Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52J02SE00047

Record: MDI52J02SE00047

General

Mineral Record Identification
Record Name(s) Coveney Island - 1955, New Santiago #2 - 1955
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1995-May-26
Date Last Modified 2023-Jun-09
Created By
Revised By

Commodities

Primary Commodities: Thorium, Uranium

Secondary Commodities: Cerium, Lanthanum, Niobium, Rare Earth Elements



Location

Township or Area: Squash Lake Area

Latitude: 50° 0' 18.17"    Longitude: -90° 43' 46.35"

UTM Zone: 15    Easting: 662692.78   Northing: 5541662.05    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52J02SE

Point Location Description: Precise

Location Method: Conversion from MDI



Exploration History

1955: property optioned by New Santiago Mines Ltd. OGS field party dug pits and collected samples. 1964: OGS staff collected samples. 1970: Amax Exploration Inc. carried out a magnetometer survey.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
2.336 52J02SE8769 52J02SE8769

Geology

Province: Superior

Subprovince: Wabigoon

Belt: Sturgeon Lake

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Syenite 1 Host
Mafic lava flow-unsubdivided 2 Near

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1FluoriteEconomicOre
2MagnetiteEconomicOre
1FeldsparEconomicGangue
2CarbonateEconomicGangue

Mineralization Comments

Apr 29, 2020 (Therese Pettigrew) - An occurrence of higher radioactivity was located on the southwest tip of Coveney Island, Sturgeon Lake. It occurs on the contact zone between the Sturgeon Lake syenite and the altered volcanic country rock. A small pit, 4-5 feet across and about 6 feet deep, has been sunk on a radioactive, highly altered, red-coloured contact phase of the syenite. This is a red feldspar rock containing purple fluorite, minor magnetite, traces of sulphides and an unidentified black mineral. Abundant secondary carbonate occurs in both the volcanic rocks and the syenite. Qualitative spectrographic analysis of a grab sample taken by the author from this pit gave: about 0.05 percent niobium; detectable amounts of thorium, cerium, and lanthanum; and 0.06 percent U3O8 equivalent (Rogers 1964). Four radioactive dykes were located on Coveney Island. The best assays were 0.15% U3O8 and 0.48% ThO2 (radiometric equivalent) and 0.015-0.020% Nb2O5 (radiometric equivalent) (Robertson and Gould, 1983).



Mineral Record Details

References

Map - Sioux Lookout-Armstrong sheet, geological compilation series, Kenora and Thunder Bay districts

Publication Number: M2169 Scale: 1:253,440    Date: 1970

Author: Davies J.C., Pryslak A.P., Pye E.G.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of the Metionga Lake area, districts of Thunder Bay and Kenora

Publication Number: R024 Page: 44  Date: 1997

Author: Rogers D.P.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Uranium and thorium deposits of northern Ontario

Publication Number: MDC025 Page: 126-127  Date: 1984

Author: Robertson J.A., Gould K.L.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Kenora Resident Geologist District Office