Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52F07NW00003

Record: MDI52F07NW00003

General

Mineral Record Identification
Record Name(s) Swede Boys Island - 1980
Related Record Type Simple
Related Record(s)
Record Status Occurrence
Date Created 1980-Sep-23
Date Last Modified 2022-Aug-05
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Harper Lake Area

Latitude: 49° 23' 29.93"    Longitude: -92° 49' 30.62"

UTM Zone: 15    Easting: 512686.775   Northing: 5471009.354    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52F07NW

Point Location Description: General

Location Method: Conversion from MDI

Access Description: The two islands lying immediately northeast of the peninsula between Reliance and Jackfish Bays of Upper Manitou Lake were formerly referred to as theSwede Boys Islands, though the name is now reserved for the larger of the two islands only. According to Thomson (1933, p.36). (GR 189, p. 61, 62; 1979)



Geology

Province: Superior

Subprovince: Wabigoon

Terrane: Western Wabigoon

Belt: Eagle-Wabigoon-Manitou

Geological Age: Precambrian  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Schist-Unsubdivided 1 Adjacent
Vein 2 Contains

Lithology Comments

Feb 23, 2010 (C Ravnaas) - GRADE: BEST ASSAY - 0.29 OPT AU FROM GRAB. On the larger of these islands (H.P.259) an old shaft is located on a quartz vein, which strikes N. 50 degrees E. and dips 75 degrees S. E. The vein is about 2 feet [0.6 m] wide and may be traced about 15 feet [5 m] to the southwest. There are some old pits along the strike to the northeast, but no vein material can be observed. The wall rock of the vein is chlorite schist carrying a little pyrite. Native gold was observed in the schist. A grab sample of the ore on the dump assayed $8.80 per ton (0.44 0z/t Au) in gold. East of the shaft on the shore of a small bay a stockwork of small quartz stringers and schist occurs across a width of 6 feet [2 m] and may be traced along the shore a short distance. The quartz and schist carry a little sulphides. Another old shaft is located on the smaller island (H.P. 260) to the northeast. It was sunk on a small lens of milky-white quartz in massive agglomerate and tuff. The quartz lens is about 2 feet [0.6 m] in width and may be traced 30 feet [9 m]. It contains a trace of pyrite and chalcopyrite. A grab sample of the material on the dump assayed 80 cents ' in gold per ton. The present writer was unable to locate any of the shafts and pits referred to by Thomson. As of December 1973, Swede Boys Island was held under two patented claims, K3810 and K3811, being parts of mining location HP259. The smaller is land, former mining location HP260, was not held under patent, and is open to staking. (GR 189, p. 61, 62; 1979)




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
5ChalcopyriteEconomicOre
10GoldEconomicOre
15PyriteEconomicOre

Mineralization Comments

Feb 23, 2010 (C Ravnaas) - GRADE: BEST ASSAY - 0.29 OPT AU FROM GRAB. On the larger of these islands (H.P.259) an old shaft is located on a quartz vein, which strikes N. 50 degrees E. and dips 75 degrees S. E. The vein is about 2 feet [0.6 m] wide and may be traced about 15 feet [5 m] to the southwest. There are some old pits along the strike to the northeast, but no vein material can be observed. The wall rock of the vein is chlorite schist carrying a little pyrite. Native gold was observed in the schist. A grab sample of the ore on the dump assayed $8.80 per ton (0.44 0z/t Au) in gold. East of the shaft on the shore of a small bay a stockwork of small quartz stringers and schist occurs across a width of 6 feet [2 m] and may be traced along the shore a short distance. The quartz and schist carry a little sulphides. Another old shaft is located on the smaller island (H.P. 260) to the northeast. It was sunk on a small lens of milky-white quartz in massive agglomerate and tuff. The quartz lens is about 2 feet [0.6 m] in width and may be traced 30 feet [9 m]. It contains a trace of pyrite and chalcopyrite. A grab sample of the material on the dump assayed 80 cents ' in gold per ton. The present writer was unable to locate any of the shafts and pits referred to by Thomson. As of December 1973, Swede Boys Island was held under two patented claims, K3810 and K3811, being parts of mining location HP259. The smaller is land, former mining location HP260, was not held under patent, and is open to staking. (GR 189, p. 61, 62; 1979)



Mineral Record Details

References

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

Publication Number: OFR5731 Page: 143  Date: 1990

Author: Delisle P.C.

Publisher Name: Ontario Geological Survey

Location:


Part - Geology of the Manitou-Stormy lakes area

Publication Number: ARV42-04.001 Page: 36  Date: 1998

Author: Thomson J.E.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Gold deposits of the Kenora-Fort Frances area, districts of Kenora and Rainy River

Publication Number: MDC016 Page: 39  Date: 1976

Author: Beard R.C., Garratt G.L.

Publisher Name: Ontario Division of Mines

Location:


MonoMap - Geology of the Upper Manitou Lake area, District of Kenora

Publication Number: R189 Page: 60-61  Date: 1979

Author: Blackburn C.E.

Publisher Name: Ontario Geological Survey

Location:


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