Ontario Geological Survey
Permanent Link to this Record:
MDI52A03SW00012
| Record Name(s) | Claybar Uranium and Oil - 1958, Jarvis Point - 1935, B.W. Prieston - 1965 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1979-Jul-30 |
| Date Last Modified | 2022-Apr-27 |
| Created By | |
| Revised By |
Primary Commodities: Copper, Nickel
Secondary Commodities: Platinum, Palladium
Township or Area: Spar And Victoria Islands Area, Crooks
Latitude: 48° 6' 40.58" Longitude: -89° 19' 39.38"
UTM Zone: 16 Easting: 326749.87 Northing: 5331288.29 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52A03SW
Point Location Description: Precise
Location Method: Conversion from MDI
1935: discovered by E. Bell, who carried out pitting and prospecting. 1958: Claybar Uranium and Oil Ltd. drilled 3 DDH totalling 195.7 m. 1991: R. Kwiatkowski conducted prospecting.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 11 | 52A04SE0051 | 52A04SE0051 |
| 63.6219 | 52A03SW8101 | 52A03SW8101 |
Province: Southern
Formation Group: Animikie Group
Geological Age: Paleoproterozoic
| Rock Type | Rank | Composition | Texture | Relationship | Norite | 1 | Norite And Diabase Dyke | Host |
|---|
Feb 28, 2018 (Therese Pettigrew) - There are 2 pits, spaced 24.3 m apart, along the south shore of the peninsula. Tanton (1935) reports that Cu-Ni sulphides are also exposed in a small pit 213.4 m along strike to the southwest. The width of mineralized rock exposed is 0.6 m. Mineralization consists of pyrrhotite, chalcopyrite, pentlandite, and pyrite, which occurs as irregular veinlets up to 10 cm wide in a tabular-shaped body of norite. The norite itself is up to 1 m wide and occurs in, and parallels in strike, the diabase dyke. The diabse is lustre mottled (ophitic) and coarser-grained than the norite and is readily distinguished. The mineralized zone can be traced on the surface for 35 m. A 1 m chip sample across the zone, 10.7 m from its east end, in a pit having a diameter of 2.4 m and a depth of 1.2 m, was found by the OGS lab to contain 0.45% Cu, 0.32% Ni, and 0.01 opt Pt and 0.01 opt Pd. A sample taken in 1925 by E.A. Bell and reported to contain 3% Cu and 1.5 % Ni may have been a grab of some of the better mineralized material (Pye, 1965).
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Chalcopyrite | Economic | Ore | ||||
| 2 | Pyrrhotite | Economic | Ore | ||||
| 3 | Pentlandite | Economic | Ore | ||||
| 4 | Pyrite | Economic | Ore |
Mono - Copper, nickel, lead and zinc deposits of Ontario
Publication Number: MDC012 Page: 344 Date: 1969
Author: Shklanka R.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of Crooks Township, Jarvis and Prince locations, and offshore islands, District of Thunder Bay
Publication Number: R102 Page: 36-37 Date: 1973
Author: Geul J.J.C.
Publisher Name: Ontario Division of Mines
Location:
Publication - Copper-Nickel Mineral Occurrences in Pigeon River Area, Ontario; Geological Survey of Canada, Paper no. 35-1
Publication Number: GSC Paper 35-1 Date: 1935
Author: Tanton, T.L.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/101044
Publication - Jarvis Point Location, unpublished report
Publication Number: Unpub Rep Date: 1965
Author: Pye, E.G.
Publisher Name: Ontario Geological Survey
Location: Thunder Bay RGP Office mineral files
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