Ontario Geological Survey
Permanent Link to this Record:
MDI42E13SW00008
Record Name(s) | Crooked Green Creek Mine - 1966, Cowan Mine - 1972, Green Lake Gold Mine - 1947, Algoma Development - 1972, Northern Concentrators - 1981, N. Smith - 1946 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Prospect |
Date Created | 1987-Oct-23 |
Date Last Modified | 2022-Jul-19 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper, Silver
Township or Area: Pifher
Latitude: 49° 47' 52.23" Longitude: -87° 49' 7.66"
UTM Zone: 16 Easting: 441074 Northing: 5516475.99 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 42E13SW
Point Location Description: Shaft location in AFRI 42E13SW0059
Location Method: Conversion from MDI
Access Description: Access is via Highway 801 which runs northwest from a point on Highway 11 (the Trans-Canada Highway), 26 km east of Beardmore. A bush road turns south from Highway 801 at a point 21 km from Highway 11, and leads directly to the property, a distance of approximately 7 km.
1946: N. Smith found gold and staked claims covering the No. 1 vein. 1947: Green Lake Gold Mines conducted trenching and drilled 21 DDH. 1958-60: Chellew Gold Mines acquired the property. Martin-Sturgeon Syndicate optioned the ground from Chellew and conducted trenching, stripping, sampling and drilled 20 DDH totalling 1940 m. 1962: W. Brown optioned the ground and drilled holes. 1964: T. Christianson restaked the property. 1965: Christianson conducted bulk sampling. 1966-67: Crooked Green Creek Mine Ltd. drove an inclined shaft at 45 degrees to 38 ft and conducted diamond drilling and sampling. 1972: Algoma Development Co. acquired the property. 1981: Company name was changed to Northern Concentrators, who conducted seasonal small-scale mining operations. 1983: a joint venture of Great Western Petroleum Corp. and Anglo-Canadian Mining Corp. called Thunder Bay Joint Venture optioned part of the property from Northern Concentrators. 1984: Thunder Bay JV conducted bulk sampling. 1985: Thunder Bay JV conducted magnetic and VLF geophysical surveys, and diamond drilling on the No. 1 and 2 zones. 1987: mining operations were suspended. 1987-89: Parklane Tech conducted mapping and mag/VLF geophysical survesy, drilled 39 DDH mainly on the No. 2 vein, and took a 500 t bulk sample from the No. 2 vein. 1995-6: Spruce Ridge Resources Ltd. acquired the property and conducted sampling on the No. 2 vein pit, followed by a 10 ton bulk sample from the same site. 1997: Spruce Ridge conducted line cutting, magnetometer, VLF-EM, and IP geophysical surveys, a soil geochemistry survey, and trenching. 2001: Spruce Ridge drilled 23 DDH totalling 887 m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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63.3992 | 52N04SE0068 | 52N04SE0068 |
43 | 42E13SW0023 | 42E13SW0023 |
37 | 42E13SW0064 | 42E13SW0064 |
2.8453 | 42E13SW0041 | 42E13SW0041 |
44 | 42E13SW0025 | 42E13SW0025 |
18 | 42E13SW0084 | 42E13SW0084 |
22 | 42E13SW0075 | 42E13SW0075 |
17 | 42E13SW0090 | 42E13SW0090 |
2.18766 | 42E13SW2003 | 42E13SW2003 |
63.3993 | 42E13SW0063 | 42E13SW0063 |
2.4846 | 42E13SW0065 | 42E13SW0065 |
2.5756 | 42E13SW0059 | 42E13SW0059 |
63.4304 | 42E13SW0043 | 42E13SW0043 |
2.5722 | 42E13SW0054 | 42E13SW0054 |
63.6060 | 42E13SW0018 | 42E13SW0018 |
2.6216 | 42E13SW0052 | 42E13SW0052 |
2.6330 | 42E13SW0045 | 42E13SW0045 |
2.15381 | 42E13SW0002 | 42E13SW0002 |
OP92-391 | 42E13SW0076 | 42E13SW0076 |
2.17009 | 42E13SW0105 | 42E13SW0105 |
2.25120 | 42E13SW2011 | 42E13SW2011 |
35 | 42E13SW0057 | 42E13SW0057 |
63.2982 | 42E13SW0102 | 42E13SW0102 |
46 | 42E13SW0051 | 42E13SW0051 |
Province: Superior
Subprovince: Wabigoon
Terrane: Eastern Wabigoon
Belt: Onaman-Tashota
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Felsic Tuff | 1 | Rhyolite | Tuffaceous | Host |
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Mafic lava flow-unsubdivided | 2 | Near | ||
Vein | 3 | Quartz | Contains | |
Feldspar Porphyry | 4 | Feldspar | Near | |
Diabase | 5 | Diabase | Near | |
Intermediate lava flow-unsubdivided | 6 | Dacite And Andesite | Near |
Mar 18, 2016 (Therese Pettigrew) - The oldest rocks are banded to massive felsic metavolcanic flows and tuffs of rhyolite-dacite composition, which underlie the eastern half of the property. Overlying these are intermediate to mafic massive flows and minor intrusives. Fine-grained, crowded feldspar porphyries occur as irregular masses intruding older rocks, although they may be extrusive in part. One north-striking diabase dyke was noted in the southern part of the claims. Bedding attitudes are displayed only in banded rhyolite tuffs and where seen, predominant strikes are west-northwest with moderate to steep dips to the north. Major faults strike north-easterly, as exemplified by Forge Creek drainage and the alignment of Smith Lake (OFR5630).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Quartz | Economic And Alteration | Gangue | Silicification | 1 | Unknown | Disseminated |
1 | Chalcopyrite | Economic | Ore | ||||
2 | Pyrrhotite | Economic | Ore | ||||
3 | Gold | Economic | Ore | ||||
4 | Sphalerite | Economic | Ore | ||||
5 | Pyrite | Economic | Ore | ||||
6 | Marcasite | Economic | Ore | ||||
7 | Hematite | Economic | Ore | ||||
Sericite | Alteration | Sericitization | 2 | Unknown | Disseminated | ||
Chlorite | Alteration | Chloritic | 3 | Unknown | Disseminated |
Mar 18, 2016 (B Nelson) - The following are some economic features of the occurrence (as of 1947): No. 1 zone had a weighted average of 1.32 oz/ton Au over 0.4 m. No. 2 zone: 9 D.D.H. intersected an average of 0.379 oz/ton Au over 1.4 m. One deeper hole intersected 0.5 m of 0.77 oz/ton Au. Crooked Green Creek Mine Ltd, in 1967, had results of 5.8 oz/ton Au and 3% Cu across 50.8 cm in a channel sample. A 170 ton bulk sample averaged 1.65 oz/ton Au, 0.44 oz/ton Ag and 1% Cu. The No. 2 Zone yielded chip samples of 2.36 oz/ton Au over 0.8 m. Chip samples by T. Christianson (1966) assayed 20.3 oz/ton Au over 0.9 m.
Mar 18, 2016 (Therese Pettigrew) - Three major mineralized zones occur on the property and are numbered 1, 2 and 4. Mineralization in all veins consists of chalcopyrite, pyrrhotite and gold with minor sphalerite, pyrite, marcasite and hematite. The veins are typically coarse-grained, brecciated and smokey to blue-black. Sulphides can be very coarse and often are located in crushed quartz material surrounding larger quartz fragments. Gold is often free gold in the pyrrhotite or chalcopyrite. Chalcopyrite, pyrrhotite and low gold values occur as jointing or fracture fillings in the host rock. Sulphide content ranges from 1 to 20%. Altered host rock that is incorporated in the veins can be altered to chlorite. The No. 1 zone vein, which has been the site of much of the exploration and development to date, is a sigmoidal, east-northeast-trending quartz vein cutting a feldspar porphyry hosted in dacite and minor rhyodacite. The vein dips 45 to 70 degrees S and is 0.3 to 0.6 m wide near the abandoned inclined shaft; to the west the vein dips 70 degrees and narrows to 5 cm. The No. 2 zone is located 459 m (1,500 feet) west of No. 1 vein, strikes east-west and has been traced for 70 feet (21.3 m). The No. 2 zone consists of a minimum of 3 veins and resembles the No. 1 vein in terms of texture and colour. The No. 2 zone is hosted by intercalated banded chert, rhyolite and andesite. During the summer of 1983, this occurrence was first opened up. Initially, two flat veins cut a third more steeply dipping vein, but after seven rounds of blasting and mucking, it was evident all three veins flattened to perhaps one vein. All veins are auriferous. Numerous discontinuous quartz lenses occur near the three veins (OFR5630). Sampling of the No. 2 vein by Spruce Ridge Resources in 1995 returned assays that ranged from 1.13 g/t Au to 45.35 g/t Au (AFRI 42E13SW2003).
Mar 18, 2016 (B Nelson) - Altered host rock that is incorporated in the veins can be altered to chlorite.
Rank | Classification |
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1 | Vein |
Date: Dec 30, 1996
Geologist: B Nelson
Notes: The Beardmore-Geraldton Economic Geologist visited the occurrence July 14, 1981, July 1982, August 1982, June 21, 1983, July 7, 1983, Sept 20, 1983, Sept 27, 1983, October 24, 1983, June 5, 1984, June 12, 1984, July 20, 1984, August 7, 1984, August 28, 1984, October 11, 1984, and June 12, 1985.
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
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No. 2 Vein Zone | 1984 | Unclassified | 7500 | Carter and Eccles (1984), OFR5630 p. 183 | Gold 12 Grams per Tonne | |
No. 1 Vein Zone | 1984 | Unclassified | 25000 | Carter and Eccles (1984), OFR5630 p. 183 | Gold 12 Grams per Tonne |
Year | Tonnes | Commodities | Reference | Comment |
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1984 | 490 |
Gold 227.8 Ounces |
OFR 5630 | 213 tons at 0.394 oz/t Au (13.5 g/t Au) from No. 1 Vein and 327 tons at 0.44 oz/t Au (15.08 g/t Au) from No. 2 Vein |
1982 | 331 |
Gold 69.35 Ounces |
OFR 5630 | 365 tons at 0.19 oz/t Au (6.51 g/t Au) |
1981 | 317 |
Gold 87.5 Ounces |
OFR 5630 | 350 tons at 0.25 oz/t Au (8.57 g/t Au) |
1980 | 181 |
Gold 86 Ounces |
OFR 5630 | 200 tons at 0.43 oz/t Au (14.74 g/t Au) |
Article - Gold mineralization in the Beardmore-Geraldton area
Publication Number: MP110.007 Page: 84-97 Date: 1997
Author: Mason J.K., McConnell C.D.
Publisher Name: Ontario Geological Survey
Location:
Mono - Gold occurrences, prospects, and deposits of the Beardmore-Geraldton area, districts of Thunder Bay and Cochrane
Publication Number: OFR5630 Page: 178-185 Date: 1986
Author: Mason J.K., White G.D.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological series, Precambrian geology, Pifher Township, District of Thunder Bay
Publication Number: P3078 Scale: 1:15,840 Date: 1988
Author: Kresz D.U., Zayachivsky B.
Publisher Name: Ontario Geological Survey
Location:
Map - Sturgeon River gold area, District of Thunder Bay, Ontario
Publication Number: ARM45A Scale: 1:63,360 Date: 1998
Author: Bruce E.L., Laird H.C.
Publisher Name: Ontario Dept. of Mines
Location:
Part - The western part of the Sturgeon River area (Sturgeon R.-Beardmore section)
Publication Number: ARV45-02.002 Page: 60-117 Date: 1998
Author: Laird H.C.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Tashota-Geraldton sheet, geological compilation series, Thunder Bay and Cochrane districts
Publication Number: M2102 Date: 1997
Author: Pye E.G., Harris F.R., Fenwick K.G., Baillie J.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Conglomerate Lake area, District of Thunder Bay
Publication Number: R197 Date: 1980
Author: Amukun S.E.
Publisher Name: Ontario Geological Survey
Location:
Compend - Report of activities, 1983, Regional and Resident Geologists
Publication Number: MP117 Page: 47-106 Date: 1984
Author: Kustra C.R.
Publisher Name: Ontario Geological Survey
Location:
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