Ontario Geological Survey
Permanent Link to this Record:
MDI52E10SW00019
Record Name(s) | Monarch - 1897, Bullion No. 1 - 1897 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1980-Jun-30 |
Date Last Modified | 2022-Feb-18 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Glass
Latitude: 49° 34' 40.44" Longitude: -94° 56' 27.99"
UTM Zone: 15 Easting: 359676.58 Northing: 5493511.28 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52E10SW
Point Location Description: General
Location Method: Conversion from MDI
Access Description: The property consisted of mining locations S105, S106 and S107, with work done primarily on S106. The northern pit is 600 m north of the eastern part of Hell diver Bay, and 1.2 km east-northeast of the Olympia No. l shaft. The area may be reached by boat from Clytie Bay Landing or from Kenora via Ash Rapids.
1897: property was owned by the Bullion Mining Company, who carried out pitting and stripping. 1983: Selco Exploration Inc. conducted mag and HLEM surveys.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.5872 | 52E10SW8584 | 52E10SW8584 |
Province: Superior
Subprovince: Wabigoon
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Basalt | Adjacent |
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Vein | 2 | Contains | ||
Peridotite | 3 | Peridotite Sill | Near |
Jan 28, 2020 (Therese Pettigrew) - Rocks in the vicinity of the workings are predominately fine- to medium-grained, mafic metavolcani c flows. Pillows indicate that the northeast-trending stratigraphy is southeast-facing. A narrow, coarse-grained peridotite sill is located in the central part of the property (Davies and Smith, 1988).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Pyrrhotite | Economic | Ore | ||||
3 | Gold | Economic | Ore |
Jan 28, 2020 (Therese Pettigrew) - Two pits were found in the area of location S106 by Davies and Smith (1988). The north pit and an adjacent trench lie at the southern edge of a 105 degree-trending linear valley. The 1.8 by 2 m pit was sunk an estimated 3 m on a narrow, white, sugary quartz vein trending about 130 degrees and dipping 85 N. The vein locally contains up to 20% pyrite and rare specks of gold. Enclosing basalts contain fine disseminated pyrrhotite; they are fractured but not sheared. A second pit lies 250 m to the south, on the northwestern side of a linear valley which is apparently underlain by peridotite. The 1.8 by 2.4 m pit, now 2.5 m deep, was sunk on a 2 m wide felsite dike which trends 130 degrees and narrows to the northwest. No quartz vein is present but the felsite contains abundant pyrite and a little pyrrhotite, both disseminated and on fine fractures. The pit lies near a weak 115 degree-striking lineament (Davies and Smith, 1988).
MonoMap - Geology of the Shoal Lake-Western Peninsula area, District of Kenora
Publication Number: OFR5242 Scale: Date: 1978
Author: Davies J.C.
Publisher Name: Ontario Geological Survey
Location:
Part - Fourth report on the west Ontario gold region
Publication Number: ARV07-02.001 Scale: Date: 1998
Author: Coleman A.P.
Publisher Name: Ontario Bureau of Mines
Location:
Mono - The geological setting of gold occurrences in the Lake of the Woods area
Publication Number: OFR5695 Scale: Date: 1988
Author: Davies J.C., Smith P.M.
Publisher Name: Ontario Geological Survey
Location:
Mono - Gold deposits of the Kenora-Fort Frances area, districts of Kenora and Rainy River
Publication Number: MDC016 Scale: Date: 1976
Author: Beard R.C., Garratt G.L.
Publisher Name: Ontario Division of Mines
Location:
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