Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31E07SW00012

Record: MDI31E07SW00012

General

Mineral Record Identification
Record Name(s) International Quartz Fletcher Lake Property - 1977, Fletcher Lake Quartz - 2000
Related Record Type Simple
Related Record(s)
Record Status Developed Prospect With Reported Reserves or Resources
Date Created 1991-Feb-11
Date Last Modified 2023-Mar-21
Created By
Revised By

Commodities

Primary Commodities: Quartz



Location

Township or Area: McClintock

Latitude: 45° 20' 55.78"    Longitude: -78° 48' 37.27"

UTM Zone: 17    Easting: 671526.841   Northing: 5024034.073    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31E07SW

Point Location Description: Precise. Based on satellite imagery of pit.

Location Method: Data Compilation

Access Description: The site can be accessed from County Road 12 which follows the south shore of Lower Fletcher Lake to a short access road leading to a small control dam at the southwest end of Fletcher Lake. From the dam road, the entrance trail/haul road to the quarry site is a left branch leading closely along the north shore of Fletcher Lake for approximately l km.



Exploration History

1990-2008: F. Jones – stripping, trenching, DD-5-131 m


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
Tweed File McClintock # 52 / 2.20420 31E07SW2004 31E07SW2004
Tweed File McClintock #52 / 2.20849 31E07SW2007 31E07SW2007
Tweed File McClintock 59 / 2.26513 31E07NW2007 31E07NW2007
Tweed File McClintock #58 / 2.26663 31E07SW2009 31E07SW2009

Geology

Province: Grenville

Subprovince: Central Gneiss Belt

Terrane: Algonquin

Domain: McClintock

Geological Age: Mesoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Pegmatite 1 Host
Gneiss-Unsubdivided 2 Contains
Gabbro 3 Gabbro And Diorite Contains

Lithology Comments

Feb 20, 2013 (A Wilson) - From the surface exposures, the deposit consists of a "zoned" pegmatite body with a core of nearly pure quartz. Surrounding the quartz are essentially parallel inner zones of potassic feldspar megacrysts. Further out from the quartz is an external zone of sodic feldspar pegmatite in contact with the wallrocks (biotite gniess). This quartz vein has a general trend of 095° and is 3-5 m wide at the east and west end and thickens to 10-15 m in width in the central portion. The vein appears to form an open fold (W- faulting) as the west portion strikes at 065° and dips 80° to 90° SE and the east portion strikes 110° and dips 65° SW. The vein is exposed over a length of 180 m and has been quarried in two pits in the central portion. The eastern pit is an elongate open cut that is approximately 50 m long, 7 to 10 m wide and 4 to 6 m deep (along the north face and west end). The west pit is separated from the east pit by a ridge of blasted pegmatitic boulders and outcrop and amphibolite outcrop. The west pit has dimensions of approximately 13 m x 25 m and is 3-5 m deep. The host rock to the vein is a medium-grained lineated, biotite amphibolite. Plagioclase-rich bands gradually alternate with thin fine-grained bands, lenses and xenoliths of mafic to ultramafic composition.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1QuartzEconomicOre
2FeldsparEconomicOre
3BiotiteEconomicOre
4EpidoteEconomicOre
5EuxeniteEconomicOre
6TremoliteEconomicOre

Mineralization Comments

Feb 20, 2013 (A Wilson) - The central quartz is of exceptional purity, containing only minute traces of other minerals. Locally, some hematite staining is present on fracture surfaces – probably related to weathering effects or groundwater percolation. Occasional megacrysts of potassic feldspar are present in the quartz, especially near the quartz zone contacts. From this site, five samples resulted in an average normalized SiO2 value of 99.92% by means of XRF analysis. The normalized SiO2 range from 99.91% to 99.94%.



Mineral Record Details

Site Visit Information

Date: Jun 07, 2010

Geologist: P Sangster

Notes: site visited with MNR Aggregate Inspector - no apparent change to site since earler visit



Production Data
Year Tonnes Commodities Reference Comment
1977 7257 About 8000 tons of quartz had been marketed by 1977. The quarry was also active as an on demand site for local decorative and commercial purposes.

References

Article - 1976 report of the Sudbury Resident Geologist

Publication Number: MP071.008 Page: 122  Date: 1997

Author: Giblin P.E.

Publisher Name: Ontario Geological Survey

Location:


MonoMap - Industrial minerals of the Algonquin region

Publication Number: OFR5425 Page: 257-258  Date: 1983

Author: Martin W.

Publisher Name: Ontario Geological Survey

Location:


Mono - Granitic pegmatites of the Bancroft area, southeastern Ontario

Publication Number: OFR5717 Page: 164  Date: 1990

Author: Goad B.E.

Publisher Name: Ontario Geological Survey

Location:


Compend - Report of activities, 1991, Resident Geologists

Publication Number: MP158 Page: 344  Date: 1992

Author: Fenwick K.G., Newsome J.W., Pitts A.E.

Publisher Name: Ontario Geological Survey

Location:


Mono - Report of Activities 1999, Resident Geologist Program, Southern Ontario Regional Resident Geologist Report: Southeastern and Southwestern Districts, Mines and Minerals Information Centre and Petroleum Resources Centre

Publication Number: OFR6008 Page: 19  Date: 2000

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

Publisher Name: Ontario Geological Survey

Location:


Mono - An Evaluation of Potential High-Purity Silica Sources: Preliminary Site Investigation, Volumes 1 and 2

Publication Number: OFR5948 Page: 229-234  Date: 1996

Author: McAuley J.B.

Publisher Name: Ontario Geological Survey

Location:


Map - Precambrian Geology, Kawagama Lake Area

Publication Number: P3525 Scale: 1:50,000    Date: 2003

Author: Lumbers S.B., Vertolli V.M.

Publisher Name: Ontario Geological Survey

Location:


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