Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42D14SW00026

Record: MDI42D14SW00026

General

Mineral Record Identification
Record Name(s) Worthington Bay No. 2 - 1936, Rhyolite Zone - 1936, Yellow Rhyolite Zone - 1936, North Shores Gold Mine - 1922, Worthington Bay Base Metal - 1984
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 1991-Apr-01
Date Last Modified 2022-May-06
Created By
Revised By

Commodities

Primary Commodities: Zinc, Silver, Lead



Location

Township or Area: Priske

Latitude: 48° 45' 58.17"    Longitude: -87° 15' 46.9"

UTM Zone: 16    Easting: 480671.66   Northing: 5401494.72    UTM Datum: NAD83

Resident Geologist District: Thunder Bay South

NTS Grid: 42D14SW

Point Location Description: 5 diamond drill holes.

Location Method: Conversion from MDI

Access Description: The occurrence is located in Priske Township on the western shore of Worthington Bay, about 4 km south of Schreiber. It lies approximately 300 m south of the old mill site of the North Shores Gold Mine (Mining Location No. 2, claim map G-631, Priske Township). Access may be gained from Lake Superior or by using an old road which extends south from the old Schrieber dump (Worthington Bay Road) to the mill site of the North Shores Gold Mine, 300 m north of the occurrence.



Exploration History

Circa 1922: A 'silver vein' was noted by P.E. Hopkins on the shore of Lake Superior, 1.6 km south of the Longworth Silver Vein. 1936: In conjunction with ongoing development and exploration at the North Shores Gold Mine, plans were made to further investigate an extensive rhyolite unit which carried interesting gold values. 1937: Five shallow diamond drill holes were drilled on a brecciated, mineralized section of the rhyolite zone, intersecting massive sulphide sections and encouraging silver veins (aggregate length unknown). Circa 1969: C.S. Downey rediscovered the occurrence. 1969: M.W. Bartley inspected the occurrence and prepared a report for G.W. Phelps. 1981: M.W. Carter of the Ontario Geological Survey located and examined the occurrence during field mapping. 1997: Cyprus Canada Inc. conducted prospecting, sampling, and magnetic and VLF-EM geophysical surveys.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
2.17976 42D14SE2001 42D14SE2001
2.17860 42D14SE0104 42D14SE0104

Geology

Province: Superior

Subprovince: Wawa

Terrane: Wawa-Abitibi

Belt: Schreiber-Hemlo

Geological Age: Archean  



Geology Comments

Dec 07, 2005 (B Nelson) - The occurrence is first described in The Canadian Mining Journal (1923, p.107): On the shore of Lake Superior one mile south of the Longworth silver vein and in the strike of it is a highly altered Keewatin rhyolite carrying galena and a little silver. (Resident Geologist's Files, Schreiber Hemlo District, Thunder Bay) The Rhyolite zone is described in a 1936 North Shores Gold Mines Ltd. prospectus: ...averaging 40 feet in width and traced for a distance of approximately 3000 feet. Where sampled, this zone carries interesting gold values. The most complete and recent description of the base metal occurrence is that of *Bartley (1969): Mr. C.S. Downey of Schreiber, Ontario, (re) discovered a narrow occurrence of argentiferous galena and sphalerite in a yellowish rhyolitic formation at the water's edge of Worthington Bay. The yellowish rhyolite is distinctive and appears to be the only host for the sulphide mineralization. Whether it is a dyke or flow within a brecciated rhyolite complex is not known. Where exposed, the sulphide mineralization has a maximum width of ten inches and is composed of very narrow stringers of massive sulphides separated by apparently barren rock. The mineralization has not been traced along strike successfully. Five shallow diamond drill holes were sunk on the occurrence to determine continuity and dimensions. Because of extreme brecciation core recovery was less than 60%. The only intersection of massive sulphides occur near the collar of drill hole #1. The sections where core was not recovered may represent mineralized zones but this is conjectural.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Felsic lava flow-unsubdivided 1 Rhyolite Brecciated Host
Syenite 2 Adjacent
Mafic lava flow-unsubdivided 3 Adjacent

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1GalenaEconomicOre
2PyriteEconomicOre
3SphaleriteEconomicOre

Mineralization Comments

Dec 07, 2005 (B Nelson) - *Bartley (1969) noted the presence of sphalerite and argentiferous galena. Carter (1981a) has listed pyrite as the predominant sulphide mineral. *Bartley (1969) examined old records and concluded: Assays of sludge samples and some core sections returned low values, well below ore grade. The unsampled core, with the exception of the narrow section in Hole #1, is characteristically barren. Sporadic dissemination of fine sulphide mineralization were noted in the remaining core but the quantity is insufficient to be classed as ore material. The argentiferous galena with sphalerite occurrence on the shore of Worthington Bay is not attractive in itself because of the very limited width and accompanying low values. (Resident Geologist's Files, Schreiber Hemlo District, Thunder Bay).



Alteration Comments

Dec 07, 2005 (B Nelson) - Not known.




Mineral Record Details

References

File - Schreiber-Hemlo Resident Geologist Mineral Deposit Files, Thunder Bay office

Publication Number: Min Dep Date:

Author:

Publisher Name:

Location: Thunder Bay RGP


Map - Nipigon-Schreiber, geological compilation series, Thunder Bay District

Publication Number: M2232 Scale: 1:253,440    Date: 1973

Author: Carter M.W., McIlwaine W.H., Wisbey P.A.

Publisher Name: Ontario Division of Mines

Location:


Mono - Mineral Occurrences in the Nipigon-Marathon Area, Volumes 1 and 2.

Publication Number: OFR5951 Page: 524-527  Date: 1996

Author: Schnieders B.R., Smyk M.C., Speed A.A., McKay D.B.

Publisher Name: Ontario Geological Survey

Location:


Compend - Report of activities, 1983, Regional and Resident Geologists

Publication Number: MP117 Page: 91  Date: 1984

Author: Kustra C.R.

Publisher Name: Ontario Geological Survey

Location:


Map - Schreiber-Duck Lake area, District of Thunder Bay

Publication Number: ARM30A Scale: 1:63,360    Date: 1998

Author: Hopkins P.E., Tanton T.L.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Schreiber area, District of Thunder Bay, Ontario

Publication Number: ARM47J Scale: 1:31,680    Date: 1997

Author: Bartley M.W., Harcourt G.A.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Geological series, Precambrian geology of the Schreiber area, east part, Thunder Bay District

Publication Number: P2391 Scale: 1:15,840    Date: 1981

Author: Carter M.W.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Thunder Bay South Resident Geologist District Office