Ministry of Energy, Northern Development and Mines
Permanent Link to this Record: MDI52E11NE00005Deposit Name(s) | Cash Island - 1898, Island Mh 71 - 1898 |
---|---|
Related Deposit Type | None |
Deposit Status | discretionary occurrence |
Abandoned Mine Inventory Reference | 06396 |
Date Created | 1984-Feb-09 |
Date Last Modified | 2020-May-15 |
Created By | Q Unknown |
Revised By | T Pettigrew |
Primary Commodities: gold
Township or Area: Snowshoe Bay Area
Latitude: 49° 37' 55.77" Longitude: -95° 0' 7.29"
UTM Zone: 15 Easting: 355434 Northing: 5499658 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52E11NE
Point Location Description: Precise
Location Method: conversion from mdi
Source Map: OGS 1982, MAP 2422 BAG BAY
Sources Map Scale: 1:25 000
Access Description: Island MH 71 is near the north part of Shoal Lake, about 3.5 km west-northwest of Clytie Bay Landing. It is accessible by boat from Clytie Bay.
1898: Trenching and shaft sinking by persons unknown. No assessment reports were found over the area.
Province: Superior
Subprovince: Wabigoon
Geological Age: Archean
05/15/2020 (T Pettigrew) - The volcanic stratigraphy in the Shoal Lake area strikes northeast and has been subdivided into a lower mafic assemblage, a lower felsic assemblage and an upper mafic assemblage (Davies, 1978). In the northern part of Shoal Lake, the volcanics face northwest, although the felsic volcanics have been strongly sheared and there is some evidence for folding within them. The lower part of the upper mafic assemblage includes medium-grained sills or thick flows and in this respect resembles the lower mafic assemblage, but it also includes more pillow breccia and some interlayered intermediate volcanics and sediments (Davies and Smith, 1988).
Rock Type | Rank | Composition | Texture | Relationship |
---|---|---|---|---|
mafic metavolcanics | 1 | basalt | sheared | |
vein | 2 | quartz |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Habit Description |
---|---|---|---|---|---|---|---|
1 | pyrite | economic | ore | ||||
2 | pyrrhotite | economic | ore | ||||
1 | quartz | economic | gangue | ||||
2 | carbonate | economic | gangue |
05/15/2020 (T Pettigrew) - On Island MH 71, approximately 400 m above the base of the upper volcanic assemblage, sheared basalt lies to the northwest of a mafic sill. The basalt contains irregular veins and veinlets of quartz, which are in part oblique to the northeast-striking foliation. Locally there is abundant carbonate and up to 10% pyrite. The coarser rock contains much fine pyrrhotite near the northwest shore of the island. A cherty dyke containing minor pyrite occurs along the north-central shore; nearby are several pits and trenches and a shaft (Davies, 1978). A shaft was sunk to an estimated depth of 9 m on one vein, which is 30 to 40 cm wide, strikes 020 degrees and dips 75 E. The vein is sugary, white, and contains <1% pyrite; it also crops out in trenches 10 m and 20 m to the southwest of the shaft. Some 30 m to the east-northeast, another trench exposes a second quartz vein about 15 cm wide. A chip sample, taken in this study across 35 cm of the quartz vein in the shaft, contained 270 ppm gold (Davies and Smith, 1988).
Publication - Gold Deposits of the Kenora-Fort Frances Area, p. 22
Publication Number: MDC016 Date: 1976
Author: Garratt, G.L., Beard, R.C.
Publisher Name: OGS
Publication - Geology of the Shoal Lake-Western Peninsula Area, p. 64-65, 85-86
Publication Number: OFR5242 Date: 1978
Author: Davies, J.C.
Publisher Name: OGS
Publication - The Geological Setting of Gold Occurrences in the Lake of the Woods Area, p. 178-179
Publication Number: OFR5695 Date: 1988
Author: Davies, J.C., Smith, P.M.
Publisher Name: OGS
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