Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31D09NW00008

Record: MDI31D09NW00008

General

Mineral Record Identification
Record Name(s) Goshawk Mines Ltd. - 1989, Mississagua Lake Deposit - 1989, H.G.Greene Vermiculite Deposit - 1950, Regis Resources Ltd. - 2004, Vermiculite Corp. of Canada - 2004, Newlund Mines - 1969
Related Record Type Simple
Related Record(s)
Record Status Past Producing Mine Without Reserves or Resources
Date Created 1982-Sep-09
Date Last Modified 2023-Mar-22
Created By
Revised By

Commodities

Primary Commodities: Vermiculite, Mica



Location

Township or Area: Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish, Cavendish

Latitude: 44° 42' 15.3"    Longitude: -78° 18' 19"

UTM Zone: 17    Easting: 713476   Northing: 4953630    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31D09NW

Point Location Description: General

Location Method: Data Compilation

Access Description: The property is located approximately 56 km north of Peterborough. Highway 507 provides the main access to within 3 km of the west boundary of theproperty. A series of cottage roads bisect the claim group.



Exploration History

1950-69 : H.G. Greene; carried out an extensive programme of test pitting (2-4 ft deep) and held 39 claims in 1962.; DD-2-453 ft. 1976 ? : the property was probably acquired from Ruth Greene by Kebrew Holdings Inc. 1973-74 : Globes Minerals Inc. leased the ground and conducted limited auger and diamond drilling. 1975-77 :Goshawk Mines Ltd. (later, 1977, Insulite Development Corp.- auger sampling, diamond drilling and soil sampling and cut a large trench from which 2 bulk samples were taken. These were shipped to Vermiculite of Canada and the Ontario Research Foundation. 1992-1993: A. Archibald: till sampling, drilling, ground geophysics, linecutting, VLF-EM survey 2001-2003; Regis Resources Inc. announced the commencement of production. Adjustments made to plant with upgrading of operation with a large rotary dryer. Additional bulk sampling completed. First full level of commercial production will be reached by March 2004. The plant operated 24 hr/day, 3 days/week and employed a full time staff of 9.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
Cavendish #61/Goshawk Mines Ltd/2.2210 31D09SW9538 31D09SW9538
Cavendish #62/Goshawk Mines Ltd/63.3429 31D09NW8541 31D09NW8541
Cavendish #66/Goshawk Mines Ltd/ 63.3464 31D09NW8540 31D09NW8540
Cavendish #93/A. Archibald/ OP92-236 31D09NW0009 31D09NW0009
Cavendish #94/A. Archibald/ 2.15539 31D09NW0014 31D09NW0014
Cavendish #95/A. Archibald/ 2.15556 31D09NW0010 31D09NW0010
Cavendish #96/A. Archibald/ 2.15558 31D09NW0007 31D09NW0007
Cavendish #97/A. Archibald/ 2.15557 31D09NW0011 31D09NW0011
Cavendish #100/C.W. Archibald/ OP92-265 31D09NW0011 31D09NW0011
Cavendish #104/C.W. Archibald/ OP93-143, 144, 417 31D16SW0013 31D16SW0013
Cavendish #105/F.T Archibald/ OP92-236 31D09NW0013 31D09NW0013
Cavendish #122/Regis Resources Inc./2.23831 31D09NW2016 31D09NW2016
Cavendish #125/Regis Resources Inc./beneficiation/ 31D09NW2021 31D09NW2021
Cavendish #129/Regis Resources Inc/ 2.26015 31D09NW2024 31D09NW2024

Geology

Province: Grenville

Subprovince: Central Metasedimentary Belt

Terrane: Bancroft

Geological Age: Mesoproterozoic  



Geology Comments

Dec 07, 2005 (C Papertzian) - Vermiculite occurs in marble, the largest concentrations near surface, near the SW corner of the Anstruther Granite. Flakes are generally < 1/8 inch, but up to 1/2 inch, amber-green-black-silver. Zone A covers an area 457 m (1,500 ft) x 122 m (400 ft) on the E side of the property and is estimated to contain a minimum of 49,400 tonnes of exfoliated vermiculite, averaging 11.9 % . Zone B consists of 4 separate bodies over 2,000 ft and zone C (at the W end) appears to be of fairly good grade.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Marble 1 Silicified Host
Schist-Unsubdivided 2 Biotite Host

Lithology Comments

Jan 13, 2017 (A Wilson) - "The claim group is mainly underlain by Grenville limestone which has been altered to a marble. Areas can be seen in this marble with disseminated flakes of amber mica which has been altered to vermiculite. In some areas, the vermiculite is heavily concentrated in a mica schist, locally striking approximately east-west. On the south part of the claim group is the Anstruther granite batholith in the form of granite gneiss. Bordering this mass is a band of dark paragneiss which has been altered to biotite schist and amphibolite. In areas of vermiculite-rich limestone, the tops of the ridges generally appear to be capped by harder, vermiculite-poor limestone which has protected the softer vermiculite-rich limestone from erosion. A few localized outcrops show an estimated ten to thirty percent vermiculite. Vermiculite is prevalent in the top soil over large areas and these areas are in many places underlain by vermiculitized limestones". The vermiculite occurs in a band of crystalline limestone that is exposed for about 100 yards on both sides of the road at the point where the road crosses the boundary between lots 13 and 14, con. 2. The limestone band, which is approximately 250 feet wide, strikes northwest and dips steeply southwest. It is flanked on either side by granitic gneisses.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1VermiculiteEconomicOre
2PhlogopiteEconomicOre
3BiotiteEconomicOre

Mineralization Comments

Jan 13, 2017 (A Wilson) - Vermiculite occurs in marble, the largest concentrations near surface, near the SW corner of the Anstruther Granite. Flakes are generally < 1/8 inch, but up to 1/2 inch, amber-green-black-silver. Zone A covers an area 457 m (1,500 ft) x 122 m (400 ft) on the east side of the property and is estimated to contain a minimum of 49,400 tonnes of exfoliated vermiculite, averaging 11.9 % . Zone B consists of 4 separate bodies over 2,000 ft and zone C (at the west end) appears to be of fairly good grade. The vermiculite was found to be too fine for insulation but might be used as an additive in plaster or concrete. Augering and diamond drilling indicated that the largest concentration of vermiculite lies in the free state near surface. Zone A covers an area 457 m long by 122 m wide on the east side of the property. Zone B consists of four separate bodies over a strike length of 610 m. Zone C is located at the west end of the property and appears to be fairly good grade vermiculite.



Mineral Record Details

Production Data
Year Tonnes Commodities Reference Comment
1989 49400 grading 11.9% exfoliated vermiculite

References

File - Resident Geologist files Cavendish #60, 62, 70 - Goshawk Mines Ltd

Publication Number: Date:

Author:

Publisher Name:

Location: Tweed RGP office


Map - Geological series, Precambrian geology, Burleigh Falls area, Peterborough County

Publication Number: P3096 Scale: 1:50,000    Date: 1988

Author: Bright E.G.

Publisher Name: Ontario Geological Survey

Location:


Mono - Vermiculite in the Stanleyville area, Lanark County, eastern Ontario

Publication Number: OFR5711 Page: 76-79  Date: 1989

Author: MacKinnon A., Kingston P.W., Springer J.S.

Publisher Name: Ontario Geological Survey

Location:


File - Resident Geologist files Cavendish #54, 55, 56, 57, 58 - C.W. Archibald

Publication Number: Date:

Author:

Publisher Name:

Location: Tweed RGP office


Map - Precambrian Geology of Cavendish Township and Environs, Grenville Province

Publication Number: P3605 Scale: 1:20,000    Date: 2010

Author: Easton R.M.

Publisher Name: Ontario Geological Survey

Location:


Publication - Mica and vermiculite; Canada Centre for Mineral and Energy Technology, Canmet Report CM 90-3E

Publication Number: CM 90-3E Page: 80-81  Date: 1989

Author: Collings, R K; Andrews, P R A

Publisher Name: Canada Centre for Mineral and Energy Technology

Location: https://doi.org/10.4095/328610


File - Resident Geologist file Cavendish #116 - Regis Resources Inc

Publication Number: Date:

Author:

Publisher Name:

Location: Tweed RGP office


Mono - An inventory of the mineral resources in Peterborough County

Publication Number: OFR5635 Page: 64-65  Date: 1987

Author: Menard A.G.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Industrial minerals of the Algonquin region

Publication Number: OFR5425 Page: 291-292  Date: 1983

Author: Martin W.

Publisher Name: Ontario Geological Survey

Location:


Mono - Vermiculite in Ontario, with an appendix on perlite

Publication Number: IMR007 Page: 14-18  Date: 1998

Author: Guillet G.R.

Publisher Name: Ontario Dept. of Mines

Location:


Publication - Mica Deposits of Canada; Geological Survey of Canada, Economic Geology Series 19

Publication Number: Econ Geol 19 Page: 95, 99  Date: 1960

Author: Hoadley, J W

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/102453


Mono - Report of Activities 2000, Resident Geologist Program, Southern Ontario Regional Resident Geologist Report: Southeastern and Southwestern Districts, Mines and Minerals Information Centre and Petroleum Resources Centre

Publication Number: OFR6052 Page: Date: 2001

Author: Sangster P.J., McGuinty W.J., Papertzian V.C., Steele K.G., Lee C.R., Laidlaw D.A., Carter T.R., Spears G.J., Debicki R.L., Rowell D.J.

Publisher Name: Ontario Geological Survey

Location:


Mono - Report of Activities 2001, Resident Geologist Program, Southern Ontario Regional Resident Geologist Report: Southeastern and Southwestern Districts, Mines and Minerals Information Centre, and Petroleum Resources Centre

Publication Number: OFR6084 Page: Date: 2002

Author: Sangster P.J., McGuinty W.J., Papertzian V.C., Steele K.G., Lee C.R., Laidlaw D.A., Barua M., Carter T.R., Parkes B.D.

Publisher Name: Ontario Geological Survey

Location:


Mono - Report of Activities 2002, Resident Geologist Program, Southern Ontario Regional Resident Geologist Report: Southeastern and Southwestern Districts, Mines and Minerals Information Centre, and Petroleum Resources Centre

Publication Number: OFR6115 Page: Date: 2003

Author: Sangster P.J., McGuinty W.J., Papertzian V.C., Steele K.G., Lee C.R., Barua M., Laidlaw D.A., Carter T.R.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Precambrian Geology of Cavendish Township, Central Metasedimentary Belt, Grenville Province

Publication Number: OFR6229 Date: 2012

Author: Easton R.M.

Publisher Name: Ontario Geological Survey

Location:


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