{"text_format":"dbase-jsonl-2026-09-30","columns":[{"name":"LONG","type":"number","width":11,"decimals":4},{"name":"LAT","type":"number","width":11,"decimals":4},{"name":"ELEV","type":"number","width":6,"decimals":0},{"name":"LAMBLONG","type":"number","width":12,"decimals":2},{"name":"LAMBLAT","type":"number","width":12,"decimals":2},{"name":"LAMBELEV","type":"number","width":6,"decimals":0},{"name":"STATNUM","type":"character","width":11},{"name":"STATYPE","type":"character","width":10},{"name":"AIRPHOTO","type":"character","width":10},{"name":"TRAVNUM","type":"number","width":8,"decimals":0},{"name":"OUTCRNUM","type":"number","width":8,"decimals":0},{"name":"SKETCH","type":"character","width":12},{"name":"NAME","type":"character","width":31},{"name":"NTS","type":"character","width":7},{"name":"PROVINCE","type":"character","width":10},{"name":"COMMOD","type":"character","width":16},{"name":"DEVSTAGE","type":"character","width":21},{"name":"CANMINID","type":"character","width":8},{"name":"NMIID","type":"character","width":13},{"name":"RECDATE","type":"character","width":10},{"name":"LOCATION","type":"character","width":26},{"name":"ACCURACY","type":"character","width":12},{"name":"COMMENT","type":"character","width":254},{"name":"ACCESS","type":"character","width":254},{"name":"REGDEF","type":"character","width":254},{"name":"LITHOTECT","type":"character","width":254},{"name":"BASENUMBER","type":"number","width":8,"decimals":0}],"n_rows":365,"rows_kept":365,"cut":false,"deleted_skipped":0,"read_ended":"whole","bounds":"16MiB/16384/4096/first_that_fit","version":"dbase_level_three","encoding_class":"enc_absent","reader":"statdb_count/9"}
[-76.1500,64.4667,0,866470.17,1816666.34,0,"036CSE0006","outcrop",null,null,null,null,"Ray","036C08","Churchill","U","Resources Calculated",null,null,"29-Sep-98","Source: Government Report","1000 Metres",null,null,null,null,733]
[-76.8056,69.6733,0,678078.53,2348825.99,0,"037CNE0010","outcrop",null,null,null,null,"Eqe Bay","037C09","Churchill","Fe","Resources Calculated","52399",null,"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.",null,null,734]
[-84.3333,73.0333,0,339921.73,2646387.91,0,"048CSE0002","outcrop",null,null,null,null,"Nanisivik","048C01","Churchill","Pb-Zn-Cd-Cu","Producer","822500",null,"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 acco",null,null,null,735]
[-95.9267,61.9800,0,-47141.55,1418886.69,0,"055ENW0007","outcrop",null,null,null,null,"Turquetil Lake Northwest","5.50E+1","Churchill","Au","Resources Calculated","1088600",null,"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.",null,null,736]
[-92.1781,62.9272,0,138967.65,1524023.16,0,"055JNW0001","outcrop",null,null,null,null,"Meliadine West","055J13","Churchill","Au","Resources Calculated",null,null,"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 mineral","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",null,null,737]
[-93.8628,62.1192,0,57579.65,1434108.72,0,"055KSW0041","outcrop",null,null,null,null,"Fat Lake","055K04","Churchill","Au","Resources Calculated","1088900",null,"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 fi","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 informati",null,738]
[-92.0833,62.8167,0,144180.46,1512302.51,0,"055KNE0083","outcrop",null,null,null,null,"North Rankin Nickel Mine","055K16","Churchill","Ni-Cu-Pt-Pd-Carv","Past Producer","532500",null,"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","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 structur",null,739]
[-92.1197,62.9042,0,141954.22,1521668.61,0,"055KNE0144","outcrop",null,null,null,null,"F-Zone","055K16","Churchill","Au","Resources Calculated",null,null,"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 th","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",null,null,740]
[-94.6253,62.3686,0,18814.18,1460612.79,0,"055LSE0056","outcrop",null,null,null,null,"Cache Zone","055L07","Churchill","Au","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"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 c",null,null,741]
[-95.7742,63.6903,0,-37134.07,1603641.62,0,"055MNW0002","outcrop",null,null,null,null,"Apr-68","055M12","Churchill","U","Resources Calculated","931800",null,"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.",null,null,null,742]
[-92.1928,62.9317,0,138222.74,1524477.04,0,"055NSE0001","outcrop",null,null,null,null,"Tiriruniak Zone","055N01","Churchill","Au","Resources Calculated",null,null,"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.  Resu","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",null,null,743]
[-94.5594,64.1694,0,20774.81,1655266.71,0,"056DSE0007","outcrop",null,null,null,null,"Feb-68","056D02","Churchill","U-Mo","Resources Calculated","932300",null,"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.",null,null,null,744]
[-98.5033,61.3067,0,-182138.82,1350744.46,0,"065GSE0009","outcrop",null,null,null,null,"Cullaton Lake South","065G07","Churchill","Au","Past Producer","1051700",null,"22-Oct-97","Source: Government Report","Unknown",null,"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",null,null,745]
[-98.5000,61.2833,0,-182106.64,1348207.61,0,"065GSE0016","outcrop",null,null,null,null,"Cullaton Mine","065G08","Churchill","Au","Past Producer","1052400",null,"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.",null,null,746]
[-96.2053,61.7731,0,-61736.45,1396755.56,0,"065HNE0001","outcrop",null,null,null,null,"Heninga Lake","065H16","Churchill","Zn-Cu-Ag-Au","Resources Calculated","159400",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,747]
[-96.8331,62.8733,0,-90458.08,1516417.62,0,"065INE0001","outcrop",null,null,null,null,"Ferguson Lake","065I15","Churchill","Cu-Ni-Pt-Pd","Resources Calculated","1088202",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"Located 225 km southwest of Baker Lake, NWT.  Property is accessable by float or ski-equipped fixed wing aircraft or helicopter.",null,null,748]
[-98.6333,62.5333,0,-181318.16,1483542.07,0,"065JNE0005","outcrop",null,null,null,null,"Lac Cinquante","065J10","Churchill","U","Resources Calculated",null,null,"1-Oct-98","Source: Government Report","1000 Metres",null,null,null,null,749]
[-97.6000,64.2833,0,-122056.88,1669999.85,0,"066ASW0002","outcrop",null,null,null,null,"Lone Gull","066A05","Churchill","U","Resources Calculated","959900",null,"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.",null,null,750]
[-96.3333,65.2667,0,-60376.52,1774435.46,0,"066GSE0001","outcrop",null,null,null,null,"Lost Lake","066G08","Churchill","U","Resources Calculated",null,null,"5-Oct-98","Source: Government Report","1000 Metres",null,null,null,null,751]
[-96.0469,65.0131,0,-47859.87,1746781.16,0,"066HSE0015","outcrop",null,null,null,null,"Third Portage Lake","066H01","Churchill","Au","Resources Calculated",null,null,"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 t","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 lowe",null,752]
[-96.0489,65.0250,0,-47930.08,1748068.87,0,"066HSE0016","outcrop",null,null,null,null,"Third Portage North Exten","066H01","Churchill","Au","Resources Calculated",null,null,"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","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 lowe",null,753]
[-96.0544,65.0036,0,-48219.73,1745760.02,0,"066HSE0017","outcrop",null,null,null,null,"Goose Island","066H01","Churchill","Au","Resources Calculated",null,null,"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","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 t","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 lowe",null,754]
[-96.9333,75.3861,0,-54013.79,2877800.88,0,"068HSE0003","outcrop",null,null,null,null,"Polaris","068H08","Innuitian","Zn-Pb-Ag-Cd","Producer","834200",null,"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.",null,null,null,755]
[-96.1675,75.5419,0,-32304.88,2894530.34,0,"068HNE0002","outcrop",null,null,null,null,"Eclipse","068H09","Innuitian","Zn-Pb-Cd-Ag","Resources Calculated","36100",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,756]
[-104.5267,60.2578,0,-510636.52,1270530.93,0,"075ASE0001","outcrop",null,null,null,null,"Nickel King","075A07","Churchill","Ni-Cu-Co-Ag","Resources Calculated","1038800",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"By float or ski-equipped fixed wing aircraft from Stony Rapids, Sask., 135 km to the southeast, or Points North, Sask.",null,null,757]
[-111.7922,61.3258,0,-862828.47,1462354.12,0,"075ESW0001","outcrop",null,null,null,null,"OConnor Lake","7.50E+0","Churchill","Zn-Pb-Cu","Resources Calculated","819199",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,758]
[-111.7789,61.3250,0,-862183.58,1462090.23,0,"075ESW0012","outcrop",null,null,null,null,"OConnor Lake","7.50E+0","Churchill","Pb-Zn","Past Producer","819102",null,"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.",null,null,null,759]
[-110.2400,61.3467,0,-784148.18,1444446.88,0,"075ESE0002","outcrop",null,null,null,null,"Dussault","7.50E+0","Churchill","U","Resources Calculated",null,null,"22-Oct-97","Source: Government Report","100 Metres",null,"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",null,760]
[-109.7833,61.4403,0,-758748.91,1448751.40,0,"075FSW0001","outcrop",null,null,null,null,"Salkeld Lake","075F05","Churchill","Cu-Ag-Zn-Pb-Au","Resources Calculated","656600",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,761]
[-111.8619,62.4097,0,-835616.91,1576414.30,0,"075LSW0001","outcrop",null,null,null,null,"Sachowia Lake","075L05","Slave","Ni-Co-Bi-Ag","Resources Calculated","957400",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,762]
[-111.5594,62.5825,0,-816161.04,1590525.57,0,"075LNW0002","outcrop",null,null,null,null,"BBX","075L12","Slave","Cu-Ag-Ni-Co-Bi-P","Resources Calculated","524200",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"147 km by float-plane or helicopter east from Yellowknife. One map shows an airstrip for the Great Slave Lodge.",null,null,763]
[-110.8144,63.0111,0,-768820.31,1626079.80,0,"075MSE0001","outcrop",null,null,null,null,"Susu Lake","075M02","Slave","Cu","Resources Calculated","657000","075M02CU 002","22-Oct-97","Source: Assessment Report","500 Metres",null,"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.",null,null,764]
[-110.9483,63.0322,0,-774627.64,1629914.26,0,"075MSE0002","outcrop",null,null,null,null,"BB","075M02","Slave","Zn-Pb-Ag-Cu","Resources Calculated","36203",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,765]
[-110.9633,63.0325,0,-775332.80,1630128.43,0,"075MSE0039","outcrop",null,null,null,null,"Kennedy Lake West","075M02","Slave","Cu-Ag-Zn","Resources Calculated","75M02CU0",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,766]
[-111.2325,64.0017,0,-761682.05,1734793.22,0,"076DSW0001","outcrop",null,null,null,null,"Deb","076D03","Slave","Cu-Zn-Ag-Pb","Resources Calculated","1096300","075M14CU 003","22-Oct-97","Source: Assessment Report","100 Metres",null,"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 Tund",null,null,767]
[-111.1683,64.0183,0,-758283.73,1735762.33,0,"076DSW0002","outcrop",null,null,null,null,"Perrson","076D03","Slave","Au","Resources Calculated",null,"076D03AU_06","22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,null,768]
[-111.2706,64.1178,0,-760255.88,1747389.37,0,"076DSW0003","outcrop",null,null,null,null,"Tundra","076D03","Slave","Au","Resources Calculated","1058701","076D03AU007","22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,null,769]
[-111.2500,64.0833,0,-760256.63,1743535.67,0,"076DSW0006","outcrop",null,null,null,null,"RED 24","076D03","Slave","Au","Past Producer","660500","076D03AU001","22-Oct-97","Source: Assessment Report","1000 Metres",null,"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 sout",null,null,770]
[-111.1997,64.0597,0,-758597.14,1740467.04,0,"076DSW0008","outcrop",null,null,null,null,"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.",null,null,771]
[-111.2061,64.0561,0,-758988.39,1740166.87,0,"076DSW0009","outcrop",null,null,null,null,"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.",null,null,772]
[-111.2411,64.0750,0,-760075.91,1742561.37,0,"076DSW0010","outcrop",null,null,null,null,"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.",null,null,773]
[-111.1933,64.0367,0,-758929.97,1737985.09,0,"076DSW0019","outcrop",null,null,null,null,"Tundra Mine","076D03","Slave","Au-Ag","Past Producer",null,null,"20-May-98","Source: Government Report","500 Metres",null,"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",null,null,774]
[-111.1672,64.0083,0,-758505.01,1734703.18,0,"076DSW0020","outcrop",null,null,null,null,"Saucer Zone","076D03","Slave","Au","Resources Calculated",null,null,"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",null,null,775]
[-111.4128,64.3081,0,-761504.37,1768982.61,0,"076DSW0004","outcrop",null,null,null,null,"Jax Lake","076D06","Slave","Au","Resources Calculated","1096100",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"The Jax showing lies north of Courageous Lake approximately 250 km NE of Yellowknife.",null,null,776]
[-110.1772,64.5614,0,-698843.45,1781336.57,0,"076DNE0024","outcrop",null,null,null,null,"Ekati - Misery","076D09","Slave","Diam","Resources Calculated",null,null,"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.",null,null,777]
[-110.6803,64.6583,0,-718989.69,1797110.85,0,"076DNE0020","outcrop",null,null,null,null,"Ekati - Fox Pipe","076D10","Slave","Diam","Resources Calculated",null,null,"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.",null,null,778]
[-110.6064,64.7167,0,-714136.29,1802400.72,0,"076DNE0021","outcrop",null,null,null,null,"Ekati - Koala","076D10","Slave","Diam","Resources Calculated",null,null,"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.",null,null,779]
[-110.5856,64.7264,0,-712949.29,1803184.48,0,"076DNE0023","outcrop",null,null,null,null,"Ekati - Panda","076D10","Slave","Diam","Producer",null,null,"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.",null,null,780]
[-110.6000,64.7167,0,-713849.33,1802328.87,0,"076DNW0001","outcrop",null,null,null,null,"Koala Lake Pipes","076D10","Slave","Diam","Resources Calculated",null,null,"6-Jan-98","Source: Government Report","1000 Metres",null,"There is a 1950 m airstrip nearby as well as the Lupin winter road.",null,null,781]
[-110.5128,64.8606,0,-706182.72,1816446.93,0,"076DNE0022","outcrop",null,null,null,null,"Ekati - Sable Pipe","076D15","Slave","Diam","Resources Calculated",null,null,"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.",null,null,782]
[-110.7833,65.6083,0,-698392.09,1897833.54,0,"076ENE0001","outcrop",null,null,null,null,"Butterfly","7.60E+1","Slave","Au","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"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 fa","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",783]
[-110.9686,65.5814,0,-707142.02,1897062.35,0,"076ENE0002","outcrop",null,null,null,null,"Jon","7.60E+1","Slave","Au","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"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 fa","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",784]
[-111.2056,65.6617,0,-715222.43,1908118.86,0,"076ENW0004","outcrop",null,null,null,null,"Pan","7.60E+1","Slave","Au","Resources Calculated","1059900",null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"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 fa","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",785]
[-111.7969,65.5628,0,-743511.95,1904563.08,0,"076ENW0005","outcrop",null,null,null,null,"Gondor","7.60E+1","Slave","Zn-Au-Ag-Cu-Pb","Resources Calculated",null,null,"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","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 de",null,786]
[-111.2250,65.7647,0,-713249.58,1919114.68,0,"076ENW0017","outcrop",null,null,null,null,"Lupin Mine","7.60E+1","Slave","Au-Ag","Past Producer","1060800",null,"22-Oct-97","Method: Map/Airphoto","15 Metres",null,"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.",null,null,787]
[-108.3631,65.9172,0,-586061.64,1905930.99,0,"076FNE0001","outcrop",null,null,null,null,"Hackett River","076F16","Slave","Zn-Pb-Cu-Ag-Au","Resources Calculated","1088302",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,788]
[-107.6208,65.3231,0,-566611.14,1836299.14,0,"076GSW0001","outcrop",null,null,null,null,"Musk","076G05","Slave","Zn-Pb-Cu-Ag-Au-N","Resources Calculated",null,null,"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.",null,789]
[-106.4278,65.5439,0,-509393.51,1849656.45,0,"076GNE0017","outcrop",null,null,null,null,"Goose Lake","076G09","Slave","Au","Resources Calculated",null,null,"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 uti","The iron formation has been complexly folded and has a metamorphic grade is middle greenschist to lower amphibolite.",null,790]
[-107.4764,65.9258,0,-547510.76,1898940.58,0,"076GNW0003","outcrop",null,null,null,null,"George Lake","076G14","Slave","Au","Resources Calculated",null,null,"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","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 of",null,791]
[-111.1944,66.3167,0,-696896.54,1976550.70,0,"076LSW0008","outcrop",null,null,null,null,"Gumbo Lake Ilmenite","076L06","Slave","Ti-V-Fe","Resources Calculated","1099100",null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"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).",null,792]
[-110.9706,66.9067,0,-671608.45,2035955.53,0,"076LNE0023","outcrop",null,null,null,null,"Ulu","076L15","Slave","Au-As-Bi-Zn-Ag-C","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"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-plungin",null,793]
[-110.8500,67.3814,0,-653968.40,2084491.73,0,"076MSE0053","outcrop",null,null,null,null,"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",null,794]
[-110.8436,67.3758,0,-653859.32,2083838.23,0,"076MSE0054","outcrop",null,null,null,null,"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",null,795]
[-111.3711,67.7175,0,-665733.29,2125140.09,0,"076MNW0084","outcrop",null,null,null,null,"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 fabr",null,796]
[-111.3583,67.7181,0,-665207.77,2125069.04,0,"076MNW0085","outcrop",null,null,null,null,"Fred Vein","076M11","Slave","Au","Resources Calculated",null,null,"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",null,797]
[-108.7861,67.0494,0,-577982.68,2029523.28,0,"076NSE0006","outcrop",null,null,null,null,"Pistol Lake","076N02","Slave","Au-Ag-Cu","Resources Calculated","308700","076N02AU 001","22-Oct-97","Source: Assessment Report","100 Metres",null,"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 a",null,798]
[-108.9403,67.2169,0,-580401.70,2048632.15,0,"076NSE0010","outcrop",null,null,null,null,"Turner Lake Main Gold","076N02","Slave","Au","Resources Calculated","1058900","076N02AU 002","22-Oct-97","Source: Assessment Report","500 Metres",null,"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 fol",null,799]
[-106.3500,67.6167,0,-466150.53,2069771.66,0,"076ONE0010","outcrop",null,null,null,null,"Boston","076O09","Slave","Au","Resources Calculated",null,null,"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 ki","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",null,null,800]
[-115.1564,60.7564,0,-1049567.25,1453894.81,0,"085BNE0001","outcrop",null,null,null,null,"Great Slave Reef","085B10","Arctic, In","Pb-Zn-Ind1","Resources Calculated","1132203",null,"22-Oct-97","Source: Assessment Report","5000 Metres",null,null,null,null,801]
[-115.0833,60.7500,0,-1046103.50,1452032.34,0,"085BNW0006","outcrop",null,null,null,null,"Great Slave Reef","085B11","Arctic, In","Pb-Zn-Cu","Resources Calculated","1132100",null,"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",null,null,null,802]
[-114.4417,60.8514,0,-1010447.10,1452107.58,0,"085BNE0004","outcrop",null,null,null,null,"Pine Point Mine","085B16","Arctic, In","Pb-Zn","Past Producer","808400",null,"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.",null,null,null,803]
[-112.3028,62.2281,0,-862206.93,1563369.74,0,"085ISE0001","outcrop",null,null,null,null,"Best Bet","085I01","Slave","Li-Be-Nb-Sn-Ta","Resources Calculated","1133100",null,"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",null,804]
[-112.2172,62.1825,0,-859364.65,1557461.67,0,"085ISE0002","outcrop",null,null,null,null,"Moose #2 Dyke","085I01","Slave","Li-Nb-Be-Ta-Sn","Resources Calculated","942100",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,null,805]
[-112.6961,62.1958,0,-882261.89,1565402.32,0,"085ISE0003","outcrop",null,null,null,null,"Lens","085I02","Slave","Li-Nb-Ta-Be","Resources Calculated","1133800",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,806]
[-112.7150,62.2253,0,-882302.86,1568731.09,0,"085ISE0004","outcrop",null,null,null,null,"Mut","085I02","Slave","Li","Resources Calculated","1133600",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"90km","Pegmatite intrusion",null,807]
[-112.7481,62.2183,0,-884116.89,1568463.12,0,"085ISE0005","outcrop",null,null,null,null,"Bin","085I02","Slave","Li-Nb-Ta-Be","Resources Calculated","1133700",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,null,"Pegmatite intrusion",null,808]
[-112.5997,62.1181,0,-879874.29,1555987.56,0,"085ISE0006","outcrop",null,null,null,null,"Thor Lake","085I02","Slave","Be-Ta-Th-Y-Ga-Ce","Resources Calculated","1133400",null,"22-Oct-97","Source: Assessment Report","15 Metres",null,"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.",null,null,809]
[-113.9847,62.4956,0,-935124.41,1614886.64,0,"085ISW0007","outcrop",null,null,null,null,"Big Hill East","085I05","Slave","Li","Resources Calculated","1134400",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,810]
[-113.3661,62.4189,0,-907881.70,1597987.72,0,"085ISW0009","outcrop",null,null,null,null,"Jake","085I06","Slave","Li-Sn-Ta-Nb","Resources Calculated","1134900",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,811]
[-113.3794,62.4133,0,-908693.27,1597597.33,0,"085ISW0010","outcrop",null,null,null,null,"Paint","085I06","Slave","Li-Ta-Nb","Resources Calculated","1134800",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,812]
[-113.4350,62.4756,0,-909440.14,1604846.79,0,"085ISW0011","outcrop",null,null,null,null,"Ann","085I06","Slave","Li","Resources Calculated","1134700",null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"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.",null,null,813]
[-112.8036,62.3081,0,-884127.05,1578566.36,0,"085ISE0012","outcrop",null,null,null,null,"Hid","085I07","Slave","Li","Resources Calculated","1136300",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,null,null,null,814]
[-112.7742,62.2992,0,-882970.67,1577233.18,0,"085ISE0013","outcrop",null,null,null,null,"Mac","085I07","Slave","Li-Ta-Nb","Resources Calculated","1136100",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"The Mac showing is approximately 6 km W of Buckham Lake and is accessible by float or ski equipped fixed wing aircraft.",null,null,815]
[-112.9078,62.4178,0,-885869.61,1591411.33,0,"085ISE0017","outcrop",null,null,null,null,"Norma","085I07","Slave","Au","Resources Calculated","1135400","085I07AU 005","22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,816]
[-112.8664,62.4278,0,-883576.15,1591874.07,0,"085ISE0018","outcrop",null,null,null,null,"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.",null,null,817]
[-112.7506,62.3414,0,-880572.19,1581291.49,0,"085ISE0019","outcrop",null,null,null,null,"Bullmoose","085I07","Slave","Ag-Au","Past Producer","1135000","085I07AU 001","22-Oct-97","Source: Assessment Report","100 Metres",null,"The deposit is 80 km east of Yellowknife, NWT, and may be reached from that point by air.",null,null,818]
[-112.5733,62.4653,0,-868349.08,1591735.19,0,"085ISE0020","outcrop",null,null,null,null,"Ruth Mine","085I07","Slave","Au-Ag-As-W","Past Producer","1135500","085I07AU 006","22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,819]
[-112.1803,62.4289,0,-850459.95,1582636.14,0,"085ISE0021","outcrop",null,null,null,null,"Thor","085I08","Slave","Li-Nb-Ta-Be","Resources Calculated","1080800",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,820]
[-112.6361,62.7311,0,-863507.47,1620229.03,0,"085INE0023","outcrop",null,null,null,null,"XL","085I10","Slave","Pb-Zn-Cu-Ag","Resources Calculated","442000",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"The prospect is approximately 91 km from Yellowknife, NWT, from which point it is accessable by float/ski-equipped aircraft.","Sulphide deposition",null,821]
[-112.6500,62.7236,0,-864392.58,1619638.12,0,"085INE0149","outcrop",null,null,null,null,"Turnback Lake","085I10","Slave","Be-Ind3","Resources Calculated","1143700",null,"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",null,null,null,822]
[-113.4656,62.5925,0,-907289.76,1617392.79,0,"085INW0028","outcrop",null,null,null,null,"KI","085I11","Slave","Li","Resources Calculated","1160300",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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 Lu","Pegmatite intrusion",null,823]
[-113.4717,62.5511,0,-908862.47,1613191.92,0,"085INW0029","outcrop",null,null,null,null,"Shorty","085I11","Slave","Li-Be-Sn","Resources Calculated","1136200",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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 Hid",null,null,824]
[-113.4944,62.5825,0,-908974.65,1616768.30,0,"085INW0033","outcrop",null,null,null,null,"FI Main Dyke","085I11","Slave","Li-Be","Resources Calculated","1160000",null,"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).",null,825]
[-113.4817,62.6400,0,-906587.41,1622541.92,0,"085INW0034","outcrop",null,null,null,null,"Freda","085I11","Slave","Ta-Nb-Sn-Ti-Li-B","Past Producer","1160600",null,"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% TiO","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?",null,826]
[-113.4656,62.6067,0,-906850.37,1618863.54,0,"085INW0037","outcrop",null,null,null,null,"Thompson-Lundmark","085I11","Slave","Au-Ag","Past Producer w/ Rese","1144000",null,"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 dur","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?",null,827]
[-113.4300,62.5414,0,-907168.11,1611591.86,0,"085INW0042","outcrop",null,null,null,null,"Jim Lit","085I11","Slave","Li-Be","Resources Calculated","1160100",null,"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).",null,828]
[-113.3489,62.7375,0,-897257.21,1630759.42,0,"085INW0048","outcrop",null,null,null,null,"Pensive Yellowknife Mine","085I11","Slave","Au","Past Producer","1144600",null,"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 aircraf",null,null,829]
[-113.1083,62.7442,0,-885610.31,1628082.12,0,"085INW0049","outcrop",null,null,null,null,"Peg Tantalum","085I11","Slave","Be-Ta-Nb-Sn","Past Producer","1144100",null,"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 J",null,null,830]
[-113.5297,62.7447,0,-905624.50,1634067.56,0,"085INW0077","outcrop",null,null,null,null,"Million Dollar","085I12","Slave","Au-Ag","Past Producer","1161100",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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?",null,831]
[-113.5339,62.7419,0,-905910.88,1633837.46,0,"085INW0078","outcrop",null,null,null,null,"Old Parr South","085I12","Slave","Au-Ag","Past Producer","1161100",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,832]
[-113.5067,62.5750,0,-909794.60,1616167.47,0,"085INW0079","outcrop",null,null,null,null,"FI Southwest Dyke","085I12","Slave","Li","Resources Calculated","1162000",null,"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).",null,833]
[-113.5631,62.8367,0,-904349.14,1644067.41,0,"085INW0084","outcrop",null,null,null,null,"Vo #2","085I13","Slave","Li-Be-P2O5","Resources Calculated","1162300",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,834]
[-113.5778,62.8339,0,-905131.96,1643986.66,0,"085INW0085","outcrop",null,null,null,null,"Vo #5","085I13","Slave","Li-Be-P2O5","Resources Calculated","1162300",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,835]
[-113.5817,62.8103,0,-906051.20,1641599.32,0,"085INW0158","outcrop",null,null,null,null,"Blaisdell Lake","085I13","Slave","Be-Li-Nb-Ta","Resources Calculated","1162200",null,"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",null,null,null,836]
[-113.3483,62.9625,0,-890310.02,1654066.18,0,"085INW0104","outcrop",null,null,null,null,"Mahe","085I14","Slave","Au","Resources Calculated","1081200",null,"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 3",null,null,null,837]
[-113.2381,62.7883,0,-890435.89,1634467.90,0,"085INW0105","outcrop",null,null,null,null,"MYRT","085I14","Slave","Au-Pb-Zn-Cu","Resources Calculated","1081300",null,"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.",null,null,838]
[-113.2328,62.9058,0,-886593.29,1646575.99,0,"085INW0132","outcrop",null,null,null,null,"Gordon Lake","085I14","Slave","Au-Ag-Cu-Pb-Zn","Past Producer w/ Rese","1141900",null,"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",null,null,839]
[-113.2042,62.9847,0,-882833.23,1654358.78,0,"085INW0133","outcrop",null,null,null,null,"Camlaren Mine","085I14","Slave","Au-Ag-Cu-Pb-Zn","Past Producer w/ Rese","1142000",null,"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",null,null,null,840]
[-113.4667,62.7667,0,-901951.83,1635450.55,0,"085INW0142","outcrop",null,null,null,null,"Mitchell Lake","085I14","Slave","Au-Ag-Pb","Resources Calculated","1142900",null,"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",null,null,null,841]
[-113.2806,62.7569,0,-893415.58,1631808.68,0,"085INW0155","outcrop",null,null,null,null,"Dome Lake (Southwest Side","085I14","Slave","Au-Ag-Pb","Resources Calculated","1161800",null,"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",null,null,null,842]
[-112.3781,62.8997,0,-846276.11,1634299.51,0,"085INE0086","outcrop",null,null,null,null,"Sunrise","085I16","Slave","Zn-Pb-Ag-Cu-Au","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,null,843]
[-112.3947,62.8928,0,-847265.68,1633802.38,0,"085INE0087","outcrop",null,null,null,null,"Bear","085I16","Slave","Zn-Pb-Ag-Au-Cu","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,844]
[-114.3658,62.4964,0,-953292.56,1620626.52,0,"085JSE0012","outcrop",null,null,null,null,"Giant Mine","085J08","Slave","Au-Ag-As","Producer","1163300",null,"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 worki","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 ci",null,"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), Helmsta",845]
[-114.3194,62.4664,0,-952049.21,1616837.29,0,"085JSE0013","outcrop",null,null,null,null,"Burwash Mine","085J08","Slave","Au","Past Producer","1163100",null,"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).",null,846]
[-114.4250,62.4958,0,-956135.19,1621453.23,0,"085JSE0050","outcrop",null,null,null,null,"Rod","085J08","Slave","Au-Ag","Resources Calculated","1163000",null,"22-Oct-97","Source: Government Report","100 Metres",null,"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,","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",847]
[-114.3689,62.4394,0,-955287.92,1614794.61,0,"085JSE0056","outcrop",null,null,null,null,"Con-Rycon","085J08","Slave","Au-Ag-Sb-Pb-Cu-Z","Producer","1163200",null,"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",null,null,null,848]
[-114.1808,62.5497,0,-942753.68,1623368.45,0,"085JNE0002","outcrop",null,null,null,null,"Cassidy Point","085J09","Slave","Au-Zn-Pb","Resources Calculated","1165400",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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 stra",null,849]
[-114.1969,62.5331,0,-944054.24,1621893.83,0,"085JNE0009","outcrop",null,null,null,null,"Tom Mine","085J09","Slave","Au-Cu-Pb-Zn","Past Producer","1165500",null,"22-Oct-97","Source: Government Report","100 Metres",null,"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",null,850]
[-114.1972,62.5192,0,-944515.20,1620463.60,0,"085JNE0010","outcrop",null,null,null,null,"Ptarmigan Mine","085J09","Slave","Au","Past Producer","1164200",null,"22-Oct-97","Source: Government Report","100 Metres",null,"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",null,851]
[-114.1692,62.5381,0,-942573.11,1621999.13,0,"085JNE0011","outcrop",null,null,null,null,"Vega","085J09","Slave","Au","Resources Calculated",null,null,"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",null,852]
[-114.3614,62.5806,0,-950354.67,1629244.17,0,"085JNE0014","outcrop",null,null,null,null,"Crestaurum","085J09","Slave","Au-Ag-Sb-Pb","Past Producer w/ Rese","1164300",null,"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",null,"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), Helmsta",853]
[-114.3481,62.5231,0,-951583.82,1623115.16,0,"085JNE0015","outcrop",null,null,null,null,"Supercrest","085J09","Slave","Au-Ag-As","Past Producer w/ Rese","1163400",null,"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 B",null,"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), Helmsta",854]
[-114.3600,62.5428,0,-951512.69,1625324.93,0,"085JNE0044","outcrop",null,null,null,null,"Lynx","085J09","Slave","Au","Resources Calculated","1165100",null,"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 S","The Vee Lake road off NWT Highway 4 provides excellent year-round access to the site.",null,"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).",855]
[-114.0097,62.5003,0,-936169.37,1615739.97,0,"085JNE0051","outcrop",null,null,null,null,"Big Hill West","085J09","Slave","Li","Resources Calculated","1164000",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,856]
[-116.3042,63.3514,0,-1014909.63,1738362.16,0,"085NSE0043","outcrop",null,null,null,null,"Camp Lake","085N08","Slave","Au-Zn-Pb-Cu","Resources Calculated","1168500",null,"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.",null,null,857]
[-116.1106,63.2675,0,-1008984.16,1726713.60,0,"085NSE0044","outcrop",null,null,null,null,"Slemon Lake","085N08","Slave","Au-Ag-Cu","Resources Calculated","1168600",null,"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.",null,null,858]
[-116.7403,63.5453,0,-1027854.12,1765133.07,0,"085NNE0001","outcrop",null,null,null,null,"Cab","085N10","Bear","Bi-Co-Cu-Au-As-W","Resources Calculated","1088400",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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",null,"Mineralization thought to be related to felsic magmatic and volcanic activity in Great Bear Magmatic Zone.",859]
[-116.7458,63.5500,0,-1027933.64,1765700.52,0,"085NNE0045","outcrop",null,null,null,null,"Lou Lake (Southeast of)","085N10","Slave","Bi-Co-Au-Cu-W","Resources Calculated","1168700",null,"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",null,null,null,860]
[-116.9167,63.7583,0,-1028086.81,1789661.75,0,"085NNE0035","outcrop",null,null,null,null,"SUE","085N15","Bear","Cu-Ag-U-Au-Fe","Resources Calculated","980200",null,"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 occur",null,null,null,861]
[-114.0539,63.1053,0,-918982.50,1678874.14,0,"085OSE0007","outcrop",null,null,null,null,"Viking Yellowknife","085O01","Slave","Au","Resources Calculated","1168900",null,"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","The property is southwest of Morris Lake and approximately 45 miles north-northeast of Yellowknife.",null,null,862]
[-115.8250,63.1811,0,-998831.71,1713370.55,0,"085OSW0001","outcrop",null,null,null,null,"Bugow","085O04","Slave","Au","Resources Calculated","1169500",null,"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.",null,null,863]
[-115.5181,63.0375,0,-989550.31,1693865.31,0,"085OSW0013","outcrop",null,null,null,null,"Mosher Lake","085O04","Slave","Au","Resources Calculated","1169600",null,"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.",null,null,864]
[-115.8239,63.1739,0,-999031.09,1712616.43,0,"085OSW0042","outcrop",null,null,null,null,"Cabin Lake","085O04","Slave","Au","Resources Calculated",null,null,"30-Jun-98","Source: Assessment Report","100 Metres",null,"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.",null,null,865]
[-113.7694,63.2494,0,-901135.20,1689694.78,0,"085PSW0001","outcrop",null,null,null,null,"Nicholas Lake","085P04","Slave","Au-Zn-Pb-As","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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 k",null,null,866]
[-113.8917,63.1867,0,-908817.11,1684953.00,0,"085PSW0032","outcrop",null,null,null,null,"Discovery Mine","085P04","Slave","Au-Pb-Cu","Past Producer","1171300",null,"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",null,null,null,867]
[-113.9222,63.1694,0,-910788.94,1683601.46,0,"085PSW0035","outcrop",null,null,null,null,"Winter Lake","085P04","Slave","Au","Resources Calculated","1171600",null,"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.",null,null,868]
[-113.5467,63.0992,0,-895416.61,1671009.30,0,"085PSW0037","outcrop",null,null,null,null,"Cross Lake","085P04","Slave","Au-Pb-Zn-Cu","Resources Calculated","1171800",null,"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.",null,null,869]
[-113.0403,63.2847,0,-866026.36,1683223.08,0,"085PSW0040","outcrop",null,null,null,null,"Gordon Lake","085P06","Slave","Au","Resources Calculated","1172100",null,"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.",null,null,870]
[-115.2183,64.1533,0,-937895.33,1803785.75,0,"086BSW0012","outcrop",null,null,null,null,"Anna (Barker Vein)","086B03","Slave","Au","Past Producer","1066300",null,"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 160","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.",null,871]
[-115.1139,64.1392,0,-933689.24,1800801.85,0,"086BSW0050","outcrop",null,null,null,null,"Horseshoe Zone","086B03","Slave","Au","Resources Calculated",null,null,"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 l","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","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).",null,872]
[-115.7583,64.4083,0,-953225.94,1837956.33,0,"086BSW0027","outcrop",null,null,null,null,"Norris Lake (North End)","086B05","Bear","Au","Resources Calculated","1154000",null,"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.",null,null,873]
[-115.2706,64.3167,0,-934705.58,1821328.67,0,"086BSW0002","outcrop",null,null,null,null,"Kim","086B06","Slave","Au","Resources Calculated","1154600",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,null,null,null,874]
[-115.2667,64.2956,0,-935246.27,1819105.67,0,"086BSW0003","outcrop",null,null,null,null,"Cass","086B06","Slave","Au-As","Resources Calculated",null,null,"22-Oct-97","Source: Assessment Report","100 Metres",null,null,"Mineralized quartz-carbonate veins and sulphides are deformed by the last deformation and thus predate it.",null,875]
[-115.0856,64.3975,0,-923749.73,1826923.12,0,"086BSW0004","outcrop",null,null,null,null,"Colomac","086B06","Slave","Au-Ag","Past Producer","1155000",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,876]
[-115.2100,64.2867,0,-933019.03,1817359.34,0,"086BSW0019","outcrop",null,null,null,null,"Leta (No. 1 Zone)","086B06","Slave","Au","Resources Calculated","1069800",null,"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",null,null,null,877]
[-115.1292,64.4931,0,-922471.98,1837376.53,0,"086BSW0028","outcrop",null,null,null,null,"Treasure Island","086B06","Slave","Au","Resources Calculated","1154100",null,"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.",null,null,878]
[-115.2100,64.2750,0,-933414.09,1816158.11,0,"086BSW0029","outcrop",null,null,null,null,"Indin Lake (Leta Arm) -1","086B06","Slave","Au","Resources Calculated","1154200",null,"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",null,null,null,879]
[-115.2167,64.2633,0,-934108.23,1815055.26,0,"086BSW0035","outcrop",null,null,null,null,"North Inca (Indian Lake N","086B06","Slave","Au-Ag","Resources Calculated","1154901",null,"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",null,null,null,880]
[-118.1861,64.7347,0,-1047427.05,1909343.68,0,"086DNE0002","outcrop",null,null,null,null,"CORMAC","086D09","Bear","U","Resources Calculated","926300",null,"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 hig",null,null,null,881]
[-118.1667,64.8167,0,-1043432.42,1917306.35,0,"086DNE0004","outcrop",null,null,null,null,"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).",null,null,null,882]
[-118.1153,65.6042,0,-1010957.45,1996039.34,0,"086ENE0012","outcrop",null,null,null,null,"Terra Mine","8.60E+1","Bear","Ag-Cu-Bi-Co-Ni-U","Past Producer w/ Rese","660300",null,"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.",null,null,883]
[-117.9569,65.5875,0,-1004972.00,1991840.57,0,"086FNW0010","outcrop",null,null,null,null,"Norex Mine","086F12","Bear","Ag-Bi-Cu-Ni-Co-A","Past Producer w/ Rese","517900",null,"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",null,null,null,884]
[-117.8000,65.9944,0,-982963.96,2030575.30,0,"086FNW0021","outcrop",null,null,null,null,"Contact Lake","086F13","Bear","Ag-U-Ra-Cu-Ni-Co","Past Producer w/ Rese","929300",null,"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",null,null,null,885]
[-115.5667,65.1681,0,-918642.50,1912969.96,0,"086GSW0002","outcrop",null,null,null,null,"Oldest Rocks","086G04","Slave","ExSt","Past Producer",null,null,"1-Sep-98","Source: Assessment Report","500 Metres",null,"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 loca",null,null,886]
[-112.9858,65.3825,0,-800215.68,1900219.97,0,"086HSE0032","outcrop",null,null,null,null,"REN","086H07","Slave","Au","Resources Calculated","1156900",null,"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 amp",null,887]
[-112.7989,65.6311,0,-784695.70,1923714.38,0,"086HNE0087","outcrop",null,null,null,null,"Izok Lake","086H10","Slave","Cu-Zn-Pb-Ag","Resources Calculated","528400",null,"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",null,888]
[-112.7094,66.0342,0,-768871.71,1964526.83,0,"086ISE0001","outcrop",null,null,null,null,"Takijuq H-41","086I02","Slave","Zn-Cu-Ag","Resources Calculated","528700",null,"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 grani",null,889]
[-112.7536,66.0600,0,-769971.86,1967744.26,0,"086ISE0002","outcrop",null,null,null,null,"Takijuq H-10","086I02","Slave","Zn-Pb-Cu-Ag-Au","Resources Calculated","528600",null,"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 s",null,890]
[-115.2500,66.9167,0,-845780.26,2088058.90,0,"086OSW0097","outcrop",null,null,null,null,"Muskox Intrusion","086O03","Bear","Cr-Cu-Ni-Pt-Pd","Resources Calculated","1077000",null,"22-Oct-97","Source: Government Report","Unknown","Location is the approximate center of the intrusive body.",null,null,null,891]
[-117.5236,66.4436,0,-954704.00,2071904.79,0,"086KSW0006","outcrop",null,null,null,null,"G W Group","086K05","Bear","Cu","Resources Calculated","529901",null,"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",null,null,null,892]
[-118.0361,66.0847,0,-989235.91,2043375.15,0,"086LSE0004","outcrop",null,null,null,null,"Port Radium","086L01","Bear","U-Ra-Ag-Cu-Ni-Pb","Past Producer w/ Rese","927400",null,"22-Oct-97","Source: Government Report","Unknown","Also in CANMINDEX as 00530800.",null,null,null,893]
[-118.0222,66.0931,0,-988343.59,2044008.73,0,"086LSE0006","outcrop",null,null,null,null,"URANIUM Group","086L01","Bear","Cu-U-Ag","Past Producer w/ Rese","927600",null,"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.",null,null,null,894]
[-118.0750,66.0028,0,-993976.06,2035699.01,0,"086LSE0007","outcrop",null,null,null,null,"El Bonanza","086L01","Bear","Ag-Cu-U-Ni-Pb-Zn","Past Producer w/ Rese","1075300",null,"22-Oct-97","Source: Government Report","Unknown","Also CANMINDEX Number",null,null,null,895]
[-116.4500,67.3347,0,-879069.19,2147175.21,0,"086NSE0014","outcrop",null,null,null,null,"Coronation Northwest Zone","086N08","Bear","Cu","Resources Calculated","501400",null,"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",null,null,null,896]
[-116.4119,67.4100,0,-874873.84,2154345.61,0,"086NSE0121","outcrop",null,null,null,null,"Wreck Lake","086N08","Bear","Cu","Resources Calculated","651800",null,"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",null,null,null,897]
[-117.5931,67.7333,0,-908967.60,2203854.80,0,"086NNW0070","outcrop",null,null,null,null,"CARL 7","086N12","Bear","Cu","Resources Calculated","507000",null,"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",null,null,null,898]
[-115.0583,67.5736,0,-815982.38,2153139.76,0,"086ONW0084","outcrop",null,null,null,null,"JUNE","086O11","Bear","Cu","Resources Calculated","553200",null,"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",null,null,null,899]
[-127.5625,61.5389,0,-1608475.90,1791798.30,0,"095ENW0002","outcrop",null,null,null,null,"RAM & ROD Groups","9.50E+1","Cordillera","Pb-Zn-Ag","Resources Calculated","362100",null,"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",null,null,null,900]
[-124.7917,61.5597,0,-1481277.01,1726475.17,0,"095FNE0013","outcrop",null,null,null,null,"Prairie Creek","095F10","Cordillera","Zn-Pb-Ag-Cu-Cd","Resources Calculated","534999",null,"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",null,null,null,901]
[-126.6200,62.6942,0,-1506314.30,1878072.09,0,"095LNE0007","outcrop",null,null,null,null,"Coates Lake","095L10","Cordillera","Cu-Ag","Resources Calculated","1085000",null,"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.",null,null,902]
[-127.8297,63.7722,0,-1501337.23,2008554.56,0,"095MNW0001","outcrop",null,null,null,null,"Jay (Keele River)","095M13","Cordillera","Cu","Resources Calculated","363200",null,"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",null,null,null,903]
[-127.9722,63.8217,0,-1504610.25,2016571.61,0,"095MNW0038","outcrop",null,null,null,null,"June Creek (Keele River)","095M13","Cordillera","Cu","Resources Calculated","1088100",null,"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.",null,null,null,904]
[-123.5500,63.2167,0,-1346107.53,1859511.05,0,"095OSW0006","outcrop",null,null,null,null,"Wrigley","095O04","Arctic, In","Pb-Zn","Resources Calculated",null,null,"26-Oct-98","Source: Government Report","1000 Metres",null,null,null,null,905]
[-128.2683,61.9717,0,-1616761.22,1850368.36,0,"105HNE0001","outcrop",null,null,null,null,"Cantung","105H16","Cordillera","W","Past Producer w/ Rese","361200",null,"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",null,null,null,906]
[-129.2583,62.4750,0,-1632295.07,1922581.51,0,"105ISW0018","outcrop",null,null,null,null,"Howards Pass (6km East of","105I06","Cordillera","Zn-Pb","Resources Calculated","1148400",null,"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 an","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 sphalerit",null,907]
[-128.6167,62.3708,0,-1610337.34,1896528.11,0,"105ISE0003","outcrop",null,null,null,null,"Lened","105I07","Cordillera","W-Cu","Resources Calculated","441000",null,"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",null,null,null,908]
[-128.6069,62.7722,0,-1588038.30,1933753.96,0,"105INE0002","outcrop",null,null,null,null,"PR","105I15","Cordillera","Cu","Resources Calculated","440800",null,"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.",null,null,909]
[-130.1528,63.2847,0,-1624605.05,2020296.75,0,"105OSE0001","outcrop",null,null,null,null,"Mactung","105O08","Cordillera","W","Resources Calculated",null,null,"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","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.",null,null,910]
[-129.4167,64.0472,0,-1551567.82,2072308.26,0,"106ASW0002","outcrop",null,null,null,null,"Bear-Twit","106A03","Cordillera","Pb-Zn-Ag-Cu-Sb-C","Resources Calculated","158600",null,"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",null,null,null,911]
[-130.6833,64.9333,0,-1551717.99,2184808.08,0,"106BNE0014","outcrop",null,null,null,null,"Gayna River -1","106B15","Cordillera","Zn-Pb","Resources Calculated","1153500",null,"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",null,null,null,912]
[-133.0333,65.2500,0,-1622604.09,2272106.15,0,"106FSE0002","outcrop",null,null,null,null,"Crest","106F02","Cordillera","Fe","Resources Calculated",null,null,"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","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",null,null,913]
[-110.2833,63.1083,0,-741008.40,1629969.84,0,"075MSE0028","outcrop",null,null,null,null,"JUF","075M01","Slave","U","Reconnaissance","940500","075M01U_001","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.  As well, this showing has been recorded as an NMI record.",null,null,null,914]
[-110.8144,63.0111,0,-768820.31,1626079.80,0,"075MSE0001","outcrop",null,null,null,null,"Susu Lake","075M02","Slave","Cu","Resources Calculated","657000","075M02CU 002","22-Oct-97","Source: Assessment Report","500 Metres",null,"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.",null,null,915]
[-110.9483,63.0322,0,-774627.64,1629914.26,0,"075MSE0002","outcrop",null,null,null,null,"BB","075M02","Slave","Zn-Pb-Ag-Cu","Resources Calculated","36203",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,916]
[-110.7628,63.0411,0,-765568.05,1628600.57,0,"075MSE0005","outcrop",null,null,null,null,"COTTONGRASS Au","075M02","Slave","Au","Reconnaissance",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The COTTONGRASS Au showing is located 200 km NE of Yellowknife, NWT and can be accessed by fixed wing float-equipped aircraft.",null,null,917]
[-110.9356,63.1364,0,-771231.57,1640670.31,0,"075MSE0006","outcrop",null,null,null,null,"Dawn & Gem-1","075M02","Slave","Zn-Pb-Ag-Cu","Drilled","656700",null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The Dawn & Gem-1 showing is approximately 120 miles NE of Yellowknife and is accessible by float or ski equipped airplane.",null,null,918]
[-110.9533,63.1281,0,-772292.82,1640016.03,0,"075MSE0007","outcrop",null,null,null,null,"Dawn & Gem-2","075M02","Slave","Cu-Zn-Ag-As","Drilled","656800",null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The Dawn & Gem-2 showing is approximately 120 miles NE of Yellowknife and is accessible by float or ski equipped airplane.",null,null,919]
[-110.6783,63.0936,0,-760163.18,1633089.07,0,"075MSE0008","outcrop",null,null,null,null,"Plex Lake","075M02","Slave","Cu","Observed Ore Mineral","656900",null,"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.  The showing is located 3 miles ESE of Plex Lake.",null,null,null,920]
[-110.7781,63.0753,0,-765388.28,1632368.13,0,"075MSE0009","outcrop",null,null,null,null,"Susu Lake North","075M02","Slave","Cu","Reconnaissance","657100",null,"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.  Showing is located 4 miles north of Susu Lake.",null,null,null,921]
[-110.9511,63.0042,0,-775511.80,1627016.65,0,"075MSE0010","outcrop",null,null,null,null,"5 Mi West of Susu Lake","075M02","Slave","Cu","Observed Ore Mineral","657200",null,"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.  Showing is located 5 miles west of Susu Lake.",null,null,null,922]
[-110.9347,63.0817,0,-772654.60,1634931.83,0,"075MSE0017","outcrop",null,null,null,null,"Brislane Lake-1","075M02","Slave","Cu","Reconnaissance","657900",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"The showing property lies approximately 135 miles NE of Yelllowknife and is accessible by float or ski equipped airplane.",null,null,923]
[-110.9108,63.0683,0,-771878.53,1633238.48,0,"075MSE0018","outcrop",null,null,null,null,"Brislane Lake-2","075M02","Slave","Au-Cu","Reconnaissance","658000",null,"22-Oct-97","Source: Assessment Report","100 Metres",null,"The Brislane Lake-2 showing is approximately 135 miles from Yellowknife, and is accessible by float or ski equipped airplane.",null,null,924]
[-110.9506,63.0644,0,-773873.36,1633313.72,0,"075MSE0019","outcrop",null,null,null,null,"BRI-8","075M02","Slave","Cu-Au","Undrilled",null,null,"22-Oct-97","Source: Assessment Report","100 Metres","In AR 083129 reference to work done in the 1950s in which 4 trenches and small pits were explored was made although no original report was located on the work.","The Bri-8 showing is approximately 190 km north-east of Yellowknife, and is accessible by ski or float equipped aircraft.",null,null,925]
[-110.9111,63.0997,0,-771052.65,1636530.30,0,"075MSE0020","outcrop",null,null,null,null,"Taco Island","075M02","Slave","Cu-Au","Undrilled",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The Taco Island showing is approximately 190 km north-east of Yellowknife and is accessible by ski or float equipped aircraft.","Metamorphism is said to be skarn-type metamorphism and is assumed to be equivalent to middle amphibolite facies.",null,926]
[-110.9433,63.0500,0,-773912.68,1631717.15,0,"075MSE0021","outcrop",null,null,null,null,"Brislane Lake-5","075M02","Slave","Cu","Observed Ore Mineral","658300",null,"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.",null,null,null,927]
[-110.9625,63.0458,0,-774937.78,1631511.17,0,"075MSE0022","outcrop",null,null,null,null,"Brislane Lake-6","075M02","Slave","Cu","Observed Ore Mineral","658400",null,"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.",null,null,null,928]
[-110.9397,63.0439,0,-773905.11,1631034.63,0,"075MSE0023","outcrop",null,null,null,null,"BRI 6","075M02","Slave","Cu-Au","Reconnaissance",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The BRI 6 showing is approximately 190 km north-east of Yellowknife and is accessible by ski or float equipped aircraft.",null,null,929]
[-110.9131,63.0756,0,-771792.43,1634030.84,0,"075MSE0024","outcrop",null,null,null,null,"BRI 3","075M02","Slave","Cu","Reconnaissance",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The BRI 3 showing is approximately 190 km north-east of Yellowknife and is accessible by ski or float aircraft.",null,null,930]
[-110.8939,63.0406,0,-771816.17,1630132.56,0,"075MSE0025","outcrop",null,null,null,null,"Brislane Lake - 11","075M02","Slave","Cu","Observed Ore Mineral","658700",null,"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.",null,null,null,931]
[-110.9017,63.0400,0,-772203.07,1630164.40,0,"075MSE0026","outcrop",null,null,null,null,"Brislane Lake - 12","075M02","Slave","Cu","Observed Ore Mineral","658800",null,"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.",null,null,null,932]
[-110.9219,63.0944,0,-771706.94,1636106.28,0,"075MSE0027","outcrop",null,null,null,null,"BRI 5","075M02","Slave","Cu","Reconnaissance",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The BRI 5 showing is approximately 190 km north-east of Yellowknife and is accessible by ski or float equipped aircraft.",null,null,933]
[-110.7967,63.0233,0,-767653.47,1627144.15,0,"075MSE0029","outcrop",null,null,null,null,"Susu Lake West","075M02","Slave","Cu","Observed Ore Mineral","1055500",null,"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 0.5 miles west of Susu Lake.  The only record of the showing is from GSC map 119",null,null,null,934]
[-110.7783,63.0561,0,-765907.30,1630358.85,0,"075MSE0030","outcrop",null,null,null,null,"COTTONGRASS Cu","075M02","Slave","Cu","Reconnaissance",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The area is approximately 200 km NE of Yellowknife and is accessible by ski or float equipped airplane.",null,null,935]
[-110.8683,63.0319,0,-770831.11,1628910.95,0,"075MSE0031","outcrop",null,null,null,null,"Susu Lake West 2","075M02","Slave","Cu","Observed Ore Mineral","1055700",null,"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.  Showing is located 3 miles west of Susu Lake.",null,null,null,936]
[-110.9208,63.1078,0,-771296.00,1637496.11,0,"075MSE0032","outcrop",null,null,null,null,"HO 16","075M02","Slave","Cu-Ag-Zn","Drilled","1055800","075M02CU 007","22-Oct-97","Source: Government Report","100 Metres","The information for this showing is from NMI Cu references.","The HO 16 showing is approximately 120 miles north-east of Yellowknife and is accessible by float or ski equipped aircraft.",null,null,937]
[-110.8994,63.1122,0,-770163.32,1637697.57,0,"075MSE0033","outcrop",null,null,null,null,"Pb No. 5","075M02","Slave","Cu-Zn","Drilled","1055900","075M02CU 006","22-Oct-97","Source: Assessment Report","100 Metres","This showing has been derived from the NMI records.","The Pb No. 5 showing is approximately 130 miles north-east of Yellowknife and is accessible by ski or float equipped aircraft.",null,null,938]
[-110.9236,63.1089,0,-771399.35,1637645.25,0,"075MSE0034","outcrop",null,null,null,null,"FLO","075M02","Slave","Cu","Drilled","1056000","075M02CU 010","22-Oct-97","Source: Government Report","Unknown","The FLO showing is referenced in the NMI Cu book.","The FLO showing is approximately 130 miles north-east of Yellowknife and is accessible by float or ski aircraft.",null,null,939]
[-110.9633,63.0325,0,-775332.80,1630128.43,0,"075MSE0039","outcrop",null,null,null,null,"Kennedy Lake West","075M02","Slave","Cu-Ag-Zn","Resources Calculated",null,"75M02CU012","22-Oct-97","Source: Assessment Report","100 Metres",null,"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.",null,null,940]
[-110.9333,63.1167,0,-771650.41,1638579.66,0,"075MSE0040","outcrop",null,null,null,null,"VOY","075M02","Slave","Cu-Zn-Ag","Observed Ore Mineral","1056600",null,"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.",null,null,null,941]
[-110.9119,63.1211,0,-770518.00,1638780.97,0,"075MSE0041","outcrop",null,null,null,null,"Benny Bay Zone","075M02","Slave","Zn-Ag-Pb-Cu","Drilled",null,null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The Benny Bay Zone is approximately 120 miles north-east of Yellowknife and is accessible by ski or floated equipped aircraft.",null,null,942]
[-110.9267,63.1386,0,-770750.96,1640792.79,0,"075MSE0042","outcrop",null,null,null,null,"Northern Zinc Zone","075M02","Slave","Zn-Cu-Pb","Drilled","1056800",null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The Northern Zinc Zone showing is approximately 120 miles north-east of Yellowknife and is accessible by float or ski equipped aircraft.",null,null,943]
[-110.9436,63.1181,0,-772101.22,1638851.24,0,"075MSE0043","outcrop",null,null,null,null,"No. 2 Copper Zone","075M02","Slave","Cu-Zn-Ag","Drilled","1057100",null,"22-Oct-97","Source: Assessment Report","30 Metres",null,"The No. 2 Copper Zone showing is approximately 120 miles NE of Yellowknife and is accessible by float or ski equipped aircraft.",null,null,944]
[-110.6367,63.0117,0,-760341.36,1624006.62,0,"075MSE0044","outcrop",null,null,null,null,"Susu Lake East","075M02","Slave","Be-Nb-Ta","Observed Lithology","1093800",null,"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.",null,null,null,945]
[-110.9000,63.1667,0,-768734.59,1643412.22,0,"075MSE0045","outcrop",null,null,null,null,"Brislane Lake","075M02","Slave","Zn","Observed Ore Mineral","1093900",null,"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 1 km north of Brislane Lake.",null,null,null,946]
[-111.6708,63.3561,0,-799860.52,1672720.09,0,"075MSW0011","outcrop",null,null,null,null,"HART","075M05","Slave","Zn","Drilled","657300","075M05CU 002","22-Oct-97","Source: Assessment Report","500 Metres","A drill hole testing an HLEM conductor in 1967 yielded a best intersection of 0.26% Zn over 3 feet.",null,null,null,947]
[-111.5625,63.4250,0,-792865.50,1678558.05,0,"075MSW0012","outcrop",null,null,null,null,"TIP","075M05","Slave","Au-Cu-Ag-As","Drilled","657400",null,"22-Oct-97","Source: Assessment Report","500 Metres","There is also a notable copper showing 1000 m NNE (up strike) of the TIP showing where Nebex Resources (Assessment report 083232) sampled a peice of float which assayed 4% copper.","The Tip showing is located one and a half km north east of the Asp showing on the west shore of Lac du Rocher approximately 174 km northeast of Yellowknife NWT. The property is accessable by float or ski equiped aircraft or by helicopter from Yellowknife",null,null,948]
[-111.8317,63.3539,0,-807462.50,1674523.48,0,"075MSW0015","outcrop",null,null,null,null,"SAN","075M05","Slave","Cu-Zn-Ni","Drilled","657700",null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"The SAN Showing is two km due north of the north shore of Rivett Lake and one km south of the Beaulieu River, approximately 158 km northeast of Yellowknife NWT. The property is accessable by float or ski equiped aircraft or by helicopter from Yellowknife",null,null,949]
[-111.6556,63.2819,0,-801224.00,1664782.95,0,"075MSW0038","outcrop",null,null,null,null,"LEN","075M05","Slave","Au-Cu-Ni","Drilled","1056400",null,"22-Oct-97","To Be Determined","Unknown",null,"The LEN showing is located on the south west shore of Lac Sans Disant south of Camsell lake, approximately 180 km northeast of Yellowknife NWT.  It can be accessed from Yellowknife, via helicopter or float or ski-equipped fixed wing aircraft.",null,null,950]
[-111.5972,63.3944,0,-795342.01,1675795.81,0,"075MSW0039","outcrop",null,null,null,null,"Asp","075M05","Slave","Au","Reconnaissance",null,null,"13-Aug-98","Source: Assessment Report","1000 Metres","The Wind zone is a small satelite zone 200 m NNE of the Asp zone with similar mineralization in an up to 2 foot wide quartz vein.  The best assay returned to date is 18 g/t silver and .66% copper.(Nebex Resources 083232, 1993)","The Asp showing is located one and a half km south west of the TIP showing on the west shore of Lac du Rocher approximately 170 km north east of Yellowknife NWT. The property is accessable by float or ski equiped aircraft or by helicopter from Yellowknif",null,null,951]
[-111.5167,63.4542,0,-789912.27,1681037.96,0,"075MSW0040","outcrop",null,null,null,null,"Canoe","075M05","Slave","Au-Ag-Pb-Zn-Cu","Reconnaissance",null,null,"14-Aug-98","Source: Assessment Report","500 Metres",null,"The Tip showing is located one and a half km northeast of the Asp showing on the west shore of Lac du Rocher approximately 174 km north east of Yellowknife NWT. The property is accessable by float or ski equiped aircraft or by helicopter from Yellowknife",null,null,952]
[-111.6000,63.3750,0,-796014.13,1673805.12,0,"075MSW0041","outcrop",null,null,null,null,"WK","075M05","Slave","Cu-Ag","Reconnaissance",null,null,"14-Aug-98","Source: Assessment Report","500 Metres",null,"The WK showing is located six km SSW of the TIP showing on the west shore of Lac du Rocher approximately 165 km north east of Yellowknife NWT. The property is accessable by float or ski equiped aircraft or by helicopter from Yellowknife.",null,null,953]
[-111.8514,63.3589,0,-808243.86,1675295.25,0,"075MSW0042","outcrop",null,null,null,null,"C3","075M05","Slave","Zn-Cu","Undrilled",null,"075M05CU 005","18-Sep-98","Source: Assessment Report","500 Metres",null,"This occurrence is located and immediately south of the Beaulieu River, approximately 180 km northeast of Yellowknife NWT.  It can be accessed from Yellowknife via float- or ski-equipped fixed wing aircraft.",null,null,954]
[-111.7597,63.3608,0,-803894.72,1674331.37,0,"075MSW0044","outcrop",null,null,null,null,"P2","075M05","Slave","Cu-Zn-Ni","Undrilled",null,null,"18-Sep-98","Source: Assessment Report","500 Metres",null,null,null,null,955]
[-110.1625,63.5706,0,-723465.06,1677119.88,0,"075MNE0015","outcrop",null,null,null,null,"CL 25","075M09","Slave","Diam","Drilled",null,null,"10-Aug-98","Source: Assessment Report","30 Metres",null,"The CL 25 showing is approximately 190 km northeast of Yellowknife and is accessible by ski or float equipped aircraft.","The region has been metamorphosed although the kimberlite pipe has not.",null,956]
[-110.1628,63.5711,0,-723466.34,1677175.80,0,"075MNE0016","outcrop",null,null,null,null,"CL 174","075M09","Slave","Diam","Drilled",null,null,"21-Aug-98","Source: Media/News Release","30 Metres",null,"The CL 174 showing is approximately 190 km northeast of Yellowknife and is accessible by ski or float equipped aircraft.  As well, the Salmita airstrip which can accommodate a Hercules airplane is about 50 km north of the showing.","The Camsell Lake area has undergone metamorphism although the kimberlite has not and thus no facies will be entered.",null,957]
[-110.9833,63.6167,0,-760583.98,1691529.22,0,"075MNE0013","outcrop",null,null,null,null,"DOD","075M10","Slave","Cu-Ni","Drilled","657500",null,"22-Oct-97","Source: Government Report","100 Metres","Location of showing determined from Cu Commodity File.","The DOD showing is located approximately 130 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft.",null,null,958]
[-110.9000,63.6167,0,-756703.19,1690535.69,0,"075MNE0014","outcrop",null,null,null,null,"EGO","075M10","Slave","Cu-Zn","Observed Ore Mineral","657600",null,"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 approximately 130 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft.",null,null,959]
[-110.8017,63.5908,0,-752810.18,1686656.55,0,"075MNE0017","outcrop",null,null,null,null,"CL 186","075M10","Slave","Diam","Drilled",null,null,"24-Aug-98","Source: Media/News Release","30 Metres",null,"The CL 186 showing is approximately 140 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft.","Although the surrounding rock is metamorphosed, the kimberlite is not and this no metamorphic facies has been entered.",null,960]
[-110.7281,63.5925,0,-749330.75,1685965.59,0,"075MNE0018","outcrop",null,null,null,null,"Snap Lake Dyke","075M10","Slave","Diam","Drilled",null,null,"26-Aug-98","Source: Media/News Release","30 Metres",null,"The Snap Lake showing is approximately 140 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft.","No metamorphic facies has been entered as the kimberlite has not been metamorphosed.",null,961]
[-110.8619,63.6089,0,-755135.80,1689266.04,0,"075MNE0019","outcrop",null,null,null,null,"Snap Lake Boulders","075M10","Slave","Diam","Undrilled",null,null,"26-Aug-98","Source: Media/News Release","30 Metres",null,"The Snap Lake boulders are approximately 140 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft.",null,null,962]
[-111.1208,63.5806,0,-767965.28,1689403.43,0,"075MNW0016","outcrop",null,null,null,null,"CAM","075M11","Slave","Cu-Zn","Drilled","657800",null,"22-Oct-97","Source: Assessment Report","500 Metres","Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District of Mackenzie.","The CAM showing is located 1 km inland from the SE shore of Camsell Lake, 1 1/2 km SW of Timber Bay and about 215 km NE of Yellowknife NWT.  The property is accessable from Yellowkmife via helicopter or float or ski-equiped aircraft.",null,null,963]
[-111.0139,63.6083,0,-762235.41,1691016.26,0,"075MNW0035","outcrop",null,null,null,null,"PEP","075M11","Slave","Cu-Zn","Drilled","1056100",null,"22-Oct-97","Source: Assessment Report","500 Metres","Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District of Mackenzie.","The PEP showing is located 2 km inland from the SE shore of Camsell Lake, 4 km ENE of Timber Bay, 6 km NE of the CAM showing, and about 215 km NE of Yellowknife NWT.  The property is accessable from Yellowkmife via helicopter or float or ski-equiped airc",null,null,964]
[-111.9578,63.5622,0,-807437.28,1697847.25,0,"075MNW0004","outcrop",null,null,null,null,"BAY Group","075M12","Slave",null,"Below Cutoff - Drille","442600",null,"22-Oct-97","Source: Assessment Report","500 Metres","One drill hole in 1974 tested a magnetic - EM - soil geochemical anomaly in sheared and altered andesite. It cut pyrrhotite and minor chalcopyrite as breccia filling in andesite. Samples were assayed for Au, Ag, Cu, Pb, and Zn; the highest detectable res","Float or ski equiped aircraft to Esker Lake.",null,null,965]
[-111.2208,63.9944,0,-761344.03,1733889.73,0,"075MNW0003","outcrop",null,null,null,null,"TALL2","075M14","Slave","Zn","Drilled",null,null,"22-Oct-97","Source: Assessment Report","500 Metres",null,"The property is situated approximately 230 km northeast of Yellowknife NWT, 14 km south of  the old Tundra mine, and 18 km south of the Salmita mine.  It can be accessed from Yellowknife, via helicopter or float or ski-equipped fixed wing aircraft.  The",null,null,966]
[-111.2208,64.0000,0,-761191.36,1734475.38,0,"075MNW0036","outcrop",null,null,null,null,"SECUM","075M14","Slave","Cu","Observed Lithology","1056200",null,"22-Oct-97","Source: Assessment Report","1000 Metres","Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District of Mackenzie.","The property is situated approximately 230 km northeast of Yellowknife NWT, 13 km south of  the old Tundra mine, and 17 km south of the Salmita mine.  It can be accessed from Yellowknife,  via helicopter or float or ski-equipped fixed wing aircraft.  The",null,null,967]
[-111.2278,64.0000,0,-761512.69,1734559.17,0,"075MNW0037","outcrop",null,null,null,null,"KM","075M14","Slave","Cu","Observed Ore Mineral","1056300",null,"22-Oct-97","Method: Map/Airphoto","1000 Metres","During 1948 500 feet of diamond drilling was recorded on the KM12 claim by J. McAvoy for  Cunaxa Mining Ltd.  No further work has been recorded.","The property is situated approximately 230 km northeast of Yellowknife NWT, 13 km south of the old Tundra mine, and 17 km south of the Salmita mine.  It can be accessed from Yellowknife, via helicopter or float or ski-equipped fixed wing aircraft.  The S",null,null,968]
[-111.1667,63.9833,0,-759161.43,1732082.12,0,"075MNW0046","outcrop",null,null,null,null,"Mackay Lake Nodica Narrows","075M14","Slave","Au-As","Observed Ore Mineral","1094000",null,"22-Oct-97","Method: Map/Airphoto","5000 Metres",null,"The deposit is located near the northeast shore of MacKay Lake, approximately 235 km northeast  of Yellowkmife NWT, from which it can be reached by float or ski-epuipped aircraft.  The Lupin ice road runs within a few kms to the west of the property, and",null,null,969]
[-111.1556,63.9611,0,-759254.33,1729627.38,0,"075MNW0047","outcrop",null,null,null,null,"BERTHA 5","075M14","Slave","Au","Reconnaissance",null,null,"10-Aug-98","Source: Assessment Report","1000 Metres",null,"The Bertha 5 showing is located 1km inland from MacKay Lake north of Nodinka Narrows.  The property is situated approximately 230 km northeast of Yellowknife NWT, 10 km south of  the old Tundra mine, and 16 km south of the Salmita mine.  It can be access",null,null,970]
[-111.1611,63.9694,0,-759281.75,1730561.27,0,"075MNW0048","outcrop",null,null,null,null,"BERTHA 6","075M14","Slave","Au","Reconnaissance",null,null,"10-Aug-98","Source: Assessment Report","500 Metres",null,"The BERTHA 6 showing is located 1 km inland from MacKay Lake north of Nodinka Narrows.  The property is situated approximately 230 km northeast of Yellowknife NWT, 9 km south of the old Tundra mine, and 15 km south of the Salmita mine.  It can be accesse",null,null,971]
[-111.1792,63.9514,0,-760603.23,1728894.69,0,"075MNW0049","outcrop",null,null,null,null,"TALL","075M14","Slave","Au","Reconnaissance",null,null,"11-Aug-98","Source: Assessment Report","1000 Metres",null,"The TALL showing is located on the shore of MacKay Lake north of Nodinka Narrows.  The property is situated approximately 230 km northeast of Yellowknife NWT, 11 km south of  the old Tundra mine, and 17 km south of the Salmita mine.  It can be accessed f",null,null,972]
[-111.0972,63.8489,0,-759604.86,1717191.70,0,"075MNW0050","outcrop",null,null,null,null,"HARE 8","075M14","Slave","Au","Reconnaissance",null,null,"11-Aug-98","Source: Assessment Report","100 Metres",null,"The HARE 8 showing is located 2 km inland from the north shore of Portage Bay, MacKay Lake. The property is situated approximately 225 km northeast of Yellowknife NWT, 20 km south of  the old Tundra mine, and 26 km south of the Salmita mine.  It can be a",null,null,973]
[-111.2278,64.0000,0,-761512.69,1734559.17,0,"075MNW0037","outcrop",null,null,null,null,"KM","075N03","Slave","Cu","Observed Ore Mineral","1056300",null,"22-Oct-97","Method: Map/Airphoto","1000 Metres","During 1948 500 feet of diamond drilling was recorded on the KM12 claim by J. McAvoy for  Cunaxa Mining Ltd.  No further work has been recorded.","The property is situated approximately 230 km northeast of Yellowknife NWT, 13 km south of the old Tundra mine, and 17 km south of the Salmita mine.  It can be accessed from Yellowknife, via helicopter or float or ski-equipped fixed wing aircraft.  The S",null,null,974]
[-114.5270,62.4910,0,-961154.34,1622495.78,0,"075yellow","outcrop",null,null,null,null,null,null,"Slave","Au",null,null,null,"31-Jan-00",null,null,"Yellowknife City",null,null,null,975]
[-106.8583,65.0525,0,-538211.54,1800962.54,0,"076GSE0006","outcrop",null,null,null,null,"Dox 0759","076G02","Slave","Au","Reconnaissance","1098500",null,"22-Oct-97","Source: Assessment Report","500 Metres","Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District of Mackenzie.  The latitude and longitude given are taken from the sample site of the map accompanying assessment","The Beech showing is approximately 290 miles NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,976]
[-106.6156,65.2467,0,-523507.57,1819574.59,0,"076GSE0009","outcrop",null,null,null,null,"Ira","076G02","Slave","Cu-Ag-Au-Mo","Undrilled",null,null,"6-Apr-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 081682.","The IRA showing is approximately 500 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.","Within 1860 acres that surround the IRA showing the regional metamorphic grade is transitional from upper greenschist (NW) to lower amphibolite facies (SE). Assessment report 081682 notes that the cordiorite-staurolite isograd passes through this area. C",null,977]
[-106.5586,65.2000,0,-521879.43,1814141.06,0,"076GSE0010","outcrop",null,null,null,null,"Beech 1","076G02","Slave","Au-Cu","Undrilled",null,null,"6-Apr-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 082993.","The Beech 1 showing is approximately 500 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.","Archean aged sediments and volcanic rocks grade from upper greenschist to upper amphibolite facies.",null,978]
[-106.5408,65.1614,0,-521837.59,1809890.72,0,"076GSE0011","outcrop",null,null,null,null,"Beech","076G02","Slave","Au-Cu","Undrilled",null,null,"6-Apr-98","Source: Assessment Report","30 Metres","The latitude and longitude given is taken from the best sample site of the map accompanying assessment report 082993.","The Beech showing is approximately 500 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.","Metamorphic range of the area is upper greenschist to upper amphibolite",null,979]
[-106.8703,65.0811,0,-538176.22,1804102.15,0,"076GSE0012","outcrop",null,null,null,null,"Casey Lake","076G02","Slave","Zn","Reconnaissance",null,null,"7-Apr-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 081656.","The Beech showing is approximately 465 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.","Cordierite and staurolite isograd trends through the area.",null,980]
[-106.9033,65.0753,0,-539771.54,1803765.71,0,"076GSE0013","outcrop",null,null,null,null,"GM7","076G02","Slave","Zn","Reconnaissance",null,null,"7-Apr-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 081656.","The Beech showing is approximately 465 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.","strike 120-130 dip 70-75 E  Metavolcanic rocks occur as a series of fault bounded lenses",null,981]
[-107.1386,65.0886,0,-550040.25,1807193.66,0,"076GSW0010","outcrop",null,null,null,null,"Needle Lake","076G03","Slave","Au","Drilled",null,null,"3-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude of the showing is taken from the site of the highest gold value in the showing area.","The Needle Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed","At least four periods of deformation have affected the Yellowknife Supergroup. Metamorphic grade in the Back River Region ranges from sub-greenschist to upper amphibolite facies. In the Needle Lake area the general metamorphic grade is upper greenschist",null,982]
[-107.2294,65.0928,0,-554017.31,1808427.42,0,"076GSW0011","outcrop",null,null,null,null,"Moth Valley","076G03","Slave","Au","Undrilled",null,null,"5-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude of the showing is taken from the site of the highest assay value in the showing area.","The Moth Valley area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 180 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed","The Moth Valley iron formation is folded into moderate to steeply west plunging isoclinal folds and have axial planes that plunge west. The Beechey Lake Group rocks in the Moth Valley area are folded into a large west trending synform which has a range i",null,983]
[-107.1681,65.0453,0,-552250.67,1802853.66,0,"076GSW0012","outcrop",null,null,null,null,"Gollum Lake","076G03","Slave","Au","Reconnaissance",null,null,"5-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude of the showing is taken from a single sample site that comprises the showing.","The Gollum Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed","A shear zone exists parallel along the contact of a granitic pluton and sediment package.",null,984]
[-107.1681,65.0453,0,-552250.67,1802853.66,0,"076GSW0013","outcrop",null,null,null,null,"North Gollum Lake","076G03","Slave","Au","Reconnaissance",null,null,"5-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude of the showing is from the area with the highest assay values.","The North Gollum Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped",null,null,985]
[-107.2344,65.0206,0,-555733.03,1800810.02,0,"076GSW0014","outcrop",null,null,null,null,"Phaedrus Lake","076G03","Slave","Au","Reconnaissance",null,null,"5-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude of the showing is taken from the site of the highest assay value.","The Phaedrus Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixe",null,null,986]
[-107.1150,65.0986,0,-548779.18,1808051.25,0,"076GSW0015","outcrop",null,null,null,null,"North Jaeger Lake","076G03","Slave","Au","Reconnaissance",null,null,"5-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are for the site of the highest gold value in the showing area which consists of 3 rock grab samples.","North Jaeger Lake is a on the NE shore of a small lake north of Jaeger Lake. Dwg. 0605.N-10 shows the location and sample sites for the area. North Jaeger Lake is 1.5 km NE of the Needle Lake showing. The Needle Lake area is south and east of Malley Rapi",null,null,987]
[-107.2942,65.0956,0,-556858.20,1809290.37,0,"076GSW0016","outcrop",null,null,null,null,"BLS-3","076G03","Slave","Au","Reconnaissance",null,null,"6-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are from the site of the highest gold value in the showing area.","The BLS-3 Showing is centred approximately 7.3 km from the Needle Lake showing. Dwg. 0605.N-10 shows the location and sample sites for the area. The Needle Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km N",null,null,988]
[-107.3328,65.2142,0,-556114.21,1822209.86,0,"076GSW0017","outcrop",null,null,null,null,"Feather Lake","076G03","Slave","Au","Undrilled",null,null,"6-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are from the site of the highest gold value in the showing area.","The Feather Lake Showing is located along the Back River in the NW quadrant of NTS map 076G/03. This area has also been called Malley Rapids. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing","Yellowknife Supergroup rocks in the area are folded into a steeply dipping, NW striking, regional scale anticlinorium that plunges to the SE. The Beechey Lake Group rocks within this anticlinorium are in a shallow SE plunging synform that is complexly fo",null,989]
[-107.3067,65.2089,0,-555062.21,1821419.63,0,"076GSW0018","outcrop",null,null,null,null,"Bor Lake","076G03","Slave","Au","Reconnaissance",null,null,"9-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are for the highest gold value in the showing area.","The Bor Lake Showing is located along the Back River in the NW quadrant of NTS map 076G/03. This area has also been called Malley Rapids. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing air",null,null,990]
[-107.2781,65.2006,0,-553960.50,1820289.71,0,"076GSW0019","outcrop",null,null,null,null,"Bor Lake SE","076G03","Slave","Au","Reconnaissance",null,null,"9-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are from the site of the highest gold value in the showing area.","The Bor Lake SE Showing is located along the Back River in the NW quadrant of NTS map 076G/03. This area has been called Malley Rapids previously. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed",null,null,991]
[-107.2992,65.2483,0,-553909.66,1825534.29,0,"076GSW0020","outcrop",null,null,null,null,"Zone F","076G03","Slave","Au","Undrilled",null,null,"9-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are from the site of the highest gold value in the showing area.","The Zone F Showing is located at the top of the NW quadrant of NTS map 076G/03. This area has been called Malley Rapids previously. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft",null,null,992]
[-107.1161,65.2269,0,-546202.31,1821679.82,0,"076GSW0021","outcrop",null,null,null,null,"Bee","076G03","Slave","Au","Undrilled",null,null,"9-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are from the site of the highest gold value in the showing area.","The Bee area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.",null,null,993]
[-107.1603,65.2319,0,-548067.87,1822590.75,0,"076GSW0022","outcrop",null,null,null,null,"Robbs Pond","076G03","Slave","Au","Reconnaissance",null,null,"10-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given is the site of the highest gold value.","The Robbs Pond area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.",null,null,994]
[-107.0786,65.2006,0,-545068.87,1818566.16,0,"076GSW0023","outcrop",null,null,null,null,"Dox 2380","076G03","Slave","Au","Reconnaissance",null,null,"10-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given is from the site of the single gold sample that comprises this showing.","The sample area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.",null,null,995]
[-107.1011,65.2056,0,-545969.74,1819289.93,0,"076GSW0024","outcrop",null,null,null,null,"Dox 2384","076G03","Slave","Au","Reconnaissance",null,null,"10-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are for the single sample site (gold) that comprises this  showing.","The sample area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.",null,null,996]
[-107.0494,65.1869,0,-544045.88,1816861.66,0,"076GSW0025","outcrop",null,null,null,null,"Dox 2372","076G03","Slave","Au","Reconnaissance",null,null,"12-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are from the single sample site (gold) that comprises this  showing.","The sample area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.",null,null,997]
[-107.1281,65.2108,0,-547066.58,1820073.92,0,"076GSW0026","outcrop",null,null,null,null,"HG-106","076G03","Slave","Au","Reconnaissance",null,null,"18-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from the single sample site that comprises this showing.","The area of the sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,998]
[-107.2169,65.2058,0,-551126.10,1820309.83,0,"076GSW0027","outcrop",null,null,null,null,"FG-74","076G03","Slave","Au","Reconnaissance",null,null,"18-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given is from the single sample site that comprises this showing.","The area of the sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",null,null,999]
[-107.7167,65.2167,0,-573143.76,1825882.79,0,"076GSW0003","outcrop",null,null,null,null,"Hunt","076G04","Slave","Cu-Zn-Pb-Co-As","Reconnaissance","442500",null,"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 Mackenzie.  Location of showing determined from Cu Commodity File.","The Hunt Showing is approximately 460 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1000]
[-107.6106,65.0778,0,-571382.48,1810209.05,0,"076GSW0007","outcrop",null,null,null,null,"Fidler Lake","076G04","Slave","Au","Undrilled","1098600",null,"22-Oct-97","Source: Assessment Report","500 Metres","Latitude and longitude are from the best sample site within the showing area.","The Fidler Lake showing is approximately 420 km NW of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1001]
[-107.9592,65.2067,0,-584141.81,1827029.75,0,"076GSW0008","outcrop",null,null,null,null,"Ack","076G04","Slave","Au","Drilled","1098700","076G04AU 002","22-Oct-97","Source: Assessment Report","100 Metres","The latitude and longitude for this showing is from the site of the highest gold value.","The Ack showing is located approximately 2 km SSW of Uist Lake and 445 km NE of Yellowknife NT. Access to the area is by ski or float equipped fixed wing aircraft.","Tight folding at the outcrop scale with folds plunging NW and SW suggesting refolding at a regional scale. Assessment reports list this as",null,1002]
[-107.5261,65.0056,0,-569130.72,1801798.48,0,"076GSW0035","outcrop",null,null,null,null,"Alb","076G04","Slave","Au","Drilled",null,null,"20-Apr-98","Source: Assessment Report","500 Metres","The lat and long are from the approximate location of DDH 84-01. The map it was taken from is a very poorly photocopied map.","The Alb showing is located in the SE corner of NTS sheet 076/04 approximately 450 km from Yellowknife, NT. Access is by fixed wing ski or float equipped aircraft or by helicopter.",null,null,1003]
[-107.5700,65.0711,0,-569709.16,1809134.72,0,"076GSW0036","outcrop",null,null,null,null,"Barrel","076G04","Slave","Au","Undrilled",null,null,"23-Apr-98","Source: Assessment Report","100 Metres","Latitude and longitude are from the best sample site within the showing area.","The Barrel showing is approximately 420 km NW of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1004]
[-107.6778,65.1053,0,-573798.35,1813728.26,0,"076GSW0037","outcrop",null,null,null,null,"Algood","076G04","Slave","Au","Drilled",null,null,"23-Apr-98","Source: Assessment Report","30 Metres","Latitude and longitude are from the #1 showing area.","The Algood showing is approximately 440 km NE of Yellowknife, NT, and approximately 3.75 km N of Fidler Lake. Access is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1005]
[-107.6758,65.0328,0,-575260.59,1806027.97,0,"076GSW0038","outcrop",null,null,null,null,"South Fidler Lake","076G04","Slave","Au","Drilled",null,null,"30-Apr-98","Source: Assessment Report","30 Metres","The showing location is from the area of highest assay values.","The South Fidler Lake showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.","The Back River Group (on a regional scale) is highly folded and has been affected by granitoid intrusions. Regional and contact metaqmorphism is variable from greenschist facies to middle amphibolite facies.",null,1006]
[-107.6939,65.0836,0,-574982.40,1811574.33,0,"076GSW0039","outcrop",null,null,null,null,"Narrow Lake","076G04","Slave","Au","Undrilled",null,null,"5-May-98","Source: Assessment Report","100 Metres","The showing location is from highest insitu gold value from assessment report 082625.","The Narrow Lake showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,"Conjugate fault trends N10W, 2 metres wide",1007]
[-107.7211,65.0922,0,-576013.30,1812731.62,0,"076GSW0040","outcrop",null,null,null,null,"MG1","076G04","Slave","Au","Undrilled",null,null,"6-May-98","Source: Assessment Report","30 Metres","The Showing location is determined by the highest assay value from assessment report 082624","The MG1 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1008]
[-107.7583,65.1078,0,-577339.11,1814721.58,0,"076GSW0041","outcrop",null,null,null,null,"Grid 4","076G04","Slave","Au","Reconnaissance",null,null,"7-May-98","Source: Assessment Report","100 Metres","The Showing location is from the site of the highest assay value from assessment report 082625","The Grid 4 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1009]
[-107.8744,65.0878,0,-582955.89,1813662.20,0,"076GSW0042","outcrop",null,null,null,null,"Grid 5","076G04","Slave","Au","Undrilled",null,null,"8-May-98","Source: Assessment Report","30 Metres","The showing location is from the sample site with the highest assay value.","The Grid 5 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1010]
[-107.8314,65.1039,0,-580686.64,1814973.91,0,"076GSW0043","outcrop",null,null,null,null,"Grid 2","076G04","Slave","Au","Drilled",null,null,"8-May-98","Source: Assessment Report","30 Metres","The latitude and longitude given are for the highest assay value of the showing area. Three drill holes were drilled within the showing but no samples had assay values above cutoff.","The Grid 2 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1011]
[-107.7800,65.0922,0,-578644.40,1813266.23,0,"076GSW0044","outcrop",null,null,null,null,"Grid 3","076G04","Slave","Au","Undrilled",null,null,"11-May-98","Source: Assessment Report","100 Metres","The latitude and longitude given are for the highest assay value of the showing area.","The Grid 3 showing is located on the eastern shore of Regan Lake approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1012]
[-107.5861,65.1289,0,-569200.97,1815405.44,0,"076GSW0045","outcrop",null,null,null,null,"Kate Zone","076G04","Slave","Au","Reconnaissance",null,null,"12-May-98","Source: Assessment Report","30 Metres","The latitude and longitude given are for the highest assay value of the showing area.","The Kate Zone showing is located approximately 6 km south of Fidler Lake approximately 470 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1013]
[-107.6617,65.1953,0,-571155.30,1823120.43,0,"076GSW0046","outcrop",null,null,null,null,"Twin Lake East","076G04","Slave","Au","Reconnaissance",null,null,"12-May-98","Source: Assessment Report","100 Metres","The latitude and longitude given are for the highest assay value of the showing area.","The Twin lakes East showing is located in the NE corner of NTS map 076G approximately 480 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1014]
[-107.8544,65.1142,0,-581489.82,1816274.88,0,"076GSW0047","outcrop",null,null,null,null,"Fire","076G04","Slave","Au","Reconnaissance",null,null,"12-May-98","Source: Assessment Report","100 Metres","Latitude and longitude are from the single sample site from assessment report 083298.","The Fire Showing is located at the NE tip of Regan Lake in the NE corner of NTS map 076G approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1015]
[-107.8997,65.1189,0,-583408.58,1817187.41,0,"076GSW0048","outcrop",null,null,null,null,"Syn","076G04","Slave","Au","Reconnaissance",null,null,"13-May-98","Source: Assessment Report","100 Metres","Latitude and longitude are from a single sample site as given in Assessment Report 083298.","The Syn showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1016]
[-107.9433,65.1322,0,-585062.65,1818996.10,0,"076GSW0049","outcrop",null,null,null,null,"A0902","076G04","Slave","Zn-Cu","Reconnaissance",null,null,"14-May-98","Source: Assessment Report","100 Metres","Latitude and longitude are taken from the single sample site from assessment report 081610","The A0902 Showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1017]
[-107.9028,65.1558,0,-582743.19,1821123.11,0,"076GSW0050","outcrop",null,null,null,null,"A0865","076G04","Slave","Au","Reconnaissance",null,null,"14-May-98","Source: Assessment Report","100 Metres","Latitude and longitude are taken from the single sample site from assessment report 081610","The A0865 showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1018]
[-107.9625,65.1558,0,-585402.14,1821671.31,0,"076GSW0051","outcrop",null,null,null,null,"A0912 & A0913","076G04","Slave","Au-Cu","Reconnaissance",null,null,"14-May-98","Source: Assessment Report","100 Metres","This showing consists of two samples only.","The A0912 & A0913 showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",null,null,1019]
[-107.9483,65.2289,0,-583172.09,1829280.13,0,"076GSW0052","outcrop",null,null,null,null,"Uist Lake","076G04","Slave","Au","Reconnaissance",null,null,"19-May-98","Source: Assessment Report","100 Metres","This showin consists of a  single sample listed in assessment report 081610","The Uist Lake showing is located on the south shore of Uist Lake approximately 447 km NE of Yellowknife NT. Access is by float or ski equipped fixed wing aircraft or by helicopter.",null,null,1020]
[-107.9311,65.2089,0,-582844.69,1827004.90,0,"076GSW0053","outcrop",null,null,null,null,"DC Grid","076G04","Slave","Au","Undrilled",null,null,"19-May-98","Source: Assessment Report","100 Metres",null,"The DC Grid is located approximately 445 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.","The iron formation grades into amphibolitic argillites and amphibolitic chlorite schists. Felsic plutons in the Uist Lake area intrude the sediments and produce amphibolite grade metamorphism.",null,1021]
[-107.9208,65.1939,0,-582713.99,1825322.29,0,"076GSW0054","outcrop",null,null,null,null,"H Grid","076G04","Slave","Au","Undrilled",null,null,"19-May-98","Source: Assessment Report","100 Metres","Location is from the best sample result.","The H Grid is located approximately 440 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.","Felsic plutons in the Uist Lake area intrude the sediments and produce amphibolite grade metamorphism.",null,1022]
[-107.9033,65.1628,0,-582613.00,1821868.91,0,"076GSW0055","outcrop",null,null,null,null,"As Grid","076G04","Slave","Au","Undrilled",null,null,"19-May-98","Source: Assessment Report","100 Metres","Location determined by sample site highest assay values.","The As Grid is located approximately 440 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.","Felsic plutons in the Uist Lake area intrude the sediments and produce amphibolite grade metamorphism.",null,1023]
[-107.7425,65.1189,0,-576394.93,1815754.20,0,"076GSW0056","outcrop",null,null,null,null,"Soc","076G04","Slave","Au","Drilled",null,null,"20-May-98","Source: Assessment Report","100 Metres","The Soc Showing includes the FFB Showing (076GSW0057) which is located approximately 700 m to the west.","The Soc showing is located approximately 450 km NE of Yellowknife NT. Access to the area is via ski or float equipped fixed wing aircraft onto larger lakes, or aircraft with tundra tires can access some of the local eskers.",null,null,1024]
[-107.7564,65.1206,0,-576978.63,1816060.32,0,"076GSW0057","outcrop",null,null,null,null,"FFB","076G04","Slave","Au","Drilled",null,null,"21-May-98","Source: Assessment Report","100 Metres","This showing is part of the Soc showing. For further information and references see Normin ID # 076GSW0056",null,null,null,1025]
[-107.7892,65.1325,0,-578185.25,1817618.75,0,"076GSW0058","outcrop",null,null,null,null,"Main","076G04","Slave","Au","Drilled",null,null,"21-May-98","Source: Assessment Report","100 Metres","The Main Showing includes the West Main Showing (076GSW0059) which is located approximately 750 m to the west.","The Main showing is located approximately 450 km NE of Yellowknife NT. Access to the area is via ski or float equipped fixed wing aircraft onto larger lakes, or aircraft with tundra tires can access some of the local eskers.",null,null,1026]
[-107.7978,65.1389,0,-578430.51,1818374.87,0,"076GSW0059","outcrop",null,null,null,null,"West Main","076G04","Slave","Au","Drilled",null,null,"21-May-98","Source: Assessment Report","100 Metres","This showing is part of the Main showing. For further information and references see Normin ID # 076GSW0058",null,null,null,1027]
[-107.9600,65.1069,0,-586360.47,1816471.36,0,"076GSW0060","outcrop",null,null,null,null,"Fire 10","076G04","Slave","Zn-Pb-Ag","Reconnaissance",null,null,"25-May-98","Source: Assessment Report","100 Metres","The latitude and longitude are from the highest assay value sample site.","The Fire 10 showing is approximately 450 km NE of Yellowknife, NT. Access is by float or ski equipped fixed wing aircraft.",null,null,1028]
[-107.9897,65.2375,0,-584822.18,1830570.72,0,"076GSW0061","outcrop",null,null,null,null,"Uist 1","076G04","Slave","Au","Undrilled",null,null,"27-May-98","Source: Assessment Report","100 Metres","Latitude and longitude for the showing are from the site of highest gold values. The Uist 1 showing consists of two grid/showing areas called Wallys showing and Eds showing.","The Uist 1 showing is located along the south shore of Uist Lake approximately 430 km NE of Yelloweknife, NWT. The area is accessible by float or ski equipped fixed wing aircraft or by helicopter.","Beechey Lake group rocks are metamorphosed to at least greenschist facies - biotite grade.  Four phases of deformation are documented for the region but only three are evidenced on the showing property.",null,1029]
[-107.9742,65.2342,0,-584206.32,1830078.93,0,"076GSW0062","outcrop",null,null,null,null,"Eds Showing","076G04","Slave","Au","Undrilled",null,null,"29-May-98","Source: Assessment Report","100 Metres","This showing is part of the Uist 1 showing. For further information and references see Normin ID # 076GSW0061.",null,null,null,1030]
[-107.6208,65.3231,0,-566611.14,1836299.14,0,"076GSW0001","outcrop",null,null,null,null,"Musk","076G05","Slave","Zn-Pb-Cu-Ag-Au-N","Resources Calculated",null,null,"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.",null,1031]
[-107.7622,65.4947,0,-569176.73,1855746.50,0,"076GSW0033","outcrop",null,null,null,null,"Gaet","076G05","Slave","Au","Undrilled",null,null,"15-Apr-98","Source: Assessment Report","500 Metres","The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 083071. The area discussed is the central area of a grid that is 3 km long by 2 km wide and has the best assay results.","The general area of the sample site is approximately 450 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1032]
[-107.8000,65.4900,0,-570941.35,1855587.33,0,"076GSW0034","outcrop",null,null,null,null,"Gaet 4","076G05","Slave","Au","Reconnaissance",null,null,"16-Apr-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from a single sample site of map 1 accompanying assessment report 083071.","The general area of the sample site is approximately 450 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1033]
[-107.6881,65.3972,0,-568004.98,1844752.70,0,"076GSW0063","outcrop",null,null,null,null,"IM 1","076G05","Slave","Au","Undrilled",null,null,"1-Jun-98","Source: Assessment Report","100 Metres","The Triangle Lake Showing is part of the IM 1 Showing (ID 076GSW0063). The IM 1 Showing is approximately 700 m NW along strike. The latitude and longitude of the showing was determined by the highest assay value reported.  Gold mineralization occurs with","The IM 1 showing is located approximately 460 km NE of Yellowknife, NT. Access is by float or ski equipped fixed wing aircraft or by helicopter.",null,null,1034]
[-107.6817,65.3925,0,-567822.92,1844197.48,0,"076GSW0064","outcrop",null,null,null,null,"Triangle Lake","076G05","Slave","Au","Undrilled",null,null,"1-Jun-98","Source: Assessment Report","100 Metres","The Triangle Lake Showing is part of the IM 1 Showing (ID 076GSW0063). The IM 1 Showing is approximately 700 m NW along strike.",null,null,null,1035]
[-107.5458,65.3072,0,-563624.78,1833947.32,0,"076GSW0065","outcrop",null,null,null,null,"Orc","076G05","Slave","Zn-Au-Cu","Reconnaissance",null,null,"4-Jun-98","Source: Assessment Report","100 Metres","Location determined by highest assay values.","The Orc showing is approximately 475 km NE of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft.",null,null,1036]
[-107.4669,65.2881,0,-560527.97,1831224.94,0,"076GSW0028","outcrop",null,null,null,null,"KG-97A","076G06","Slave","Au","Reconnaissance",null,null,"18-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 081930.","The general area of the sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",null,null,1037]
[-107.3053,65.2608,0,-553921.14,1826913.59,0,"076GSW0029","outcrop",null,null,null,null,"KG-117 & KG-140","076G06","Slave","Au","Reconnaissance",null,null,"18-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are from the highest gold value sample site of the map accompanying assessment report 081930.","The showing site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",null,null,1038]
[-107.1622,65.3203,0,-546336.17,1831989.95,0,"076GSW0030","outcrop",null,null,null,null,"Dior","076G06","Slave","Au","Reconnaissance",null,null,"18-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude is from a single sample site that makes up this gold showing.","The sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",null,null,1039]
[-107.1344,65.3239,0,-545028.77,1832133.58,0,"076GSW0031","outcrop",null,null,null,null,"Sed","076G06","Slave","Au","Reconnaissance",null,null,"18-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude is from the site of the highest gold value.","The showing site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter","AR #82966 states that the metamorphic grade varies from greenshist to amphibole within the sedimentary package",null,1040]
[-107.0317,65.4378,0,-538155.76,1843352.03,0,"076GSW0032","outcrop",null,null,null,null,"Gersdorffite","076G06","Slave","Ni-Cu-Pd","Undrilled",null,null,"30-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 082070.","The showing site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1041]
[-106.6758,65.4525,0,-522128.88,1841947.52,0,"076GSE0007","outcrop",null,null,null,null,"Burnside","076G07","Slave","Au","Drilled",null,null,"13-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given is the site of the highest assay value in the showing area.","The Burnside showing is located approximately 500 km northeast of Yellowknife, NT. The community of Bathurst Inlet is 150 km to the north, and the Lupin mine site is 200 km to the west.  The property is accessible by ski or float equipped fixed wing airc",null,null,1042]
[-107.8467,65.4811,0,-573189.08,1855064.55,0,"076GSE0008","outcrop",null,null,null,null,"Skarn","076G07","Slave","Au","Reconnaissance",null,null,"17-Mar-98","Source: Assessment Report","30 Metres","The latitude and longitude given is the site of the highest of the highest gold value in the showing area.","The Skarn showing is located approximately 500 km northeast of Yellowknife, NT. The community of Bathurst Inlet is 150 km to the north, and the Lupin minesite is 200 km to the west.  The property is accessable by ski or float equipped fixed wing aircraft",null,null,1043]
[-106.4044,65.7519,0,-504350.60,1871600.02,0,"076GNE0006","outcrop",null,null,null,null,"Ellice River","076G09","Slave","Au","Drilled",null,null,"9-Jan-98","Source: Assessment Report","30 Metres","The Ellice River area lies within the Back River Region and consists of the Ellice and Eagle occurrences. The Eagle occurrence is within the Contact-Hawk Lakes area. The latitude and longitude given is the point with the highest assay values.","The Ellice River area and the Boot Lake area both lie within the Back River Region which is approximately 510 km northeast of Yellowknife, the Lupin Mine at Contoyto Lake is approximately 215 km to the west. The centre of the Ellice River area is approxi","The Beachey Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion Lake (approximately 5 km to the SW)to Hammer Lake (approximately 11.5 k",null,1044]
[-106.4772,65.6992,0,-508557.95,1866572.84,0,"076GNE0010","outcrop",null,null,null,null,"Boot Lake","076G09","Slave","Au","Drilled",null,null,"30-Jan-98","Source: Assessment Report","30 Metres","The Boot Lake Showing is in oxide and silicate iron formation which lies within the Back River Region. The Boot Lake area consists of numerous mineral occurances including: Chick Pond, Ayers, Aiomon, Aiomon West, Poison Pond, Boot West, Boot Lake North,","The approximate centre of the Boot Lake area is 1.8 km from the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin","The Boot Lake sediments have a metamorphic grade of upper greenschist facies except in the 250 to 300 m contact metamorphic aureole that surrounds the Boot Lake stock (situated approximately 2 km S from the centre of the Boot Lake showing). In that area",null,1045]
[-106.4283,65.6567,0,-507235.87,1861661.01,0,"076GNE0011","outcrop",null,null,null,null,"Winter","076G09","Slave","Au","Undrilled",null,null,"30-Jan-98","Source: Assessment Report","30 Metres","The Winter Showing is a gold showing hosted by oxide and silicate iron formation which lies within the Back River Region.  The latitude and longitude is the site of the highest assay value.","The approximate centre of the Winter Showing is 3.3 km from the Boot Lake Camp (situated on the north shore of Boot Lake). The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski eq","The Boot Lake Area sediments have a metamorphic grade of upper greenschist facies except in the 250 to 300 m contact metamorphic aureole that surrounds the Boot Lake stock. In that area the regional metamorphic grade is overprinted to lower amphibolite f",null,1046]
[-106.2903,65.6542,0,-501223.45,1860301.00,0,"076GNE0012","outcrop",null,null,null,null,"Rooster-Hammer","076G09","Slave","Au","Drilled",null,null,"30-Jan-98","Source: Assessment Report","30 Metres","The Rooster-Hammer Showing is a gold showing hosted by oxide and silicate iron formation which lies within the Back River region. The Rooster-Hammer Showing is composed of the Rooster, Hammer, Fox Pond, Falcon Creek and Falcon Creek North occurences. The","The approximate centre of the Rooster-Hammer Area is about 7 km from the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra whee","The Rooster-Hammer area sediments have a metamorphic grade of upper greenschist facies.",null,1047]
[-106.4456,65.7469,0,-506249.74,1871395.33,0,"076GNE0013","outcrop",null,null,null,null,"Dumbo Lake","076G09","Slave","Au","Undrilled",null,null,"9-Feb-98","Source: Assessment Report","1000 Metres","The Dumbo Lake Showing latitude and longitude location is the site of the highest gold values.","The approximate centre of the Dumbo Lake area is 5.3 km NE from the Boot Lake Camp (located on the north shore of Boot Lake). The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski","The sedimentary rocks of the Dumbo Lake area have a metamorphic grade ranging from greenschist to upper greenschist adjacent to a granitic sill.",null,1048]
[-106.3475,65.6658,0,-503513.28,1861987.29,0,"076GNE0014","outcrop",null,null,null,null,"Shell Lake","076G09","Slave","Au","Undrilled",null,null,"20-Feb-98","Source: Assessment Report","30 Metres","The Shell Lake Showing latitude and longitude location is the site of the highest gold values.","The approximate centre of the Shell Lake area is 7 km SE of the Boot Lake Camp (located on the north shore of Boot Lake). The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equ",null,null,1049]
[-106.4278,65.5439,0,-509393.51,1849656.45,0,"076GNE0017","outcrop",null,null,null,null,"Goose Lake","076G09","Slave","Au","Resources Calculated",null,null,"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 uti","The iron formation has been complexly folded and has a metamorphic grade is middle greenschist to lower amphibolite.",null,1050]
[-106.4564,65.5456,0,-510621.62,1850066.62,0,"076GNE0018","outcrop",null,null,null,null,"Goose Neck","076G09","Slave","Au","Reconnaissance",null,null,"25-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude given is the site of the highest gold value for the showing area.","Goose Neck 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 uti","An airborne geophysical survey shows complex folding and faulting exists in the Goose Neck area.",null,1051]
[-106.5269,65.7394,0,-509952.58,1871246.94,0,"076GNE0007","outcrop",null,null,null,null,"Trout Lake","076G10","Slave","Au","Undrilled",null,null,"28-Jan-98","Source: Assessment Report","30 Metres","The Trout Lake Showing lies within the Back River Region. The latitude and longitude given is the site of the highest assay value.","Trout lake is located approximately 6.5 km northwest of the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otte","At least four periods of deformation have affected the rocks of the Yellowknife Supergroup (Chandler et al, 1992). The Beachey Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed i",null,1052]
[-106.5192,65.7181,0,-510030.52,1868919.59,0,"076GNE0008","outcrop",null,null,null,null,"Scorpion Lake North","076G10","Slave","Au","Drilled",null,null,"29-Jan-98","Source: Assessment Report","30 Metres","The Scorpion Lake North Showing is in oxide and silicate iron formation on the southwest shore of Scorpion Lake which lies within the Back River Region and is an extension of the Boot Lake Showing. The latitude and longitude are from the area of the high","Scorpion Lake North is located approximately 5 km northwest of the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Tw","The Beechy Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion to Hammer Lake. The Boot Lake granitic stock (located south of Boot Lake",null,1053]
[-106.5053,65.7078,0,-509622.18,1867712.57,0,"076GNE0009","outcrop",null,null,null,null,"Scorpion Lake","076G10","Slave","Au","Drilled",null,null,"29-Jan-98","Source: Assessment Report","30 Metres","The Scorpion Lake showing is in oxide and silicate iron formation on the southwest shore of Scorpion Lake which lies within the Back River Region and is an extension of the Boot Lake Showing. The latitude and longitude given is the site of the highest go","Scorpion Lake is located approximately 3.5 km northwest of the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin O","The Beachy Lake Group sedimentary rocks, including the oxide iron formations, within the Ellis-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion to Hammer Lake. The Boot Lake granitic stock (located south of Boot Lake)",null,1054]
[-106.9086,65.6642,0,-528158.10,1866367.63,0,"076GNE0015","outcrop",null,null,null,null,"Boulder Pond","076G10","Slave","Au","Drilled",null,null,"23-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are the site of the highest gold values of the Boulder Lake area which includes the following gold occurences: East Boulder Pond, West Boulder Pond, Peace Lake, Opener Lake, Porkchop, Jaeger, Player, 4DHZ004 and Humpback.","The approximate centre of the Boulder Pond area is about 37.6 km SE of the George Lake Camp. The property is approximately 500 km northeast of Yellowknife, NT. and 150 km south of the community of Bathurst Inlet. The property is accessable by float or sk","Abundant chlorite indicates that this area has undergone upper greenschist facies metamorphism.  Coarse grained euhedral magnetite porphyroblasts replace chlorite within zones of intense alteration of the oxide iron formation. Howe(1993)suggests this may",null,1055]
[-106.8775,65.6253,0,-527575.78,1861976.54,0,"076GNE0016","outcrop",null,null,null,null,"Soi Lake","076G10","Slave","Au","Undrilled",null,null,"24-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are taken from the site of the highest gold value in the Soi Lake area.","The approximate centre of the Soi Lake area is about 41 km SE of the George Lake Camp. The property is approximately 500 km northeast of Yellowknife, NT. and 150 km south of the community of Bathurst Inlet. The property is accessable by float or ski plan","South of Soi Lake the Vega oxide iron formation is 70-80 m wide and extends 200 m south where it terminates adjacent to a 60 m wide NW trending gabbroic dyke. This termination may be due to a fold closure, this is indicated by repetative outcrop scale is",null,1056]
[-106.5058,65.5492,0,-512729.38,1850846.94,0,"076GNE0019","outcrop",null,null,null,null,"Goose Creek","076G10","Slave","Au","Undrilled",null,null,"25-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude given is the site of the highest gold value for the showing area.","Goose Creek 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 ut","Ground and airborne magnetic surveys indicate that the sedimentary sequence of the Goose Creek area is folded into a large S configuration.",null,1057]
[-106.5500,65.5711,0,-514249.77,1853532.94,0,"076GNE0020","outcrop",null,null,null,null,"Llama Lake","076G10","Slave","Au","Undrilled",null,null,"25-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude given is the site of the highest gold value in the showing area.","Llama 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 uti","West of Llama Lake approximately 1.5 km a granitic pluton intrudes the sediments. Cordiorite within a biotite schist about 800 m west of Llama Lake indicates that the sediments have been metamorphosed to lower amphibolite grade near the pluton.  Ground m",null,1058]
[-107.4061,65.5722,0,-551875.94,1860824.60,0,"076GNW0014","outcrop",null,null,null,null,"Knight","076G11","Slave","Au","Reconnaissance",null,null,"7-Apr-98","Source: Assessment Report","100 Metres","The location is the sample site of sample 421-1 from assessment report 082070 map 6/7","The Knight occurrence is approximately 500 km NE of Yellowknife, NT. Access is by ski or float equipped fixed wing airplane or by helicopter.",null,null,1059]
[-107.9383,65.6044,0,-574526.53,1868949.87,0,"076GNW0002","outcrop",null,null,null,null,"Yava","076G12","Slave","Zn-Cu-Ag-Pb-Au","Drilled","159300","076G12ZN 001","22-Oct-97","Source: Assessment Report","100 Metres","The Yava Showing has been cited in numerous references as having drill-indicated reserves of 1,000,000 to 2,000,000 tonnes grading 3% Zn, 0.5% Cu, 0.5% Pb, 102.8 g/t (or 10%) Ag and 2 g/t Au. It is difficult to determine what these figures are based on,","The Yava 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.",null,null,1060]
[-107.8075,65.5103,0,-570832.38,1857805.22,0,"076GNW0018","outcrop",null,null,null,null,"Gaet 3","076G12","Slave","Au","Reconnaissance",null,null,"3-Jun-98","Source: Assessment Report","30 Metres","The latitude and longitude are the coordinates of the single sample that make up this showing.","Gaet 3 is located approximately 460 km NE of Yellowknife, NT. The showing area is accessable  by ski or float equipped fixed wing aircraft.",null,null,1061]
[-107.8186,65.5294,0,-570907.01,1859928.24,0,"076GNW0019","outcrop",null,null,null,null,"Trumpet","076G12","Slave","Au","Undrilled",null,null,"4-Jun-98","Source: Assessment Report","100 Metres","The Trumpet showing has three","076GNW0021 (the Flute Showing is approximately 500 m SSE of the Trumpet) & 076GNW0022 (the Picallo Showing is approximately 800 m SSE of the Trumpet).  Latitude and longitude locations is of the best assay value.\"","The Trumpet showing is located approximately 460 km NE of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft.","Metamorphosed to greenschist-biotite grade",1062]
[-107.8114,65.5219,0,-570752.93,1859069.10,0,"076GNW0020","outcrop",null,null,null,null,"Oboe","076G12","Slave","Au","Undrilled",null,null,"4-Jun-98","Source: Assessment Report","30 Metres",null,null,null,null,1063]
[-107.8142,65.5364,0,-570562.25,1860630.32,0,"076GNW0021","outcrop",null,null,null,null,"Piccalo","076G12","Slave","Au","Undrilled",null,null,"8-Jun-98","Source: Assessment Report","100 Metres",null,null,null,null,1064]
[-107.8164,65.5328,0,-570736.78,1860268.69,0,"076GNW0022","outcrop",null,null,null,null,"Flute","076G12","Slave","Au","Undrilled",null,null,"8-Jun-98","Source: Assessment Report","30 Metres",null,null,null,null,1065]
[-107.9408,65.6375,0,-573912.85,1872477.73,0,"076GNW0023","outcrop",null,null,null,null,"Buck","076G12","Slave","Au","Drilled",null,null,"8-Jun-98","Source: Assessment Report","30 Metres","Latitude and longitude mark the highest concentration of drilling and the best gold values. This showing has two","The Buck showing is located approximately 480 km NE of Yellowknife, NT and is accessable by float or ski equipped fixed wing aircraft.","Greenschist-biotite facies",null,1066]
[-107.9439,65.6456,0,-573871.42,1873363.49,0,"076GNW0024","outcrop",null,null,null,null,"Buck North","076G12","Slave","Au","Undrilled",null,null,"11-Jun-98","Source: Assessment Report","100 Metres",null,null,null,null,1067]
[-107.9508,65.6542,0,-573985.05,1874336.48,0,"076GNW0025","outcrop",null,null,null,null,"Chopin","076G12","Slave","Au","Drilled",null,null,"11-Jun-98","Source: Assessment Report","100 Metres",null,null,null,null,1068]
[-107.9344,65.6833,0,-572632.77,1877270.40,0,"076GNW0026","outcrop",null,null,null,null,"Lin","076G12","Slave","Au","Undrilled",null,null,"12-Jun-98","Source: Assessment Report","100 Metres","Latitude and longitude are from the location of the highest assay value.","The Lin showing is located approximately 460 km NE of Yellowknife, NT and is accessable by float or ski equipped fixed wing aircraft.","Regionally, metamorphic facies fall within this range.",null,1069]
[-107.9308,65.6900,0,-572329.32,1877947.58,0,"076GNW0027","outcrop",null,null,null,null,"Mozart","076G12","Slave","Au","Reconnaissance",null,null,"12-Jun-98","Source: Assessment Report","100 Metres","The latitude and longitude for the showing is based on the highest gold values.","The Mozart showing is located approximately 460 km NE of Yellowknife, NT. The showing is accessable by ski or float equipped fixed wing aircraft.",null,null,1070]
[-107.9881,65.6836,0,-574970.54,1877786.61,0,"076GNW0028","outcrop",null,null,null,null,"Bach","076G12","Slave","Au","Undrilled",null,null,"12-Jun-98","Source: Assessment Report","100 Metres","Latitude and longitude are from the area of highest gold values from a silicate and/or oxide iron formation within greywacke turbidites.","The Bach Showing is approximately 460 km NE of Yellowknife, NT. The showing area is accessable by float or ski equipped fixed wing aircraft.","Sediments are metamorphosed to at least greenschist facies - biotite grade",null,1071]
[-107.9392,65.7144,0,-572162.93,1880607.26,0,"076GNW0029","outcrop",null,null,null,null,"Lin 1","076G12","Slave","Au","Reconnaissance",null,null,"15-Jun-98","Source: Assessment Report","100 Metres","This showing is from a single reconnaissance sample that is located on map 3a of AR 082994. It is noted that this sample was located from previous reconnaissance work.","The Lin 1 showing is approximately 470 km NE of Yellowknife, NT and is accessable by either float or ski equipped fixed wing aircraft.",null,null,1072]
[-107.9353,65.7094,0,-572102.06,1880042.65,0,"076GNW0030","outcrop",null,null,null,null,"Lin 2","076G12","Slave","Au","Reconnaissance",null,null,"15-Jun-98","Source: Assessment Report","100 Metres","This showing is from a single reconnaissance sample.","The Lin 2 showing is approximately 460 km NE of Yellowknife, NT and is accessable by either float or ski equipped fixed wing aircraft.",null,null,1073]
[-107.8836,65.5925,0,-572389.81,1867196.40,0,"076GNW0031","outcrop",null,null,null,null,"WL1","076G12","Slave","Au","Undrilled",null,null,"15-Jun-98","Source: Assessment Report","100 Metres","Latitude and longitude are determined by the site of the best gold value.","The WL1 showing is approximately 465 km NE of Yellowknife, Nt and is accessable by either ski or float equipped fixed wing aircraft.",null,null,1074]
[-107.9025,65.6008,0,-573037.15,1868245.67,0,"076GNW0032","outcrop",null,null,null,null,"Nuts","076G12","Slave","Au","Reconnaissance",null,null,"15-Jun-98","Source: Assessment Report","100 Metres","This showing consists of 2 reconnaissance samples.","The Nuts showing is located approximately 460 km NE of Yellowknife, NT. Access is by fixed wing aircraft equipped with either skis or floats.",null,null,1075]
[-107.8997,65.6978,0,-570801.87,1878494.23,0,"076GNW0033","outcrop",null,null,null,null,"51536","076G12","Slave","Au","Reconnaissance",null,null,"15-Jun-98","Source: Assessment Report","100 Metres","This showing consists of a single reconnaissance sample",null,null,null,1076]
[-107.8950,65.6894,0,-570779.64,1877562.33,0,"076GNW0034","outcrop",null,null,null,null,"51535","076G12","Slave","Au","Reconnaissance",null,null,"16-Jun-98","Source: Assessment Report","100 Metres","This showing is a single reconnaissance sample that had a gold value of 0.51 g/tonne.",null,null,null,1077]
[-107.7622,65.4947,0,-569176.73,1855746.50,0,"076GSW0033","outcrop",null,null,null,null,"Gaet","076G12","Slave","Au","Undrilled",null,null,"15-Apr-98","Source: Assessment Report","500 Metres","The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 083071. The area discussed is the central area of a grid that is 3 km long by 2 km wide and has the best assay results.","The general area of the sample site is approximately 450 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.",null,null,1078]
[-107.4764,65.9258,0,-547510.76,1898940.58,0,"076GNW0003","outcrop",null,null,null,null,"George Lake","076G13","Slave","Au","Resources Calculated",null,null,"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","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 of","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",1079]
[-107.4900,65.8808,0,-549049.40,1894284.57,0,"076GNW0017","outcrop",null,null,null,null,"Dex","076G13","Slave","Au","Undrilled",null,null,"15-Apr-98","Source: Assessment Report","30 Metres","The showing location is centred on the area of best assay data from assessment report 083071.","The Dex showing is approximately 450 km NE of Yellowknife NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.","Greywackes of the showing area are relatively unmetamorphosed.",null,1080]
[-107.4764,65.9258,0,-547510.76,1898940.58,0,"076GNW0003","outcrop",null,null,null,null,"George Lake","076G14","Slave","Au","Resources Calculated",null,null,"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","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 of","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",1081]
[-107.2864,65.8764,0,-540303.20,1892074.24,0,"076GNW0004","outcrop",null,null,null,null,"Rifle Lake","076G14","Slave","Au","Drilled",null,null,"12-Feb-98","Source: Assessment Report","500 Metres","The Latitude and longitude given is the site of the highest gold value.","Rifle Lake is in the SW section of the George Lake area, approximately 9.2 km from the George Lake Camp (SW shore of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by floa","The NW section of the Rifle Lake area is highly folded forming a SE plunging syncline. Fold closures have an average plunge of 65 degrees SE.",null,1082]
[-107.3625,65.8708,0,-543724.61,1892128.43,0,"076GNW0005","outcrop",null,null,null,null,"Komatik Lake","076G14","Slave","Au","Undrilled",null,null,"16-Feb-98","Source: Assessment Report","500 Metres","The Latitude and longitude given is the site of the highest gold value.of the Komatik Lake occurrence on the SSW end of Komatik Lake.","The Komatik Lake area is 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",null,null,1083]
[-107.3447,65.8678,0,-543014.17,1891658.03,0,"076GNW0006","outcrop",null,null,null,null,"Mouse","076G14","Slave","Au","Undrilled",null,null,"16-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are measured from the site of the highest assay of the Mouse showing along strike of the George Lake belt.","The Mouse showing is within the George Lake belt and is approximately 7.8 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area i",null,null,1084]
[-107.3094,65.8667,0,-541503.74,1891240.36,0,"076GNW0007","outcrop",null,null,null,null,"Bullwinkle Lake","076G14","Slave","Au","Undrilled",null,null,"16-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are measured from the site of the highest assay value of the Bullwinkle showing along strike of the Fold Nose belt of the George Lake area.","The Bullwinkle showing is within the Fold Nose belt of the George Lake area and is approximately 9 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake a",null,null,1085]
[-107.3678,65.8786,0,-543791.78,1893001.39,0,"076GNW0008","outcrop",null,null,null,null,"Takrark Lake","076G14","Slave","Au","Undrilled",null,null,"17-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are measured from the site of the highest gold value of the Takrark Lake Showing along strike of the Fold Nose belt of the George Lake area.","The Takrark Lake showing is within the Fold Nose belt of the George Lake area and is approximately 5.4 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George La",null,null,1086]
[-107.2664,65.8614,0,-539745.53,1890312.37,0,"076GNW0009","outcrop",null,null,null,null,"4LBZ005","076G14","Slave","Au","Reconnaissance",null,null,"17-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are measured from the site of the 4LBZ005 sample along strike of the Lookout Hill belt of the George Lake area.","The 4LBZ005 showing is within the Lookout Hill belt of the George Lake area and is approximately 10.8 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lak",null,null,1087]
[-107.2700,65.8522,0,-540092.71,1889366.44,0,"076GNW0010","outcrop",null,null,null,null,"West Rapids","076G14","Slave","Au","Reconnaissance",null,null,"18-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are measured from the site of the highest assay value of the West Rapids showing along strike of the Fold Nose belt of the George Lake area.","The West Rapids showing runs along strike of the Fold Nose belt of the George Lake area and is approximately 11.3 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of th",null,null,1088]
[-107.2489,65.8383,0,-539463.15,1887712.01,0,"076GNW0011","outcrop",null,null,null,null,"Oar Lake","076G14","Slave","Au","Drilled",null,null,"18-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are measured from the site of the highest gold value of the Oar Lake showing along strike of the Lookout Hill belt of the George Lake area.","The Oar Lake showing runs along strike of the Lookout Hill belt of the George Lake area and is approximately 12.4 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of th","The iron formation is structurally complex with minor folds, faults and crosscutting quartz veins.",null,1089]
[-107.3861,65.9131,0,-543864.23,1896818.53,0,"076GNW0012","outcrop",null,null,null,null,"Shadow Pond","076G14","Slave","Au","Undrilled",null,null,"18-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are the site of the highest gold value of the Shadow Pond Showing which lies along strike of the Lookout Hill belt of the George Lake area.","The Shadow Pond showing runs along strike of the Lookout Hill belt of the George Lake area and is approximately 3.4 km NE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of","Steeply dipping SW trending faults cut through the area with displacements up to 200 m.",null,1090]
[-107.4203,65.9303,0,-544985.89,1898936.17,0,"076GNW0013","outcrop",null,null,null,null,"Lookout Hill","076G14","Slave","Au","Drilled",null,null,"18-Feb-98","Source: Assessment Report","30 Metres","The latitude and longitude are measured from the site of the highest gold value of the Lookout Hill showing which lies along strike of the Lookout Hill belt of the George Lake area.","The Lookout Hill showing runs along strike of the Lookout Hill belt of the George Lake area and is approximately 2 km ENE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of","Steeply dipping SW trending faults cut through the Lookout Hill area.",null,1091]
[-107.3942,65.9356,0,-543744.22,1899275.13,0,"076GNW0015","outcrop",null,null,null,null,"U-1","076G14","Bear","U-Au-Pb","Undrilled",null,null,"8-Apr-98","Source: Assessment Report","1000 Metres","The U-1 showing location is from a sample location marked on map 5 from assessment report 081178. The sample sites are clearly marked but there are no corresponding sample numbers. The assessment report does state that the samples are from this area.","The U-1 showing is located approximately 500 km NE of Yellowknife, NT. The area is accessable by float or ski equipped fixed wing aircraft.","The Goulburn Group has been folded - intensity varies with competancy. The Western River Formation is tightly folded, less competant and the Burnside Formation drapes over it. Folds have NS axial planes which are vertical or dip steeply east.",null,1092]
[-107.1078,65.8267,0,-533561.90,1885290.31,0,"076GNW0016","outcrop",null,null,null,null,"U-2","076G14","Slave","U","Reconnaissance",null,null,"9-Apr-98","Source: Assessment Report","100 Metres","The U-2 showing location is from sample locations marked on map 5 from assessment report 081178. The sample sites are clearly marked but thee are no corresponding sample numbers just listed assay values that are not discussed in the body of the report.","The U-2 showing is located approximately 500 km NE of Yellowknife, NT. The area is accessable by float or ski equipped fixed wing aircraft.","Folding and faulting noted.",null,1093]
[-107.4900,65.8808,0,-549049.40,1894284.57,0,"076GNW0017","outcrop",null,null,null,null,"Dex","076G14","Slave","Au","Undrilled",null,null,"15-Apr-98","Source: Assessment Report","30 Metres","The showing location is centred on the area of best assay data from assessment report 083071.","The Dex showing is approximately 450 km NE of Yellowknife NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.","Greywackes of the showing area are relatively unmetamorphosed.",null,1094]
[-106.4528,65.8100,0,-505342.74,1878165.95,0,"076GNE0004","outcrop",null,null,null,null,"Western River 1","076G16","Slave","Cu","Observed Ore Mineral","526000",null,"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",null,null,null,1095]
[-106.4208,65.7819,0,-504488.69,1874922.17,0,"076GNE0005","outcrop",null,null,null,null,"Western River 2","076G16","Slave","Cu","Observed Ore Mineral","1061300",null,"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",null,null,null,1096]
[-106.4044,65.7519,0,-504350.60,1871600.02,0,"076GNE0006","outcrop",null,null,null,null,"Ellice River","076G16","Slave","Au","Drilled",null,null,"9-Jan-98","Source: Assessment Report","30 Metres","The Ellice River area lies within the Back River Region and consists of the Ellice and Eagle occurrences. The Eagle occurrence is within the Contact-Hawk Lakes area. The latitude and longitude given is the point with the highest assay values.","The Ellice River area and the Boot Lake area both lie within the Back River Region which is approximately 510 km northeast of Yellowknife, the Lupin Mine at Contoyto Lake is approximately 215 km to the west. The centre of the Ellice River area is approxi","The Beachey Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion Lake (approximately 5 km to the SW)to Hammer Lake (approximately 11.5 k",null,1097]