Resources Calculated,926500,086D16U 003,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: Hottah:lake Area Record modified according to National Mineral Inventory (NMI).,, 65.6042,-118.1153,0,086ENE0012,outcrop,Terra Mine,8.60E+10,Bear,Ag-Cu-Bi-Co-Ni-U-Zn-Au-As,Past Producer w/ Reserves,660300,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,"The Terra Mine is located on a peninsula in the Camsell River about 8 km SE of Great Bear Lake. From 1970 - 85 the mine produced 14,457,200 oz silver from 520,500 tons ore.", 65.5875,-117.9569,0,086FNW0010,outcrop,Norex Mine,086F12,Bear,Ag-Bi-Cu-Ni-Co-As-Pb,Past Producer w/ Reserves,517900,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 65.9944,-117.8,0,086FNW0021,outcrop,Contact Lake,086F13,Bear,Ag-U-Ra-Cu-Ni-Co-Bi-Mn-Zn-Pb,Past Producer w/ Reserves,929300,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: Camsell River Area,, 65.1681,-115.5667,0,086GSW0002,outcrop,Oldest Rocks,086G04,Slave,ExSt,Past Producer,,,1-Sep-98,Source: Assessment Report,500 Metres,,"The claim is aproximately 330 km NNW of the City of Yellowknife and 120 km SE of Great Bear Lake, covering an unnamed island on an unnamed lake which is part of the Acasta River System and located 18 km due South of Acasta Lake, NWT. The showing is located on the lakeshore at the East side of the island. This is the location where the original 3.962 Billion old rock sample was taken. ", 65.3825,-112.9858,0,086HSE0032,outcrop,REN,086H07,Slave,Au,Resources Calculated,1156900,,22-Oct-97,Source: Assessment Report,500 Metres,Updated & entered Jun30/93.,Float/ ski plane 300km NNE from Yellowknife to north arm of Point Lake 1km S. Lupin Mine airstrip and winter road terminus is 100km NE of showing.,"According to EGS 1985-8, at least 4 phases of Archean deformation, the oldest affecting only the basement to YK Supergroup, affected the area, as well as several generations of faulting/shearing. The cordierite isograd marking the transition to lower amphibolite facies is immediately east of the showing, so the showing itself is more or less at the greenschist - amphibolite boundary." 65.6311,-112.7989,0,086HNE0087,outcrop,Izok Lake,086H10,Slave,Cu-Zn-Pb-Ag,Resources Calculated,528400,,22-Oct-97,Source: Assessment Report,500 Metres,Update & enter Jul09/93.,Float/ski plane 330 km NNE of Yellowknife to Izok Lake.,"See Bostock 1980 (GSC Memoir 391); region was affected by polyphase Archean deformation involving early isoclinal folding, cross-folding, and fabric formation, and Archean regional metamorphism, followed by Proterozoic faulting. Grade is lower to middle amphibolite. syngenetic sulphides" 66.0342,-112.7094,0,086ISE0001,outcrop,Takijuq H-41,086I02,Slave,Zn-Cu-Ag,Resources Calculated,528700,,22-Oct-97,Source: Assessment Report,500 Metres,Updated and entered Jul12/93.,"Float/ski plane 400 km NNE of Yellowknife to Takijuq Lake, 8 km NW of deposit, or lakes 4 km north of it.","From Rockingham 1979: F1 produced a major syncline whose axis trends and plunges 70 degrees NE (showing is on its SE limb), and a bedding- parallel foliation. F2 produced minor north-south folds and crenulation lineations. Intrusion of late Archean granitic bodies post-dated deformation. Regional lower greenschist facies overprinted by later lower amphibolite contact metamorphism related to granite intrusion. A set of east trending dextral faults with less than 500 m horizontal displacement and a set of north trending faults with no apparent displacement transect the area. Syngenetic sulphides, partly re-mobilized during deformation and/or metamorphism?" 66.06,-112.7536,0,086ISE0002,outcrop,Takijuq H-10,086I02,Slave,Zn-Pb-Cu-Ag-Au,Resources Calculated,528600,,22-Oct-97,Source: Assessment Report,500 Metres,Updated and entered Jul13/93.,"Float/ski plane 400 km NNE of Yellowknife to Takijuq Lake, 5 km west of deposit, or Hanikahimajuk Lake 2 km NE of it.","From AR 060501, 1973: Deposit lies on SE limb of a regional (F1?) syncline whose axial plane is at 005 - 015 degrees/80 - 85 degrees SE regionally, affected by minor (F2?) folds whose axial planes strike north. From Rockingham 1979: F1 produced a major syncline whose axis trends and plunges 70 degrees NE (showing is on its SE limb), and a bedding-parallel foliation. F2 produced minor north-south folds and crenulation lineations. Intrusion of late Archean granitic bodies post-dated deformation. Regional lower greenschist facies overprinted by later lower amphibolite contact metamorphism related to granite intrusion. A set of east trending dextral faults with less than 500 m horizontal displacement and a set of north trending faults with no apparent displacement transect the area. From Gill 1976: Some of the mineralization is replacement (of amygdaloidal host) and some sedimentary (massive, banded sulphides)." 66.9167,-115.25,0,086OSW0097,outcrop,Muskox Intrusion,086J13,Bear,Cr-Cu-Ni-Pt-Pd,Resources Calculated,1077000,,22-Oct-97,Source: Government Report,Unknown,Location is the approximate center of the intrusive body., 66.4436,-117.5236,0,086KSW0006,outcrop,G W Group,086K05,Bear,Cu,Resources Calculated,529901,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 66.0847,-118.0361,0,086LSE0004,outcrop,Port Radium,086L01,Bear,U-Ra-Ag-Cu-Ni-Pb-Pota-Co-Zn-Bi-Mn,Past Producer w/ Reserves,927400,,22-Oct-97,Source: Government Report,Unknown,Also in CANMINDEX as 00530800., 66.0931,-118.0222,0,086LSE0006,outcrop,URANIUM Group,086L01,Bear,Cu-U-Ag,Past Producer w/ Reserves,927600,,22-Oct-97,Source: Government Report,Unknown,Also in CANMINDEX as 00530900. Great Bear Lake area. Part of the old workings of the Eldorado (Prot Radium) mine., 66.0028,-118.075,0,086LSE0007,outcrop,El Bonanza,086L01,Bear,Ag-Cu-U-Ni-Pb-Zn-Ind3-Mn-Co,Past Producer w/ Reserves,1075300,,22-Oct-97,Source: Government Report,Unknown,Also CANMINDEX Number, 67.3347,-116.45,0,086NSE0014,outcrop,Coronation Northwest Zone,086N08,Bear,Cu,Resources Calculated,501400,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 67.41,-116.4119,0,086NSE0121,outcrop,Wreck Lake,086N08,Bear,Cu,Resources Calculated,651800,,22-Oct-97,Method: Map/Airphoto,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 67.7333,-117.5931,0,086NNW0070,outcrop,CARL 7,086N12,Bear,Cu,Resources Calculated,507000,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 66.9167,-115.25,0,086OSW0097,outcrop,Muskox Intrusion,086O03,Bear,Cr-Cu-Ni-Pt-Pd,Resources Calculated,1077000,,22-Oct-97,Source: Government Report,Unknown,Location is the approximate center of the intrusive body., 67.5736,-115.0583,0,086ONW0084,outcrop,JUNE,086O11,Bear,Cu,Resources Calculated,553200,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 61.5389,-127.5625,0,095ENW0002,outcrop,RAM & ROD Groups,9.50E+13,Cordilleran,Pb-Zn-Ag,Resources Calculated,362100,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 61.5597,-124.7917,0,095FNE0013,outcrop,Prairie Creek,095F10,Cordilleran,Zn-Pb-Ag-Cu-Cd,Resources Calculated,534999,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 62.6942,-126.62,0,095LNE0007,outcrop,Coates Lake,095L10,Cordilleran,Cu-Ag,Resources Calculated,1085000,,22-Oct-97,Method: Map/Airphoto,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,"This showing lies 160 km west of Wrigley, YT." 63.7722,-127.8297,0,095MNW0001,outcrop,Jay (Keele River),095M13,Cordilleran,Cu,Resources Calculated,363200,,22-Oct-97,Source: CANMINDEX,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie, 63.8217,-127.9722,0,095MNW0038,outcrop,June Creek (Keele River),095M13,Cordilleran,Cu,Resources Calculated,1088100,,22-Oct-97,Method: Map/Airphoto,500 Metres,"Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie MR 223 lists the latitude and longitude as 63 degrees 45 minutes, 127 degrees 57 minutes.", 63.2167,-123.55,0,095OSW0006,outcrop,Wrigley,095O04,"Arctic, Interior & Hudson Platforms",Pb-Zn,Resources Calculated,,,26-Oct-98,Source: Government Report,1000 Metres,, 61.9717,-128.2683,0,105HNE0001,outcrop,Cantung,105H16,Cordilleran,W,Past Producer w/ Reserves,361200,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 62.475,-129.2583,0,105ISW0018,outcrop,Howards Pass (6km East of,105I06,Cordilleran,Zn-Pb,Resources Calculated,1148400,,22-Oct-97,Source: Publication/Thesis,1000 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,Howards Pass is located in the Cordillera Structural Province within the Mackenzie Mountain region along the Yukon-NWT border and 400 km west-northwest of Fort Simpson. Access to the property is by wheel equipped aircraft on to an old gravel airstrip and by ground transport on a now-abandoned all weather road connected to Yokons Nahanni Range Road.,"Two styles of deformation have been noted in the Howard Pass deposit. The first event noted was a localized compressional event causing small scale folding, pressure dissolution of quartz and carbonate, and dissolution and recrystallization of sphalerite, galena and pyrite. Regional compressional folding was the second deformational event observed in the area (Late Cretaceous)." 62.3708,-128.6167,0,105ISE0003,outcrop,Lened,105I07,Cordilleran,W-Cu,Resources Calculated,441000,,22-Oct-97,Method: Map/Airphoto,1000 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 62.7722,-128.6069,0,105INE0002,outcrop,PR,105I15,Cordilleran,Cu,Resources Calculated,440800,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,The showing is approximately 48 km NE of Howards Pass., 63.2847,-130.1528,0,105OSE0001,outcrop,Mactung,105O08,Cordilleran,W,Resources Calculated,,,26-Oct-98,Source: Government Report,1000 Metres,"Mactung is a Cretaceous aged tugsten skarn deposit formed by quartz monzonite intrusions within Cambrian aged shaley carbonates. The deposit is situated mostly with in the Yukon border (80 percent) but a small portion does occur within the NWT. Being the largest known tungsten deposit in North America it has a calculated resource of 6,100,000 tonnes grading 1.2 percent WO3 (underground) and 17,200,000 tonnes grading 0.8 percent WO3 accessable through open pit operations.",Mactung is situated 270 kilometres southwest of Norman Wells on the NWT-Yukon border at Macmillan Pass. Access to the property is by ground support via the Yukon/NWT Canol Heritage Trail., 64.0472,-129.4167,0,106ASW0002,outcrop,Bear-Twit,106A03,Cordilleran,Pb-Zn-Ag-Cu-Sb-Cd,Resources Calculated,158600,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 64.9333,-130.6833,0,106BNE0014,outcrop,Gayna River -1,106B15,Cordilleran,Zn-Pb,Resources Calculated,1153500,,22-Oct-97,Source: Government Report,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada. Administrative Region: District Of Mackenzie,, 65.25,-133.0333,0,106FSE0002,outcrop,Crest,106F02,Cordilleran,Fe,Resources Calculated,,,30-Oct-98,Source: Government Report,100 Metres,Crest is an iron deposit (third richest in North America) hosted in an Neoproterozoic iron formation formed in the basal portion of the Raptian Group of glacial-marine sediements. The showing is located in the norhteastern Cordillera along the NWT-Yukon border (Mackenzie Mountains). The iron formation consist of laminated hematite and jasper and is thought to have been formed in a marine environment associated with glacial waters and hydrothermal (rifting related) activities. Crest is the most iron-rich showing in the area with a resource of 5.6 billion tonnes grading 47.2%. Three structural fault blocks occur in the Rapitan Group of sediments exposing iron formation east of the Snake River. Crest is is situated in the most western fault block. ,Crest is situated in the Snake River area within the northern portion of the Mackenzie Mountains along the NWT-Yukon border and located 300 kilometres west of Normin Wells. Access to the property is by float or ski-euippped fixed-wing aircraft. A gravel strip was constructed in 1963 on the property.,