Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31M05NE00080

Record: MDI31M05NE00080

General

Mineral Record Identification
Record Name(s) Nipissing 400 - 1904, Nipissing 400 W1/2-401 Parcel 2 - 1902, Nipissing Mining Company Ltd. - 1922, Nipissing O'Brien - 1952, Agnico Mines Ltd. - 1958, Silver Regent Mines Ltd. - 1967
Related Record Type Partial
Related Record(s)
Record Status Past Producing Mine Without Reserves or Resources
Date Created 1980-Oct-22
Date Last Modified 2023-Aug-24
Created By
Revised By

Commodities

Primary Commodities: Silver, Cobalt



Location

Township or Area: Coleman

Latitude: 47° 24' 3.11"    Longitude: -79° 41' 3.24"

UTM Zone: 17    Easting: 599280.65   Northing: 5250551.51    UTM Datum: NAD83

Resident Geologist District: Kirkland Lake

NTS Grid: 31M05NE

Point Location Description: Shaft

Location Method: Data Compilation



Exploration History

1904-1932: Nipissing Mines Company Ltd. – 5 shafts; extensive numbers of drifts and cross cuts; in production. 1967-68: Shaft No. 73 was dewatered and some drifting was carried out. Drifting was carried out along the new No.101 Vein where assays of 3790 oz./t silver over 1½ inches were encountered. Leaf and ruby silver extend to 2 feet on either side of the vein.


Geology

Province: Southern

Subprovince: Cobalt Basin

Supergroup: Huronian Supergroup

Formation Group: Cobalt Group

Geological Age: Paleoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Sandstone 1 Hanging Wall
Diabase 2 Nipissing Diabase Hanging Wall

Lithology Comments

Jul 25, 2017 (A Wilson) - Subhorizontal Cobalt sediments increase in thickness from 150 ft. to 600 ft. southeasterly and overlie steeply dipping Keewatin volcanics. Nipissing diabase formerly overlie the sediments. Two pre-ore fault systems occur; e.g. the reverse Valley Fault that strikes NNE with low dip east, and the normal Fault 64 that strikes ESE with steep dip south. Veins tend to strike parallel to Keewatin volcanic beds which follow a broad fold; they occur in both volcanics and overlying Cobalt sediments but with rich silver ore-shoots restricted to the later within 150 ft. above the conformity. Silver mineralization also occurred in wall rocks.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1SilverEconomicGangue

Mineral Record Details

Production Data
Year Tonnes Commodities Reference Comment
1932 1 Silver
MDC010, p.162-163 Production :Vein No. 73 -13,000,000 ounces; Vein No. 98- 4,000,000 ounces; Vein No. 64 probably well over 10,000,000 ounces; Vein No. 490 probably several million ounces

References

File - Resident Geologist file CO-0723

Publication Number: Date:

Author:

Publisher Name:

Location: Kirkland Lake RGP office


Map - Cobalt silver area, northern sheet, Timiskaming District

Publication Number: M2050 Scale: 1:12,000    Date: 1997

Author: Thomson R.

Publisher Name: Ontario Dept. of Mines

Location:


Part - Geology of the mine workings of Cobalt and South Lorrain silver areas

Publication Number: ARV31-02.001 Page: 46-57  Date: 1998

Author: Knight C.W.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Preliminary report on part of Coleman Township, concession 6, lots 1 to 6, District of Timiskaming

Publication Number: PR1961-03 Date: 1998

Author: Thomson R.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Silver cobalt calcite vein deposits of Ontario

Publication Number: MDC010 Page: 84-86, 162-163  Date: 1968

Author: Sergiades A.O.

Publisher Name: Ontario Dept. of Mines

Location:


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