Ontario Geological Survey
Permanent Link to this Record:
MDI42C01NW00049
Record Name(s) | Firepump Lake Zone - 1990, Hamilton Pyrite - 1916 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2001-Apr-30 |
Date Last Modified | 2022-Sep-07 |
Created By | |
Revised By |
Primary Commodities: Gold, Iron
Township or Area: Cowie
Latitude: 48° 10' 48.13" Longitude: -84° 27' 46.88"
UTM Zone: 16 Easting: 688581 Northing: 5339423.22 UTM Datum: NAD83
Resident Geologist District: Sault Ste. Marie
NTS Grid: 42C01NW
Point Location Description: Stripped area between Forge and Firepump Lake
Location Method: Based on Assessment
Access Description: The site is accessible from Hawk Junction. Drive north along the Alden Station road (parallel to the ACR tracks) for 11.4 km to where the rail crossing has been taken out. Drive east along the Forge Lake access road for 7 km. The lake is located on the south side of the road.
1913-1914: trenching. 1989-90: Corona Corporation - prospecting, mapping, ground geophysical survey, soil survey, stripping, trenching. 1991-92: Noranda Exploration Co. Ltd. - sampling, till sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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WP ABOTOSS.26 | ||
WP.ABOTOSS.25 | ||
WP Corbiere-14 | 42C06SE0002 | 42C06SE0002 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Michipicoten
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (A Wilson) - The lithologies north of the Hawk Lake granite complex are variously sheared over a width of 750 to 1500 m. The north limit of the shear is the north contact of the main sedimentary unit and within 100 m f this contact towards the north. The south limit is marked by the supracrustal-granite contact.
Rock Type | Rank | Composition | Texture | Relationship | Schist-Unsubdivided | 1 | Chlorite | Host |
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Vein | 2 | Quartz-Carbonate | Host |
Dec 07, 2005 (A Wilson) - Stripping has exposed a sequence of intense shearing. The chlorite schist and chlorite-sericite-ankerite schist are intruded by sheared quartz-feldspar porphyry dikes. The quartz veining has been extensively disrupted to form a quartz vein breccia.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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Ankerite | Alteration | Carbonatization | 1 | Medium | Replacement |
Dec 07, 2005 (A Wilson) - Grab samples collected by Corona Corporation returned values up to 17 g/t Au. The highest gold values are returned from areas of ankerite-pyrite alteration. The best assay value was 3.1 g/t Au over 0.8 m.
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Irregular | 500 | 20 | 90 | 67 |
File - Resident Geologist files WP Abotossaway.25, WP Abotossaway.26
Publication Number: Date:
Author:
Publisher Name:
Location: SSM RGP office
Map - Geological compilation series, Wawa sheet, districts of Algoma and Sudbury
Publication Number: P0640 Scale: 1:126,720 Date: 1997
Author: Leahy E.J., Rupert R.J., Giblin P.E., Giguere J.F.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Mono - Pyrite deposits of Ontario
Publication Number: MDC005 Page: 29 Date: 1967
Author: Hewitt D.F.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Iron deposits of Ontario
Publication Number: MDC011 Page: 48 Date: 1968
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Goudreau and Michipicoten gold areas, District of Algoma
Publication Number: ARV40-04.001 Page: 5 Date: 1998
Author: Moore E.S.
Publisher Name: Ontario Dept. of Mines
Location:
Book - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Page: 10 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
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