Ontario Geological Survey
Permanent Link to this Record:
MDI31D15SE00097
Record Name(s) | Simmons Occurrence (North Group) - 1957 |
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Related Record Type | Simple |
Record Status | Occurrence |
Date Created | 1982-Jan-18 |
Date Last Modified | 2022-Jan-05 |
Created By | Q Unknown |
Revised By | A Wilson |
Primary Commodities: Copper
Township or Area: Snowdon
Latitude: 44° 51' .38" Longitude: -78° 40' 13.97"
UTM Zone: 17 Easting: 684075 Northing: 4968939 UTM Datum: NAD83
Resident Geologist District: Southern Ontario
NTS Grid: 31D15SE
Point Location Description: General
Location Method: Data Compilation
Access Description: 150 m north of Hwy 519 and Kendrick Cr.
1957:M.A. Winkler – prospecting, pitting, ground magnetometer survey
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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63.964 | 31D16NW0053 | 31D16NW0053 |
Province: Grenville
Geological Age: Mesoproterozoic
Rock Type | Rank | Composition | Texture | Relationship | Gneiss-Unsubdivided | 1 | Granitic | Host |
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Jan 06, 2017 (A Wilson) - The showing is contained in gneiss of the Kinmount Lithodeme, Glamorgan Gneiss Complex.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Ore | ||||
2 | Pyrrhotite | Economic | Ore |
Jan 06, 2017 (A Wilson) - Recent prospecting on the property has disclosed a mineralized zone on Claim KO 24997 where, in two test pits about 125 feet apart, considerable sulphide mineralization - consisting essentially of chalcopyrite with a narrow band of massive pyrrhotite, has been opened up. The main pit, which is an open cut on the hill, discloses mineralization over an approximate length of 20 feet and a width of 5 to 6 feet. The east wail of the zone consisted of pegmatite and granite. The west wall was not exposed on the downside of the hill. The sulphides probably occur in paragneiss. It is estimated that the zone would run about 3% copper over the exposed widths in the open cut. Bands of massive sulphides, a few inches wide, would assay much higher. The pyrrhotite was not nickeliferous, according to field tests.
Jan 06, 2017 (D Laidlaw) - Up to 3% Cuis reported in sample. The evidence of massive chalcopyrite mineralization and the probability that the zone continues for at least 800 feet is sufficiently important to warrant a thorough test of the property.
Rank | Characteristic |
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1 | Disseminated |
MonoMap - Geology of the Howland area, Haliburton, Peterborough and Victoria counties
Publication Number: OFR5639 Scale: Date: 1987
Author: Easton R.M.
Publisher Name: Ontario Geological Survey
Map - Haliburton-Bancroft area, Province of Ontario
Publication Number: M1957B Scale: 1:126,720 Date: 1997
Author: Satterly J., Hewitt D.F.
Publisher Name: Ontario Dept. of Mines
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