Ontario Geological Survey
Permanent Link to this Record:
MDI31M05NE00047
Record Name(s) | Kerr Lake Mine - 1905, Glen Lake Silver Mines Ltd. - 1940, Kerr Lake Lease (HiHo Silver Mines) - 1948 |
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Related Record Type | Partial |
Related Record(s) | |
Record Status | Past Producing Mine Without Reserves or Resources |
Date Created | 1984-Nov-02 |
Date Last Modified | 2023-Aug-24 |
Created By | |
Revised By |
Primary Commodities: Silver, Cobalt
Secondary Commodities: Copper, Nickel
Township or Area: Coleman
Latitude: 47° 22' 32.09" Longitude: -79° 39' 24.57"
UTM Zone: 17 Easting: 601397 Northing: 5247777 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 31M05NE
Point Location Description: Shaft
Location Method: AMIS Site Visit
Access Description: From hwy 11b, turn southeast following Coleman Rd which continues into Kerr Lake Rd (mileage 3.4km). Continue on Kerr Lake Rd for 0.5km to property boundary, approximately 200m east of Penn Mill/University Rd turnoff.
1904: silver vein discovered on shore of Kerr Lake. 1905-1939: Kerr Lake Mining Co. Ltd - 13 shafts and development work, in production. 1940-1948: Glen Lake Silver Mines Ltd. - in production. 1953-1956: Cobalt Consolidated Mining Corporation Ltd . - production from Kerr Lake and Crown Reserve properties
Province: Southern
Subprovince: Cobalt Basin
Supergroup: Huronian Supergroup
Formation Group: Cobalt Group
Geological Age: Paleoproterozoic
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Calcite | Host |
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Quartz Diabase | 2 | Quartz Diabase | Contains | |
Conglomerate | 3 | Conglomerate | Hanging Wall |
Feb 12, 2015 (A Wilson) - The southerly-dipping north limb of the New Lake Diabase basin is exposed at surface in the south part of claim No.336; the axis of the arch (usually referred to as the Kerr Lake arch) between this and the Peterson Lake Diabase basin is in the vicinity of the north line of this claim and trends a little north of east. The lower contact of the diabase on claim No.336 rests for the most part on Keewatin rocks: the Cobalt series - Keewatin contact dips northerly and the bottom diabase contact southerly. This diabase contact has irregularities both in section and plan; as shown by Knight on a north-south section along the east boundary of the property the dips over much of its length are from 10 to 20°. but at several places they are nearly vertical, constituting "rolls". This map also shows that the general dip from surface to the south boundary of the claim is appreciably steeper than south of this boundary The Cobalt Series sediments exposed at surface are for the most part conglomerate or grit - the basal member of the series. In addition to very local irregularities in the lower contact of the Cobalt series the presence of two trough-like depressions in this contact has been pointed out by Knight; he regarded the depression as being due to pre-Huronian erosion. The axes of these depressions trend northerly - one is situated near the east line of the property the other near the west Iine. It will be noted that the series extends very little south of its contact at surface with the overlying Nipissing diabase. The Cobalt series - Keewatin contact in the south part of the area covered by the series approaches a horizontal (approximately 5°N. dip) attitude in contrast with a dip of 20 N 0 in the north part. The Keewatin is not exposed at surface on this property. In the western part it is made up of andesitic lavas with interflow cherty sedimentary bands. Knight showed such a 25-foot wide chert band with irregular northerly strike in the northwest corner of the claims. On the 140-foot level of shaft No 0 13, in the west central part of the property, a band of chert is exposed about 30 feet south of the shaft. The cherty sediments near shaft No,13 are in places black and carbonaceous. The bedded cherty sediments with nearly vertical dips described by Knight as occurring at the northeast and southeast corners of the property are regarded by the present writer as part of the Keewatin sediments which are exposed at surface on the Drummond claim, adjoining to the east. The position and nature of the contact or transition zone between the predominantly lava assemblage to the west and the predominantly cherty sediments to the east is not known.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Silver | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Gangue | ||||
4 | Pyrrhotite | Economic | Gangue | ||||
5 | Galena | Economic | Gangue | ||||
6 | Sphalerite | Economic | Gangue |
Feb 12, 2015 (A Wilson) - A large number of productive veins were mined on this property; of 36 listed by Knight, No.10, No.3, Fleming, No 7, Big Chamber, Main East and McDonald are given in order of productivity as the most important ones. Silver amounting to 3,345,233 oz, is reported to have been won from the No,10 vein between Aug 31, 1910 and Aug. 31, 1921 and 867,401 oz. from the McDonald vein over the same period. A large part of the total production was obtained from a small portion (near the northern line) of the claim. Most of the veins including the No.10, Fleming, Big Chamber and Main East, in this portion constitute a vein group, which trends at about N 070 ° E. The veins in the group have strikes sub-parallel to the trend of the group and branch and rejoin in a complicated pattern. The strike of the veins in the group is approximately parallel to that of the Cobalt Series sediments; the dip, where intersecting these, is steeply to the south and approximately at right angles to the dip of the sediments as is apparent from a view of the open cuts at surface. The grade of the silver extracted from the mine between 1905 and 1916 was170 oz/t Ag
Rank | Classification |
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1 | Vein (Cobalt-Type) |
Rank | Characteristic |
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2 | Stratabound |
1 | Vein |
Year | Tonnes | Commodities | Reference | Comment |
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1956 | 10 | PR 1961-06 p.49 | total production 1953-1956, combined production from Kerr Lake and Crown Reserve properties | |
1948 | 327 | MDC010, p. 141 | total production 1940-1948 | |
1939 | 213318 |
Silver 886512447 Cobalt 295143 Copper 814 |
MDC010, p.140-141 | total production 1905-1939 |
File - Resident Geologist file CO-0692
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Map - Cobalt silver area, southeastern sheet, Timiskaming District
Publication Number: M2052 Scale: 1:12,000 Date: 1997
Author: Thomson R.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Kerr Lake and Hargrave mines, showing plans of mine levels, Cobalt, District of Timiskaming, Ontario
Publication Number: ARM31A-03 Scale: 1:3,000 Date: 1997
Author: Knight C.W.
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: 87-92 Date: 1998
Author: Knight C.W.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Preliminary report on parts of Coleman Township, concession 4, lots 1 to 5, and Gillies Limit, the eastern "A" claims, District of Timiskaming
Publication Number: PR1961-06 Page: 45-50 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, 140-141 Date: 1968
Author: Sergiades A.O.
Publisher Name: Ontario Dept. of Mines
Location:
Article - 1979 report of the Kirkland Lake Resident Geologist
Publication Number: MP091.006 Page: 81 Date: 1997
Author: Lovell H.L., Ploeger F.R.
Publisher Name: Ontario Geological Survey
Location:
Book - Agnico Eagle, Canadaka File (Company File)
Publication Number: Date: 1976
Author:
Publisher Name:
Location: Kirkland Lake RGP office
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