Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31C16SW00031

Record: MDI31C16SW00031

General

Mineral Record Identification
Record Name(s) P. Farrell Property - 1951, Northern Vermiculite Ltd. - 1956, Norden Vermiculite Ltd. - 1961
Related Record Type Simple
Related Record(s)
Record Status Past Producing Mine Without Reserves or Resources
Date Created 1982-Apr-23
Date Last Modified 2022-Apr-25
Created By
Revised By

Commodities

Primary Commodities: Vermiculite



Location

Township or Area: Burgess, Burgess, Burgess

Latitude: 44° 49' 5.64"    Longitude: -76° 19' 5.96"

UTM Zone: 18    Easting: 395768   Northing: 4963604    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31C16SW

Point Location Description: numerous pits

Location Method: AMIS Site Visit

Access Description: From Perth, west on hwy 6 for 6.71km turning left onto Glen Tay Rd for 2.92km. Right onto Scotch Line Rd (hwy 10) for 1.96km then left onto hwy 10 for 3.96km. Site is located ~75m northwest of hwy through the bush.



Exploration History

1951-1952: North Bay Mica Company Ltd. – trenching, diamond drilling. 1956-57: Northern Vermiculite Ltd. – property optioned; property in production, established exfoliating plant in Perth, then opened plant in Glen Tay. 1958: Rochester and Pittsburgh Coal Company – property optioned, 610 m DD. 1960-61: Norden Vermiculite Ltd. – DD-13.


Geology

Province: Grenville

Subprovince: Central Metasedimentary Belt

Terrane: Frontenac

Geological Age: Mesoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Marble 1 Host
Gneiss-Unsubdivided 2 Phlogopite-Diopside Adjacent

Lithology Comments

Sep 10, 2015 (A Wilson) - The main zone as "a steeply plunging pod of coarse grained phlogopite-diopside gneiss enclosed by a moderately silicated marble. The zone, measuring some 200 feet by 70 feet, elongated in a northeast-southwest direction, and plunges to the east at 75º. The degree of vermiculitization is generally low. Small lenses of biotite schist containing a high degree of vermiculitization occur elsewhere on the property. Partially hydrated, light coloured mica occurs as disseminations within the marble band. Several small (up to 1.5 m) syenitic dykes were reported by Guillet to transect both the vermiculitized zone and wallrocks, generally striking north-east and dipping easterly.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1VermiculiteEconomicOre
2PhlogopiteEconomicOre
3ApatiteEconomicOre
4DiopsideEconomicOre

Mineralization Comments

Sep 10, 2015 (A Wilson) - Mica has been partly altered to vermiculite, but the degree of hydration is generally not high. Elsewhere on the property are minor lenses of biotite schist, some of which are quite highly vermiculitized. Flake size of the mica is commonly in the range of 1/8 to 3/8 of an inch.



Mineral Record Details

Classification
RankClassification            
1 Industrial
Characteristics
Rank Characteristic            
1 Stratiform

Mineral Zones - Size and Shape

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Lens 200 70
Production Data
Year Tonnes Commodities Reference Comment
1961 1 15,000 4 ft3 bags produced from the two plants before operations ceased (1956-57)

References

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

Publication Number: Econ Geol 19 Page: 97-98  Date: 1960

Author: Hoadley, J W

Publisher Name: Geological Survey of Canada

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


Mono - Vermiculite in Ontario, with an appendix on perlite

Publication Number: IMR007 Page: 11-13  Date: 1998

Author: Guillet G.R.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geological notes for maps nos. 2053 and 2054, Madoc-Gananoque area

Publication Number: S012 Page: 24  Date: 1997

Author: Hewitt D.F.

Publisher Name: Ontario Dept. of Mines

Location:


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

Publication Number: OFR5711 Page: 41-44  Date: 1989

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

Publisher Name: Ontario Geological Survey

Location:


Publication - Classic mineral collecting localities in Ontario and Quebec; Geological Survey of Canada, Miscellaneous Report 37

Publication Number: GSC MR37 Page: 37  Date: 1983

Author: Hogarth, D D; Moyd, L; Rose, E R; Steacy, H R

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/119504


Map - Gananoque area, Ontario

Publication Number: M2054 Scale: 1:126,720    Date: 1998

Author: Hewitt D.F.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Geology Perth, Lanark and Leeds Counties, Ontario

Publication Number: Map 1089A Scale: 1:63,360    Date: 1961

Author: Wilson, M E; Dugas, J

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/107951


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