Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42E13SW00008

Record: MDI42E13SW00008

General

Mineral Record Identification
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
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

Commodities

Primary Commodities: Gold

Secondary Commodities: Copper, Silver



Location

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.



Exploration History

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.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
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

Geology

Province: Superior

Subprovince: Wabigoon

Terrane: Eastern Wabigoon

Belt: Onaman-Tashota

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Felsic Tuff 1 Rhyolite Tuffaceous Host
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

Lithology Comments

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).




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1QuartzEconomic And AlterationGangueSilicification1UnknownDisseminated
1ChalcopyriteEconomicOre
2PyrrhotiteEconomicOre
3GoldEconomicOre
4SphaleriteEconomicOre
5PyriteEconomicOre
6MarcasiteEconomicOre
7HematiteEconomicOre
SericiteAlterationSericitization2UnknownDisseminated
ChloriteAlterationChloritic3UnknownDisseminated

Mineralization Comments

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).



Alteration Comments

Mar 18, 2016 (B Nelson) - Altered host rock that is incorporated in the veins can be altered to chlorite.




Mineral Record Details

Classification
RankClassification            
1 Vein

Site Visit Information

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.



Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
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
Production Data
Year Tonnes Commodities Reference Comment
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)

References

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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For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office