Ontario Geological Survey
Permanent Link to this Record:
MDI52E10NE00013
Record Name(s) | Inglis Lake - 1990, Waite Option - 1936, Westricia Occurrence - 1937, Williams Option - 1936 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1990-Dec-08 |
Date Last Modified | 2022-Nov-28 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Clearwater Bay Area
Latitude: 49° 43' 10.06" Longitude: -94° 40' 58.39"
UTM Zone: 15 Easting: 378695 Northing: 5508799 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52E10NE
Point Location Description: Trenches on map in Assessment report 52E10NE8994
Location Method: Data Compilation
1936: J.H.C. Waite optioned the property and carried out prospecting. 1937: Westricia Gold Mines Ltd. took over these claims and continued with surface trenching and test pitting. 1983: Atikwa Resources Inc. carried out geological mapping.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.6754, 52E10NE Y-1 | 52E10NE8994 | 52E10NE8994 |
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | quartz | Host |
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Mafic Tuff | 2 |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Galena | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Gold | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Tourmaline | Economic | Gangue |
Nov 28, 2022 (Therese Pettigrew) - Surface prospecting revealed a few veins, one of which was found to carry gold values over a length of 400 feet. This lies near the southeastern corner of Inglis Lake on claim K 5849. The vein is narrow, averaging less than a foot in width (Thompson, 1936). The Williams Vein is located in the eastern part of claim 697447 near the southeastern corner of Inglis Lake. This vein consists of a narrow quartz vein which strikes north 80 degrees east and is vertical or steeply dipping either to the northwest or southeast. The vein was stripped continuously for 335 feet, with width ranging from 1 to 38 inches and averaging 8 inches. The quartz itself is a white, sugary to vitreous type, containing a large amount of tourmaline. Mineralization consists of pyrite, galena, chalcopyrite, and some small particles of visible gold. Samples taken in 1936 returned values of $0.35 over 8" (0.012 oz/t Au over 20 cm) up to $13.30 over 36" (0.44 oz/t Au over 91 cm)and $14.00 over 6" (0.47 opt Au over 15 cm) (Assessment report 52E10NE8994).
Jul 26, 2022 (Q Unknown) - Grade: 0.14 opt Au over 22 cm and 0.22 opt Au over 80 cm.
Map - North central part of the Lake of the Woods, District of Kenora, Ontario
Publication Number: ARM45B Scale: 1:63,360 Date: 1997
Author: Thomson J.E.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold deposits of the Kenora-Fort Frances area, districts of Kenora and Rainy River
Publication Number: MDC016 Page: 42 Date: 1976
Author: Beard R.C., Garratt G.L.
Publisher Name: Ontario Division of Mines
Location:
Part - Geology of the north central part of the Lake of the Woods
Publication Number: ARV45-03.001 Page: 36 Date: 1997
Author: Thomson J.E.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Reconnaissance investigation of the geology of Yarrow and Doon townships, District of Timiskaming, with emphasis on the Huronian Supergroup
Publication Number: OFR5696 Page: 173-174 Date: 1989
Author: Junnila R.M.
Publisher Name: Ontario Geological Survey
Location:
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