036CSE0006
outcrop
Ray
036C08
Churchill
U
Resources Calculated
29-Sep-98
Source: Government Report
1000 Metres
037CNE0010
Eqe Bay
037C09
Fe
52399
22-Oct-97
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.
048CSE0002
Nanisivik
048C01
Pb-Zn-Cd-Cu
Producer
822500
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
055ENW0007
Turquetil Lake Northwest
5.50E+1
Au
1088600
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.
055JNW0001
Meliadine West
055J13
26-Oct-98
Source: Media/News Release
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
055KSW0041
Fat Lake
055K04
1088900
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
055KNE0083
North Rankin Nickel Mine
055K16
Ni-Cu-Pt-Pd-Carv
Past Producer
532500
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
055KNE0144
F-Zone
27-Oct-98
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
055LSE0056
Cache Zone
055L07
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
055MNW0002
Apr-68
055M12
931800
Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  Baker Lake Area, Keewatin District.
055NSE0001
Tiriruniak Zone
055N01
28-Oct-98
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
056DSE0007
Feb-68
056D02
U-Mo
932300
065GSE0009
Cullaton Lake South
065G07
1051700
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
065GSE0016
Cullaton Mine
065G08
1052400
The Cullaton Mine (B-Zone) lies 8 km SSW of Cullaton Lake and is 320 km SW of Baker Lake.
065HNE0001
Heninga Lake
065H16
Zn-Cu-Ag-Au
159400
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.
065INE0001
Ferguson Lake
065I15
Cu-Ni-Pt-Pd
1088202
Located 225 km southwest of Baker Lake, NWT.  Property is accessable by float or ski-equipped fixed wing aircraft or helicopter.
065JNE0005
Lac Cinquante
065J10
1-Oct-98
066ASW0002
Lone Gull
066A05
959900
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.
066GSE0001
Lost Lake
066G08
5-Oct-98
066HSE0015
Third Portage Lake
066H01
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
066HSE0016
Third Portage North Exten
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
066HSE0017
Goose Island
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
068HSE0003
Polaris
068H08
Innuitian
Zn-Pb-Ag-Cd
834200
To Be Determined
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.
068HNE0002
Eclipse
068H09
Zn-Pb-Cd-Ag
36100
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
075ASE0001
Nickel King
075A07
Ni-Cu-Co-Ag
1038800
By float or ski-equipped fixed wing aircraft from Stony Rapids, Sask., 135 km to the southeast, or Points North, Sask.
075ESW0001
OConnor Lake
7.50E+0
Zn-Pb-Cu
819199
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.
075ESW0012
Pb-Zn
819102
Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District of Mackenzie.
075ESE0002
Dussault
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
075FSW0001
Salkeld Lake
075F05
Cu-Ag-Zn-Pb-Au
656600
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.
075LSW0001
Sachowia Lake
075L05
Slave
Ni-Co-Bi-Ag
957400
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.
075LNW0002
BBX
075L12
Cu-Ag-Ni-Co-Bi-P
524200
147 km by float-plane or helicopter east from Yellowknife. One map shows an airstrip for the Great Slave Lodge.
075MSE0001
Susu Lake
075M02
Cu
657000
075M02CU 002
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.
075MSE0002
BB
Zn-Pb-Ag-Cu
36203
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.
075MSE0039
Kennedy Lake West
Cu-Ag-Zn
75M02CU0
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.
076DSW0001
Deb
076D03
Cu-Zn-Ag-Pb
1096300
075M14CU 003
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
076DSW0002
Perrson
076D03AU_06
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
076DSW0003
Tundra
1058701
076D03AU007
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
076DSW0006
RED 24
660500
076D03AU001
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
076DSW0008
Salmita New Discovery Vein
Au-Ag
1058500
076D03AU003
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.
076DSW0009
Salmita South Vein
1058600
076DSW0010
Salmita North Zone
1058800
076DSW0019
Tundra Mine
20-May-98
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
076DSW0020
Saucer Zone
7-Jun-98
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
076DSW0004
Jax Lake
076D06
1096100
The Jax showing lies north of Courageous Lake approximately 250 km NE of Yellowknife.
076DNE0024
Ekati - Misery
076D09
Diam
16-Oct-98
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.
076DNE0020
Ekati - Fox Pipe
076D10
076DNE0021
Ekati - Koala
076DNE0023
Ekati - Panda
076DNW0001
Koala Lake Pipes
6-Jan-98
There is a 1950 m airstrip nearby as well as the Lupin winter road.
076DNE0022
Ekati - Sable Pipe
076D15
076ENE0001
Butterfly
7.60E+1
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
076ENE0002
Jon
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.
076ENW0004
Pan
1059900
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.
076ENW0005
Gondor
Zn-Au-Ag-Cu-Pb
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
076ENW0017
Lupin Mine
1060800
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.
076FNE0001
Hackett River
076F16
Zn-Pb-Cu-Ag-Au
1088302
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.
076GSW0001
Musk
076G05
Zn-Pb-Cu-Ag-Au-N
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.
076GNE0017
Goose Lake
076G09
24-Feb-98
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.
076GNW0003
George Lake
076G14
7-Jan-98
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
076LSW0008
Gumbo Lake Ilmenite
076L06
Ti-V-Fe
1099100
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).
076LNE0023
Ulu
076L15
Au-As-Bi-Zn-Ag-C
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
076MSE0053
High Lake AB Zone
076M07
Cu-Zn-Ag
653401
076M07CU 001
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
076MSE0054
High Lake D Zone
Zn-Cu-Ag-Pb-Au
653402
Update & entry 05/17/93.
076MNW0084
North Central Vein
076M11
1063400
076M11AU 007
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
076MNW0085
Fred Vein
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.
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
076NSE0006
Pistol Lake
076N02
Au-Ag-Cu
308700
076N02AU 001
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
076NSE0010
Turner Lake Main Gold
1058900
076N02AU 002
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
076ONE0010
Boston
076O09
15-Oct-98
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
085BNE0001
Great Slave Reef
085B10
Arctic, In
Pb-Zn-Ind1
1132203
5000 Metres
085BNW0006
085B11
Pb-Zn-Cu
1132100
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
085BNE0004
Pine Point Mine
085B16
808400
085ISE0001
Best Bet
085I01
Li-Be-Nb-Sn-Ta
1133100
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
085ISE0002
Moose #2 Dyke
Li-Nb-Be-Ta-Sn
942100
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
085ISE0003
Lens
085I02
Li-Nb-Ta-Be
1133800
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.
085ISE0004
Mut
Li
1133600
90km
085ISE0005
Bin
1133700
085ISE0006
Thor Lake
Be-Ta-Th-Y-Ga-Ce
1133400
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.
085ISW0007
Big Hill East
085I05
1134400
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.
085ISW0009
Jake
085I06
Li-Sn-Ta-Nb
1134900
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.
085ISW0010
Paint
Li-Ta-Nb
1134800
085ISW0011
Ann
1134700
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.
085ISE0012
Hid
085I07
1136300
085ISE0013
Mac
1136100
The Mac showing is approximately 6 km W of Buckham Lake and is accessible by float or ski equipped fixed wing aircraft.
085ISE0017
Norma
1135400
085I07AU 005
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.
085ISE0018
Joon
1135200
085I07AU 003
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.
085ISE0019
Bullmoose
Ag-Au
1135000
085I07AU 001
The deposit is 80 km east of Yellowknife, NWT, and may be reached from that point by air.
085ISE0020
Ruth Mine
Au-Ag-As-W
1135500
085I07AU 006
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.
085ISE0021
Thor
085I08
1080800
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.
085INE0023
XL
085I10
Pb-Zn-Cu-Ag
442000
The prospect is approximately 91 km from Yellowknife, NWT, from which point it is accessable by float/ski-equipped aircraft.
Sulphide deposition
085INE0149
Turnback Lake
Be-Ind3
1143700
Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:   District Of Mackenzie
085INW0028
KI
085I11
1160300
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
085INW0029
Shorty
Li-Be-Sn
1136200
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
085INW0033
FI Main Dyke
Li-Be
1160000
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).
085INW0034
Freda
Ta-Nb-Sn-Ti-Li-B
1160600
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?
085INW0037
Thompson-Lundmark
Past Producer w/ Rese
1144000
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?
085INW0042
Jim Lit
1160100
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.
085INW0048
Pensive Yellowknife Mine
1144600
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
085INW0049
Peg Tantalum
Be-Ta-Nb-Sn
1144100
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
085INW0077
Million Dollar
085I12
1161100
Float/ski plane to Parr Lake, 53 km NE of Yellowknife.
085INW0078
Old Parr South
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.
085INW0079
FI Southwest Dyke
1162000
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.
085INW0084
Vo #2
085I13
Li-Be-P2O5
1162300
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.
085INW0085
Vo #5
085INW0158
Blaisdell Lake
Be-Li-Nb-Ta
1162200
085INW0104
Mahe
085I14
1081200
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
085INW0105
MYRT
Au-Pb-Zn-Cu
1081300
The showing lies approximately 72 km NE of Yellowknife, NWT.
085INW0132
Gordon Lake
Au-Ag-Cu-Pb-Zn
1141900
Located at the SE shore of Gordon Lake
085INW0133
Camlaren Mine
1142000
085INW0142
Mitchell Lake
Au-Ag-Pb
1142900
085INW0155
Dome Lake (Southwest Side
1161800
085INE0086
Sunrise
085I16
Zn-Pb-Ag-Cu-Au
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
085INE0087
Bear
Zn-Pb-Ag-Au-Cu
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
085JSE0012
Giant Mine
085J08
Au-Ag-As
1163300
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
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
085JSE0013
Burwash Mine
1163100
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).
085JSE0050
Rod
1163000
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
085JSE0056
Con-Rycon
Au-Ag-Sb-Pb-Cu-Z
1163200
085JNE0002
Cassidy Point
085J09
Au-Zn-Pb
1165400
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
085JNE0009
Tom Mine
Au-Cu-Pb-Zn
1165500
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
085JNE0010
Ptarmigan Mine
1164200
The minesite, approximately 12 km NE of Yellowknife, is accessible by road. There is power to the site.
085JNE0011
Vega
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.
085JNE0014
Crestaurum
Au-Ag-Sb-Pb
1164300
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
085JNE0015
Supercrest
1163400
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
085JNE0044
Lynx
1165100
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.
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).
085JNE0051
Big Hill West
1164000
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.
085NSE0043
Camp Lake
085N08
Au-Zn-Pb-Cu
1168500
The Camp Lake Showing is located on the E side of Snare River, 131 km NW of Yellowknife, NT.
085NSE0044
Slemon Lake
1168600
The Slemon showing is located approximately 125 km NW of Yellowknife, NT and 4 km NE of Slemon Lake.
085NNE0001
Cab
085N10
Bi-Co-Cu-Au-As-W
1088400
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
Mineralization thought to be related to felsic magmatic and volcanic activity in Great Bear Magmatic Zone.
085NNE0045
Lou Lake (Southeast of)
Bi-Co-Au-Cu-W
1168700
085NNE0035
SUE
085N15
Cu-Ag-U-Au-Fe
980200
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
085OSE0007
Viking Yellowknife
085O01
1168900
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.
085OSW0001
Bugow
085O04
1169500
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.
085OSW0013
Mosher Lake
1169600
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.
085OSW0042
Cabin Lake
30-Jun-98
085PSW0001
Nicholas Lake
085P04
Au-Zn-Pb-As
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
085PSW0032
Discovery Mine
Au-Pb-Cu
1171300
085PSW0035
Winter Lake
1171600
Source: CANMINDEX
The Winter Lake showing is approximately 85 km NNE of Yellowknife, NT.
085PSW0037
Cross Lake
1171800
The Gab showing is approximately 19 km SE of Discovery Mine.
085PSW0040
085P06
1172100
This showing is located NE of Gordon Lake approximately 77 km NNE of Yellowknife.
086BSW0012
Anna (Barker Vein)
086B03
1066300
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.
086BSW0050
Horseshoe Zone
20-Jul-98
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).
086BSW0027
Norris Lake (North End)
086B05
1154000
This showing is located 224 km NNE of Yellowknife.
086BSW0002
Kim
086B06
1154600
086BSW0003
Cass
Au-As
Mineralized quartz-carbonate veins and sulphides are deformed by the last deformation and thus predate it.
086BSW0004
Colomac
1155000
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.
086BSW0019
Leta (No. 1 Zone)
1069800
086BSW0028
Treasure Island
1154100
This showing is 22 km N of Indin Lake.
086BSW0029
Indin Lake (Leta Arm) -1
1154200
086BSW0035
North Inca (Indian Lake N
1154901
086DNE0002
CORMAC
086D09
926300
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
086DNE0004
PITCH 8
086D16
926500
086D16U  003
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).
086ENE0012
Terra Mine
8.60E+1
Ag-Cu-Bi-Co-Ni-U
660300
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.
086FNW0010
Norex Mine
086F12
Ag-Bi-Cu-Ni-Co-A
517900
086FNW0021
Contact Lake
086F13
Ag-U-Ra-Cu-Ni-Co
929300
Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:   Camsell River Area
086GSW0002
Oldest Rocks
086G04
ExSt
1-Sep-98
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
086HSE0032
REN
086H07
1156900
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
086HNE0087
Izok Lake
086H10
Cu-Zn-Pb-Ag
528400
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
086ISE0001
Takijuq H-41
086I02
Zn-Cu-Ag
528700
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
086ISE0002
Takijuq H-10
528600
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
086OSW0097
Muskox Intrusion
086O03
Cr-Cu-Ni-Pt-Pd
1077000
Location is the approximate center of the intrusive body.
086KSW0006
G W Group
086K05
529901
086LSE0004
Port Radium
086L01
U-Ra-Ag-Cu-Ni-Pb
927400
Also in CANMINDEX as 00530800.
086LSE0006
URANIUM Group
Cu-U-Ag
927600
Also in CANMINDEX as 00530900. Great Bear Lake area. Part of the old workings of the Eldorado (Prot Radium) mine.
086LSE0007
El Bonanza
Ag-Cu-U-Ni-Pb-Zn
1075300
Also CANMINDEX Number
086NSE0014
Coronation Northwest Zone
086N08
501400
086NSE0121
Wreck Lake
651800
086NNW0070
CARL 7
086N12
507000
086ONW0084
JUNE
086O11
553200
095ENW0002
RAM & ROD Groups
9.50E+1
Cordillera
Pb-Zn-Ag
362100
095FNE0013
Prairie Creek
095F10
Zn-Pb-Ag-Cu-Cd
534999
095LNE0007
Coates Lake
095L10
Cu-Ag
1085000
This showing lies 160 km west of Wrigley, YT.
095MNW0001
Jay (Keele River)
095M13
363200
095MNW0038
June Creek (Keele River)
1088100
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.
095OSW0006
Wrigley
095O04
105HNE0001
Cantung
105H16
W
361200
105ISW0018
Howards Pass (6km East of
105I06
Zn-Pb
1148400
Source: Publication/Thesis
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
105ISE0003
Lened
105I07
W-Cu
441000
105INE0002
PR
105I15
440800
The showing is approximately 48 km NE of Howards Pass.
105OSE0001
Mactung
105O08
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.
106ASW0002
Bear-Twit
106A03
Pb-Zn-Ag-Cu-Sb-C
158600
106BNE0014
Gayna River -1
106B15
1153500
106FSE0002
Crest
106F02
30-Oct-98
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
075MSE0028
JUF
075M01
Reconnaissance
940500
075M01U_001
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.
075MSE0005
COTTONGRASS Au
The COTTONGRASS Au showing is located 200 km NE of Yellowknife, NWT and can be accessed by fixed wing float-equipped aircraft.
075MSE0006
Dawn & Gem-1
Drilled
656700
The Dawn & Gem-1 showing is approximately 120 miles NE of Yellowknife and is accessible by float or ski equipped airplane.
075MSE0007
Dawn & Gem-2
Cu-Zn-Ag-As
656800
The Dawn & Gem-2 showing is approximately 120 miles NE of Yellowknife and is accessible by float or ski equipped airplane.
075MSE0008
Plex Lake
Observed Ore Mineral
656900
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.
075MSE0009
Susu Lake North
657100
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.
075MSE0010
5 Mi West of Susu Lake
657200
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.
075MSE0017
Brislane Lake-1
657900
The showing property lies approximately 135 miles NE of Yelllowknife and is accessible by float or ski equipped airplane.
075MSE0018
Brislane Lake-2
Au-Cu
658000
The Brislane Lake-2 showing is approximately 135 miles from Yellowknife, and is accessible by float or ski equipped airplane.
075MSE0019
BRI-8
Cu-Au
Undrilled
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.
075MSE0020
Taco Island
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.
075MSE0021
Brislane Lake-5
658300
075MSE0022
Brislane Lake-6
658400
075MSE0023
BRI 6
The BRI 6 showing is approximately 190 km north-east of Yellowknife and is accessible by ski or float equipped aircraft.
075MSE0024
BRI 3
The BRI 3 showing is approximately 190 km north-east of Yellowknife and is accessible by ski or float aircraft.
075MSE0025
Brislane Lake - 11
658700
075MSE0026
Brislane Lake - 12
658800
075MSE0027
BRI 5
The BRI 5 showing is approximately 190 km north-east of Yellowknife and is accessible by ski or float equipped aircraft.
075MSE0029
Susu Lake West
1055500
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
075MSE0030
COTTONGRASS Cu
The area is approximately 200 km NE of Yellowknife and is accessible by ski or float equipped airplane.
075MSE0031
Susu Lake West 2
1055700
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.
075MSE0032
HO 16
1055800
075M02CU 007
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.
075MSE0033
Pb No. 5
Cu-Zn
1055900
075M02CU 006
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.
075MSE0034
FLO
1056000
075M02CU 010
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.
75M02CU012
075MSE0040
VOY
1056600
075MSE0041
Benny Bay Zone
Zn-Ag-Pb-Cu
The Benny Bay Zone is approximately 120 miles north-east of Yellowknife and is accessible by ski or floated equipped aircraft.
075MSE0042
Northern Zinc Zone
Zn-Cu-Pb
1056800
The Northern Zinc Zone showing is approximately 120 miles north-east of Yellowknife and is accessible by float or ski equipped aircraft.
075MSE0043
No. 2 Copper Zone
1057100
The No. 2 Copper Zone showing is approximately 120 miles NE of Yellowknife and is accessible by float or ski equipped aircraft.
075MSE0044
Susu Lake East
Be-Nb-Ta
Observed Lithology
1093800
075MSE0045
Brislane Lake
Zn
1093900
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.
075MSW0011
HART
075M05
657300
075M05CU 002
A drill hole testing an HLEM conductor in 1967 yielded a best intersection of 0.26% Zn over 3 feet.
075MSW0012
TIP
Au-Cu-Ag-As
657400
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
075MSW0015
SAN
Cu-Zn-Ni
657700
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
075MSW0038
LEN
Au-Cu-Ni
1056400
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.
075MSW0039
Asp
13-Aug-98
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
075MSW0040
Canoe
Au-Ag-Pb-Zn-Cu
14-Aug-98
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
075MSW0041
WK
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.
075MSW0042
C3
Zn-Cu
075M05CU 005
18-Sep-98
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.
075MSW0044
P2
075MNE0015
CL 25
075M09
10-Aug-98
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.
075MNE0016
CL 174
21-Aug-98
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.
075MNE0013
DOD
075M10
Cu-Ni
657500
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.
075MNE0014
EGO
657600
This showing is approximately 130 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft.
075MNE0017
CL 186
24-Aug-98
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.
075MNE0018
Snap Lake Dyke
26-Aug-98
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.
075MNE0019
Snap Lake Boulders
The Snap Lake boulders are approximately 140 miles northeast of Yellowknife and is accessible by ski or float equipped aircraft.
075MNW0016
CAM
075M11
657800
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.
075MNW0035
PEP
1056100
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
075MNW0004
BAY Group
075M12
Below Cutoff - Drille
442600
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.
075MNW0003
TALL2
075M14
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
075MNW0036
SECUM
1056200
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
075MNW0037
KM
1056300
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
075MNW0046
Mackay Lake Nodica Narrows
1094000
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
075MNW0047
BERTHA 5
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
075MNW0048
BERTHA 6
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
075MNW0049
TALL
11-Aug-98
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
075MNW0050
HARE 8
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
075N03
075yellow
31-Jan-00
Yellowknife City
076GSE0006
Dox 0759
076G02
1098500
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.
076GSE0009
Ira
Cu-Ag-Au-Mo
6-Apr-98
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
076GSE0010
Beech 1
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.
076GSE0011
Beech
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
076GSE0012
Casey Lake
7-Apr-98
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.
076GSE0013
GM7
strike 120-130 dip 70-75 E  Metavolcanic rocks occur as a series of fault bounded lenses
076GSW0010
Needle Lake
076G03
3-Mar-98
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
076GSW0011
Moth Valley
5-Mar-98
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
076GSW0012
Gollum Lake
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.
076GSW0013
North Gollum Lake
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
076GSW0014
Phaedrus Lake
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
076GSW0015
North Jaeger Lake
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
076GSW0016
BLS-3
6-Mar-98
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
076GSW0017
Feather Lake
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
076GSW0018
Bor Lake
9-Mar-98
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
076GSW0019
Bor Lake SE
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
076GSW0020
Zone F
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
076GSW0021
Bee
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.
076GSW0022
Robbs Pond
10-Mar-98
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.
076GSW0023
Dox 2380
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.
076GSW0024
Dox 2384
The latitude and longitude given are for the single sample site (gold) that comprises this  showing.
076GSW0025
Dox 2372
12-Mar-98
The latitude and longitude given are from the single sample site (gold) that comprises this  showing.
076GSW0026
HG-106
18-Mar-98
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.
076GSW0027
FG-74
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
076GSW0003
Hunt
076G04
Cu-Zn-Pb-Co-As
442500
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.
076GSW0007
Fidler Lake
1098600
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.
076GSW0008
Ack
1098700
076G04AU 002
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
076GSW0035
Alb
20-Apr-98
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.
076GSW0036
Barrel
23-Apr-98
The Barrel showing is approximately 420 km NW of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.
076GSW0037
Algood
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.
076GSW0038
South Fidler Lake
30-Apr-98
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.
076GSW0039
Narrow Lake
5-May-98
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.
Conjugate fault trends N10W, 2 metres wide
076GSW0040
MG1
6-May-98
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.
076GSW0041
Grid 4
7-May-98
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.
076GSW0042
Grid 5
8-May-98
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.
076GSW0043
Grid 2
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.
076GSW0044
Grid 3
11-May-98
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.
076GSW0045
Kate Zone
12-May-98
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.
076GSW0046
Twin Lake East
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.
076GSW0047
Fire
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.
076GSW0048
Syn
13-May-98
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.
076GSW0049
A0902
14-May-98
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.
076GSW0050
A0865
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.
076GSW0051
A0912 & A0913
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.
076GSW0052
Uist Lake
19-May-98
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.
076GSW0053
DC Grid
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.
076GSW0054
H Grid
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.
076GSW0055
As Grid
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.
076GSW0056
Soc
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.
076GSW0057
FFB
21-May-98
This showing is part of the Soc showing. For further information and references see Normin ID # 076GSW0056
076GSW0058
Main
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.
076GSW0059
West Main
This showing is part of the Main showing. For further information and references see Normin ID # 076GSW0058
076GSW0060
Fire 10
Zn-Pb-Ag
25-May-98
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.
076GSW0061
Uist 1
27-May-98
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.
076GSW0062
Eds Showing
29-May-98
This showing is part of the Uist 1 showing. For further information and references see Normin ID # 076GSW0061.
076GSW0033
Gaet
15-Apr-98
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.
076GSW0034
Gaet 4
16-Apr-98
The latitude and longitude given are taken from a single sample site of map 1 accompanying assessment report 083071.
076GSW0063
IM 1
1-Jun-98
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.
076GSW0064
Triangle Lake
The Triangle Lake Showing is part of the IM 1 Showing (ID 076GSW0063). The IM 1 Showing is approximately 700 m NW along strike.
076GSW0065
Orc
Zn-Au-Cu
4-Jun-98
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.
076GSW0028
KG-97A
076G06
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
076GSW0029
KG-117 & KG-140
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
076GSW0030
Dior
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
076GSW0031
Sed
The latitude and longitude is from the site of the highest gold value.
AR #82966 states that the metamorphic grade varies from greenshist to amphibole within the sedimentary package
076GSW0032
Gersdorffite
Ni-Cu-Pd
30-Mar-98
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.
076GSE0007
Burnside
076G07
13-Mar-98
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
076GSE0008
Skarn
17-Mar-98
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
076GNE0006
Ellice River
9-Jan-98
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
076GNE0010
Boot Lake
30-Jan-98
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
076GNE0011
Winter
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
076GNE0012
Rooster-Hammer
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.
076GNE0013
Dumbo Lake
9-Feb-98
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.
076GNE0014
Shell Lake
20-Feb-98
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
076GNE0018
Goose Neck
25-Feb-98
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.
076GNE0007
Trout Lake
076G10
28-Jan-98
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
076GNE0008
Scorpion Lake North
29-Jan-98
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
076GNE0009
Scorpion Lake
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)
076GNE0015
Boulder Pond
23-Feb-98
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
076GNE0016
Soi Lake
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
076GNE0019
Goose Creek
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.
076GNE0020
Llama Lake
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
076GNW0014
Knight
076G11
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.
076GNW0002
Yava
076G12
159300
076G12ZN 001
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.
076GNW0018
Gaet 3
3-Jun-98
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.
076GNW0019
Trumpet
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
076GNW0020
Oboe
076GNW0021
Piccalo
8-Jun-98
076GNW0022
Flute
076GNW0023
Buck
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
076GNW0024
Buck North
11-Jun-98
076GNW0025
Chopin
076GNW0026
Lin
12-Jun-98
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.
076GNW0027
Mozart
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.
076GNW0028
Bach
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
076GNW0029
Lin 1
15-Jun-98
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.
076GNW0030
Lin 2
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.
076GNW0031
WL1
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.
076GNW0032
Nuts
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.
076GNW0033
51536
This showing consists of a single reconnaissance sample
076GNW0034
51535
16-Jun-98
This showing is a single reconnaissance sample that had a gold value of 0.51 g/tonne.
076G13
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
076GNW0017
Dex
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.
076GNW0004
Rifle Lake
12-Feb-98
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.
076GNW0005
Komatik Lake
16-Feb-98
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
076GNW0006
Mouse
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
076GNW0007
Bullwinkle Lake
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
076GNW0008
Takrark Lake
17-Feb-98
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
076GNW0009
4LBZ005
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
076GNW0010
West Rapids
18-Feb-98
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
076GNW0011
Oar Lake
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.
076GNW0012
Shadow Pond
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.
076GNW0013
Lookout Hill
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.
076GNW0015
U-1
U-Au-Pb
8-Apr-98
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.
076GNW0016
U-2
9-Apr-98
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.
076GNE0004
Western River 1
076G16
526000
Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District Of Mackenzie
076GNE0005
Western River 2
1061300