Ontario Geological Survey
Permanent Link to this Record:
MDI42E10NW00039
Record Name(s) | Algoma Iron - 1980, Barton Bay Iron - 1980 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Developed Prospect With Reported Reserves or Resources |
Date Created | 1980-Mar-27 |
Date Last Modified | 2022-May-09 |
Created By | |
Revised By |
Primary Commodities: Iron
Township or Area: Errington
Latitude: 49° 41' 54.26" Longitude: -86° 58' 35.32"
UTM Zone: 16 Easting: 501696.24 Northing: 5505099.12 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 42E10NW
Point Location Description: Precise
Location Method: Conversion from MDI
1967-68: Little Long Lac Gold Mines conducted 1525 m of drilling for iron formation. 1970: Algoma Steel conducted line cutting. 1971: Algoma Steel conducted a magnetometer survey and trenching and drilled 3 DDH totalling 497 m. 1972: Algoma Steel took a 1170 t bulk sample. 2007: optioned from Roxmark Mines Ltd. by Premier Gold Mines Ltd. as part of the Hardrock Project.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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10 | 42E11NE0021 | 42E11NE0021 |
2.389 | 42E10NW0179 | 42E10NW0179 |
Rock Type | Rank | Composition | Texture | Relationship | Terrigenous-Clastic-Unsubdivided | 1 | Host |
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Ironstone-unsubdivided | 2 | Host | ||
Gabbroid-Unsubdivided | 3 | Adjacent |
Nov 30, 2015 (Therese Pettigrew) - The core logs describe the metasediments as fine dark green argillaceous sediment with horizons of up to 0.67 m of coarser quartzite. 1 cm thick bands of magnetic iron formation are scattered over the section with pyrite occurring as thin horizons and disseminated over sections of the sediments (AFRI 42E11NE0021). Banded iron formation (BIF) can be traced within the Beardmore-Geraldton Belt from at least the Klotz Lake area east of Longlac to Beardmore in the west and, by aeromagnetic expression, beneath the Nipigon Plate rocks to the west of Lake Nipigon. The BIF units tend to be less than 20 metres thick although thicknesses in excess of 60 metres are present, in areas of structural complexity; e.g. the island in Barton Bay. The BIF consists of mesobands of principally magnetite with minor hematite alternating with mesobands of either chert or siltstone (Macdonald, 1988).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Magnetite | Economic | Ore | ||||
2 | Hematite | Economic | Ore | ||||
3 | Pyrite | Economic | Ore |
Nov 30, 2015 (Therese Pettigrew) - The iron-bearing minerals are fine-grained and in a ratio of 2:1 hematite to magnetite.
Rank | Classification |
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1 | Sedimentary |
Rank | Characteristic |
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1 | Stratiform |
Date: Jul 10, 2009
Geologist: M Smyk
Notes: Visit from the Thunder Bay North RGP staff located the bulk sample pit at Zone 16, 501855E, 5505139N. Long Trench was located at Zone 16, 501773E, 5505118N to 501825E, 5505190N
Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
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Barton Bay | 1971 | Unclassified | 50000000 | Thunder Bay North Resident Geologist’s office files | Iron 25.2 Percent |
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Page: 266 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
File - Resident Geologist Mineral Deposit Files
Publication Number: Min Dep Date: 1996
Author:
Publisher Name:
Location: Thunder Bay RGP
Map - Township of Errington, District of Thunder Bay, Ontario
Publication Number: M1951-07 Scale: 1:12,000 Date: 1997
Author: Horwood H.C., Pye E.G.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - The Geraldton gold camp: the role of banded iron formation
Publication Number: OFR5694 Date: 1988
Author: Macdonald A.J.
Publisher Name: Ontario Geological Survey
Location:
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