Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31C15NE00010

Record: MDI31C15NE00010

General

Mineral Record Identification
Record Name(s) Purdon's Lake - 1989
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 1990-Nov-09
Date Last Modified 2022-Dec-05
Created By
Revised By

Commodities

Primary Commodities: Marble (Building Stone)



Location

Township or Area: Dalhousie

Latitude: 44° 59' 3.17"    Longitude: -76° 31' 38.79"

UTM Zone: 18    Easting: 379581.11   Northing: 4982331.67    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31C15NE

Point Location Description: Point 1.75 km southeast of Purdons Lake.

Location Method: Data Compilation

Access Description: Approximately l km east of Dalhousie Lake, 2 km north of McDonalds Corners, on a northwest-trending road, Concession VII, Lot 11..



Geology

Province: Grenville

Subprovince: Central Metasedimentary Belt

Terrane: Sharbot Lake

Geological Age: Mesoproterozoic  



Geology Comments

Dec 07, 2005 (C Papertzian) - Sample of white calcitic marble (possibly a suitable filler material) - minor impurities but some tremolite zones and granitic veins. Part of a wide belt trending NE across the SE corner of the township.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Marble 1 Dolomitic Host

Lithology Comments

Sep 15, 2015 (A Wilson) - This sample was taken from a wide marble belt which trends northeast across the southeastern corner of Dalhousie Township into Lanark and Ramsay Townships. This belt has numerous narrow metasedimentary, amphibolitic, and metaigneous units running parallel to, and contained within it. The belt is several kilometres wide in some areas and up to 20 km in length. It is flanked to the southeast by amphibolite where it is partially overlain by Ordovician sedimentary rocks, and to the northwest by metadiorite and amphibolite. Detailed mapping indicates that the area is underlain predominantly by white calcitic marble. Occurring within the marble are several narrow granitic dikes, most trending in a north-northeast direction. Only minor impurities occur within the marble, with the exception of a couple of narrow tremolite-rich zones.




Mineral Record Details

References

Mono - Geochemistry of Grenville marble in southeastern Ontario

Publication Number: MDC028 Page: 84-85  Date: 1989

Author: Grant W.T., Papertzian V.C., Kingston P.W.

Publisher Name: Ontario Geological Survey

Location:


Map - Geological series, marbles of the Pembroke-Renfrew area, southern Ontario

Publication Number: P1980 Scale: 1:126,720    Date: 1979

Author: Vos M.A., Storey C.C.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Southern Ontario Resident Geologist District Office