Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31D15SE00097

Record: MDI31D15SE00097

General

Mineral Record Identification
Record Name(s) Simmons Occurrence (North Group) - 1957
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

Commodities

Primary Commodities: Copper



Location

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.



Exploration History

1957:M.A. Winkler – prospecting, pitting, ground magnetometer survey


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
63.964 31D16NW0053 31D16NW0053

Geology

Province: Grenville

Geological Age: Mesoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Gneiss-Unsubdivided 1 Granitic Host

Lithology Comments

Jan 06, 2017 (A Wilson) - The showing is contained in gneiss of the Kinmount Lithodeme, Glamorgan Gneiss Complex.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1ChalcopyriteEconomicOre
2PyrrhotiteEconomicOre

Mineralization Comments

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.



Mineral Record Details

Characteristics
Rank Characteristic            
1 Disseminated

References

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