Ontario Geological Survey
Permanent Link to this Record:
MDI52C16SW00002
Record Name(s) | Alice A - 1894, Archibald Location - 1984 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1984-Aug-07 |
Date Last Modified | 2022-Mar-03 |
Created By | |
Revised By |
Primary Commodities: Gold, Zinc
Secondary Commodities: Lead
Township or Area: Bennett Lake Area
Latitude: 48° 45' 48.74" Longitude: -92° 28' 36.04"
UTM Zone: 15 Easting: 538458 Northing: 5401302 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52C16SW
Point Location Description: Precise
Location Method: Conversion from MDI
1894: the first reported trenching, sampling, and surface observation. 1887-99: Owned by American-Canadian Gold Mining Company, who sunk No. 1 shaft to 95 feet (29 m) with a crosscut driven north 35 feet at a depth of 60 feet, and No. 2 shaft to 70 feet (21 m). 150 to 200 tons were treated by a two-stamp mill. 1900: the English company that bought the property had difficulty raising money required to build a 100-stamp mill. The property reverted back to the Crown. 1926: H.K. Bridger staked the property and optioned it to G.B. Butterworth, who formed an association known as “The Mining Group” to provide financing. Development work included trenching, pitting, and cleaning out old open cuts and shafts. 1974: R. Pitkanen carried out stripping and trenching. 1975: Hanna Mining Company conducted magnetic and EM surveys. 1980: J.W. Redden staked the property. 1985: J.W. Redden conducted a magnetic survey. 1987: J.W. Redden conducted magnetic and VLF-EM surveys. 1988: Fire River Gold Corp. carried out line cutting, geological mapping, sampling, a magnetometer survey, geochemical survey, and humus sampling. 1990: Fire River Gold Corp. carried out a VLF-EM survey, trenching, and sampling. 1996: R. Cousineau, L. Cousineau, and K. Desjardins carried out stripping, trenching, blasting, and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
2.50545 | 20000007049 | 20000007049 |
2.13429 | 52C16SW8249 | 52C16SW8249 |
2.2297 | 52C16SW0428 | 52C16SW0428 |
63.3367 | 52C16SW0035 | 52C16SW0035 |
63.4808 | 52C16SE0005 | 52C16SE0005 |
2.54663 | 20000008971 | 20000008971 |
2.17085 | 52C16SW0012 | 52C16SW0012 |
2.57265 | 20000014841 | 20000014841 |
2.11617 | 52C16SW8245 | 52C16SW8245 |
2.12455 | 52C16SW8246 | 52C16SW8246 |
2.2081 | 52C16SW8253 | 52C16SW8253 |
2.8241 | 52C16SW8255 | 52C16SW8255 |
2.10548 | 52C16SW8243 | 52C16SW8243 |
2.10549 | 52C16SW8244 | 52C16SW8244 |
2.6399 | 52C16SW8254 | 52C16SW8254 |
Province: Superior
Subprovince: Wabigoon
Terrane: Western Wabigoon
Belt: Fort Frances-Mine Centre
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Felsic lava flow-unsubdivided | 1 | Host |
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Vein | 2 | Host | ||
Schist-Unsubdivided | 3 | Adjacent | ||
Conglomerate | 4 | Adjacent |
Sep 15, 2020 (Therese Pettigrew) - The Alice A Prospect is situated between the east-west trending Quetico Fault and the northeast-southwest trending Seine River Fault. The area is underlain by steeply dipping east-west striking, felsic to mafic metavolcanics. The metavolcanics are composed of sericite-chlorite-carbonate schists which may have originally represented a sheared and silicified rhyolite flow or a felsic fragmental rock such as a tuff or lapilli-tuff. Mafic metavolcanics, present as chlorite schists are encountered on the north portion of the property. Shearing is prominent throughout the Alice A property; the shearing strikes approximately east-west with dips of 80 degrees north to vertical (Schneiders and Dutka, 1985). The property is underlain by foliated rhyolitic metavolcanic rocks. The intense cleavage strikes 265 degrees, is near vertical and is roughly parallel with the Quetico Fault, approximately 800 m to the north (Poulsen, 2000).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Sphalerite | Economic | Ore | ||||
2 | Galena | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Pyrite | Economic | Ore | ||||
5 | Gold | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Ankerite | Economic | Gangue | ||||
3 | Siderite | Economic | Gangue |
Sep 15, 2020 (Therese Pettigrew) - Quartz-carbonate veins and stockwork appear associated within east-trending lenticular shear zones. The host rocks are felsic to mafic pyroclastic rocks. The quartz-carbonate veining is very erratic varying in width from 1 cm to over 20 cm. Generally, the veins are parallel to the shearing. Visible mineralization consists of pyrite, chalcopyrite, galena, sphalerite and gold with accessory minerals including sericite, chlorite and carbonate. Samples collected by OGS staff in 1982 returned up to 1.06 opt Au and 1.50 opt Ag from a glassy, white quartz-carbonate vein containing 8% galena, 5% sphalerite, 4% pyrite, and 2% chalcopyrite (Schneiders and Dutka, 1985). Gold-bearing quartz veins and inch-wide (2.5 cm) stringers occur as en echelon arrays and are parallel to foliation in the metavolcanic rocks. Veins are commonly folded or possess a sigmoidal shape. Accessory minerals include ankerite, siderite, sphalerite, galena, chalcopyrite and pyrite (Poulsen, 2000). Alice A consists of 60 cm to 90 cm stringer-rich zones of folded quartz with ankerite, sphalerite, galena, chalcopyrite, pyrite in altered rhyolite. A historical assay done in 1899 yielded 17 gpt Au from 10-ton test. Samples taken by Fire River Gold returned 0.21 oz/t Au, 5750 ppm Pb, and 5260 ppm Zn from the Shaft 1 (western shaft) location (Assessment report 52C16SW8249). Sample 1300 returned 12.24 g/t Au from the west shaft rubble, composed of quartz vein containing 2% pyrite, 15% seared wall rock, and 15% intermediate volcanic with quartz stringers. Sample 1286 returned 5.115 g/t Au from a red quartz vein containing oxidized pyrite. Sample 1289 returned 3.781 g/t Au from a pink quartz vein (Assessment report 20000007049).
Mono - Property visits and reports of the Atikokan economic geologist, 1979-1983, Atikokan geological survey
Publication Number: OFR5539 Scale: Date: 1985
Author: Schnieders B.R., Dutka R.J.
Publisher Name: Ontario Geological Survey
Location:
Part - Fourth report on the west Ontario gold region
Publication Number: ARV07-02.001 Scale: Date: 1998
Author: Coleman A.P.
Publisher Name: Ontario Bureau of Mines
Location:
Mono - The geological setting of mineralization in the Mine Centre-Fort Frances area, District of Rainy River
Publication Number: OFR5512 Scale: Date: 1984
Author: Poulsen K.H.
Publisher Name: Ontario Geological Survey
Location:
Part - Mines of northwestern Ontario
Publication Number: ARV08-01.004 Scale: Date: 1998
Author: Bow J.A.
Publisher Name: Ontario Bureau of Mines
Location:
Mono - Gold deposits of the Kenora-Fort Frances area, districts of Kenora and Rainy River
Publication Number: MDC016 Scale: Date: 1976
Author: Beard R.C., Garratt G.L.
Publisher Name: Ontario Division of Mines
Location:
Part - Mines of northwestern Ontario
Publication Number: ARV09.003 Scale: Date: 1998
Author: Bow J.A.
Publisher Name: Ontario Bureau of Mines
Location:
Mono - Geological Setting of Mineralization in the Mine Centre-Fort Frances Area
Publication Number: MDC029 Scale: Date: 2000
Author: Poulsen K.H.
Publisher Name: Ontario Geological Survey
Location:
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