Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42C02SW00004

Record: MDI42C02SW00004

General

Mineral Record Identification
Record Name(s) George W. Macleod Mine - 1960, Helen Iron Range - 1899
Related Record Type Compound
Related Record(s)
Record Status Past Producing Mine With Reserves or Resources
Date Created 1982-Sep-30
Date Last Modified 2022-Oct-20
Created By
Revised By

Commodities

Primary Commodities: Iron



Location

Township or Area: McMurray

Latitude: 48° 0' 58.14"    Longitude: -84° 45' 38.72"

UTM Zone: 16    Easting: 666980.96   Northing: 5320521.4    UTM Datum: NAD83

Resident Geologist District: Sault Ste. Marie

NTS Grid: 42C02SW

Point Location Description: Former head frame on patented claim DJ 62 M 778

Location Method: Conversion from MDI

Access Description: Access to the mine site is now by permission only. By prior arrangement with Algoma Steel Company the mine site is accessible via the old sintering plant site. Drive northeast from the sintering plant site for approximately 2.5 km to the top of Helen Mine hill. The fenced and reclaimed mine site is on the top of the hill overlooking the town of Wawa.



Exploration History

Multiple ore zones of the Helen Iron Range have operated at different times under a variety of names by the Algoma Steel Corporation and affiliated companies. 1953: Algoma Ore Properties - No. 5 shaft started and reaches 283 (eventually the Macleod production shaft), surface diamond drilling. 1954: Algoma Ore Properties - No. 5 shaft to 1895 feet, 1800 foot long inclined tramway driven and tied to aerial tramway. 1955: Algoma Ore Properties - No. 5 shaft to 2066 feet, tramway extended to 4410 feet. 1956: Algoma Ore Properties - construction of new sintering plant. 1957-59: Algoma Ore Properties - underground tramway extended to 4877 feet, surface diamond drilling. 1960: Algoma Ore Properties - production from old Helen ore body ceases, production from G. W. Macleod Mine begins. 1998: G. W. Macleod Mine closes and mine rehabilitation begins.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
CHABANEL 23 42C02SE8874 42C02SE8874
Lendrum-0017 42C02SE0070 42C02SE0070
McMurray-0011-A1 42C02SW9030 42C02SW9030

Geology

Province: Superior

Subprovince: Wawa

Terrane: Wawa-Abitibi

Belt: Michipicoten

Tectonic Assemblage: Wawa

Geological Age: Neoarchean   Geochronological Age: 2750 MA   Geochron. Age Ref.: OFR 5888W

Metamorphism Type: Regional

Metamorphism Grade: Greenschist



Geology Comments

Dec 07, 2005 (A Wilson) - The Helen Iron Range is one of 32 separate iron ranges that make up the Michipicoten Iron Formation. This iron formation caps the 2750 Ma volcanic cycle in the Wawa area and represents a period of considerable chemical and clastic sedimentation. The iron range is terminated by the Talbot lake Fault at the west end and the Wallbank lake Fault at the east. The great thickness of the iron formation at its west end is due to tectonic activity along the Talbot Lake Fault which thickened the iron formation by drag folding.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Carbonate Ironstone 1 Carbonate Facies Host
Felsic Tuff 2 Rhyolite To Andesite Tuff Footwall
Mafic lava flow-unsubdivided 3 Basalt Pillowed, Massive Hanging Wall

Lithology Comments

Dec 07, 2005 (A Wilson) - All five facies are developed in this iron formation, however, all mining at the Macleod Mine has taken place in the carbonate (siderite) facies. A chert horizon lies between the siderite and the footwall volcanic rocks. This unit is not observed in any of the other iron ranges. Some chert and argillite has also been reported at the base of the carbonate facies. Their presence may be due to tectonic activity along the Talbot Fault.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1SideriteEconomicOre
1PyriteEconomicGangue
2PyrrhotiteEconomicGangue
3GalenaEconomicGangue

Mineralization Comments

Dec 07, 2005 (A Wilson) - Although iron has been the chief mineral of economic importance in the deposit, galena occurs as fracture fillings in pyrite-bearing siderite on the M3 level of the mine. A specimen of this material yielded 31.2% Pb and 144 ppm Ag.



Mineral Record Details

Classification
RankClassification            
1 Sedimentary
Characteristics
Rank Characteristic            
1 Massive

Mineral Zones - Size and Shape

Rank: 1       Structure Type: Contact

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Irregular 2500 150 60 60 2750 MA OFR 5888
Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
G. W. MacLeod Mine 1998 Unclassified 18700000 OFR 5990 Iron 31 NA
Production Data
Year Tonnes Commodities Reference Comment
1998 59662710 Iron 31

References

File - Resident Geologist files Lendrum-0018-A1

Publication Number: Date:

Author:

Publisher Name:

Location: SSM RGP office


Map - Geological series, McMurray Township and parts of surrounding townships, formerly Township 29, Range 23, District of Algoma

Publication Number: P0828 Scale: 1:15,840    Date: 1973

Author: Rupert R.J.

Publisher Name: Ontario Division of Mines

Location:


Map - Geological series, Precambrian geology of McMurray Township, Wawa area, Algoma District

Publication Number: P2441 Scale: 1:15,840    Date: 1982

Author: Sage R.P., Sawitzky E., Turner J., Leeselleur P., Sagle E.

Publisher Name: Ontario Geological Survey

Location:


Map - Precambrian Geology, Michipicoten Greenstone Belt, Central Portion

Publication Number: P3303 Scale: 1:50,000    Date: 1994

Author: Sage R.P.

Publisher Name: Ontario Geological Survey

Location:


Part - Iron deposits in the District of Algoma

Publication Number: ARV55-04.001 Page: 87-118  Date: 1997

Author: Moore E.S., Armstrong H.S.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Iron deposits of Ontario

Publication Number: MDC011 Page: 65-66  Date: 1968

Author: Shklanka R.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Wawa mineral deposits data base

Publication Number: OFR5775 Page: 277  Date: 1991

Author: Frey E.D., Stewart R.C.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Geology of Chabanel, Esquega, Lastheels and McMurray Townships, District of Algoma

Publication Number: OFR5586 Page: 381-385  Date: 1993

Author: Sage R.P.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Geology of Michipicoten Greenstone Belt

Publication Number: OFR5888 Page: 54-69  Date: 1994

Author: Sage R.P.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Geology of McMurray Township and parts of surrounding townships, District of Algoma

Publication Number: OFR5283 Page: 56-62  Date: 1979

Author: Rupert R.J.

Publisher Name: Ontario Geological Survey

Location:


Book - McMurray Township - unpublished GDIF

Publication Number: GDIF Date: 1985

Author: Resident Geologist Staff

Publisher Name:

Location: Timmins RGP


Report an Error

We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.


Terms of Use

Please review our Terms of Use agreement for this data product.


Ministry Contact Information

For detailed information regarding this mineral record please contact the Sault Ste. Marie Resident Geologist District Office