Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52F09SE00009

Record: MDI52F09SE00009

General

Mineral Record Identification
Record Name(s) Black Fox - 1991
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 1991-Jan-22
Date Last Modified 2022-May-18
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Hodgson

Latitude: 49° 31' 25.19"    Longitude: -92° 5' 46.22"

UTM Zone: 15    Easting: 565412   Northing: 5486064    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52F09SE

Point Location Description: AMIS site location

Location Method: Field Visit



Exploration History

1889: shaft was sunk by Maple Leafe Gold Mining Company. Mid-1980s: several quartz veins were uncovered to test the quality of the silica for quarrying purposes. 1990: J.V. Hamilton carried out prospecting, stripping, and sampling.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
63.5828 / 52F09SE G-1 52F09SE0027 52F09SE0027
63.5827 / 52F09SE P-1 52F09SE0028 52F09SE0028



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Vein 1 quartz Host
Mafic pillowed flow 2
Mafic massive flow 3

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PyrrhotiteEconomicOre
2PyriteEconomicOre
5LimoniteEconomicOre

Mineralization Comments

Mar 31, 2022 (Therese Pettigrew) - The Weekly Herald (January 25, 1890) reported that the company had discovered free milling gold ore from a vein averaging 100 feet wide and extending for over half a mile. The average of different assayers was about $9 a ton (approximately 0.43 oz/t Au). The Black Fox shaft and the three stripped areas located nearby represent part of a massive quartz stockwork system Quartz veins up to 30 feet wide with latticed stringers dominate the outcropping areas. The dominant vein orientation varies between 090 and 120 . The quartz is of the white, milky variety which generally lacks sulphides except for patches where pyrrhotite and minor pyrite is present. Wallrock inclusions are occasionally found in the quartz veins. Wall rock alteration is minimal and indicates a relatively cool intrusion temperature. A strung structural control of the vein system and stockwork is indicated by the orientation of the main veins which are parallel to the early shears. Four samples were taken in the general vicinity of the Black Fox shaft and assayed for gold. These assays all indicate <0.002 oz/T gold for these samples (Assessment report 52F09SE0027).


Mar 31, 2022 (Q Unknown) - BEST ASSAY: 0.5 OPT AU (WEEKLY HERALD 1890).



Mineral Record Details

References

Journal - Daily Sentinel 1891-04-07

Publication Number: Daily Date: 1891

Author:

Publisher Name:

Location: Kenora RGP


Part - Geology of the Dyment area

Publication Number: ARV69-06 Date: 1997

Author: Satterly J.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Property visits by the Dryden area mineral commodity geologist, 1989

Publication Number: OFR5731 Page: 40-41  Date: 1990

Author: Delisle P.C.

Publisher Name: Ontario Geological Survey

Location:


Journal - Weekly Herald 1890-01-25

Publication Number: Herald Date: 1890

Author:

Publisher Name:

Location: Kenora RGP


Book - Weekly Herald 1891-03-07, p. 5

Publication Number: Herald Date: 1891

Author:

Publisher Name:

Location: Kenora RGP


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Ministry Contact Information

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