Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31C11SW00040

Record: MDI31C11SW00040

General

Mineral Record Identification
Record Name(s) Tweed Marble Quarry - 2022, Hungerford Quarry - 1981
Related Record Type Simple
Related Record(s)
Record Status Past Producing Mine With Reserves or Resources
Date Created 1981-Dec-16
Date Last Modified 2022-Sep-23
Created By
Revised By

Commodities

Primary Commodities: Marble (Building Stone)

Secondary Commodities: Feldspar (Gemstones)



Location

Township or Area: Hungerford

Latitude: 44° 31' 40.83"    Longitude: -77° 20' 10.61"

UTM Zone: 18    Easting: 314359.03   Northing: 4933175.19    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31C11SW

Point Location Description: Entrance to quarry from access road.

Location Method: Field Visit

Access Description: Travel north on highway 37 from Tweed to the Hawkins Bay Road. Turn left or to the west, crossing a steel grated bridge. Immediately after crossing the bridge, turn left or south onto Byer's Lane and follow the road to a salvage yard. Continue on through the salvage yard to the entrance of the quarry.



Exploration History

The deposit was developed as a building stone quarry and was operated by Vermont Marble Company in the late 1960s. The quarry measured approximately 20 x 20 meters by 10 to 15m deep. Extensive quarry block extraction occurred from 1996 to the late fall of 1998 by the Senator Stone Company. As of 2022, the quarry is currently owned by A. Marmaro & Terrazzo Olympic, LLC and is inactive.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
10 31C11SW0042 31C11SW0042

Geology

Province: Grenville

Subprovince: Central Metasedimentary Belt

Terrane: Mazinaw

Geological Age: Mesoproterozoic  



Lithology Comments

May 04, 2022 (P LeBaron) - In addition to white marble, a variety of colours can be seen in the quarry, including pink, salmon, green, and blue. Other minerals present are tremolite, wollastonite, diopside, serpentine and pyrite. A narrow pegmatite dike cutting through the quarry area contains quartz, feldspar, amphibole, garnet, tourmaline and amazonite.


Dec 07, 2005 (C Papertzian) - The marble varies from predominantly dolomitic marble with thin, coarser, intercalated calcitic and tremolitic units, to a white, wollastonite-bearing calcitic marble/calc-silicate rock. The dolomitic marble is fine to medium grained, and white to cream and green in colour. Accessory minerals include tremolite, diopside, serpentine, quartz, pyrite and local hematite staining. The rock is massive to foliated, striking 021-030 degrees and dipping southeast 73 degrees. Irregular, boudinaged amphibolite dikes up to 2 m in width intrude the marble in the vicinity of the quarry. Jointing in the quarry is regular to irregular, and limited to moderate in extent. (From OFR 5715, p135).




Mineral Record Details

Classification
RankClassification            
1 Dimension Stone
2 Pegmatite

Site Visit Information

Date: Feb 21, 2001

Geologist: C Papertzian

Notes: The property was active from the spring of 1996 up to October 1st of 1998. This was the last time that the property appeared to be active. The property was visited on November 9, 1999 and was inactive at the time. The quarry had been allowed to flood and was completely full of water. It was subsequently visited on April 28th, 2000 and July 18th, 2000. The quarry was water filled and no activity was evident.


Date: Mar 13, 2003

Geologist: C Papertzian

Notes: The deposit was visited on September 3, 2002. At that time the quarry was flooded and no work had been completed that season. What appeared to be waste blocks had been renumbered. This was all the activity that was in evidence.


Date: Mar 16, 2004

Geologist: C Papertzian

Notes: The deposit was visited on July 24th, 2003. At that time the quarry was flooded and no work had been completed that season. A number of what appeared to be waste blocks had been removed from the quarry site. This was all the activity that was in evidence.



References

Publication - Limestones of Canada, their occurrence and characteristics, part IV, Ontario

Publication Number: CMB Pub 781 Page: 95, 109-110  Date: 1938

Author: Goudge, M F

Publisher Name: Canada Mines Branch

Location: https://doi.org/10.4095/75823


Part - The limestones of Ontario

Publication Number: ARV13-02 Page: 65  Date: 1998

Author: Miller W.G.

Publisher Name: Ontario Bureau of Mines

Location:


Mono - Building stones of Ontario, part 3, marble

Publication Number: IMR016 Page: 53-54  Date: 1998

Author: Hewitt D.F.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Building stone of eastern Ontario, southern Ontario

Publication Number: OFR5556 Page: 63  Date: 1985

Author: Verschuren C.P., van Haaften S., Kingston P.W.

Publisher Name: Ontario Geological Survey

Location:


Mono - Reconnaissance survey of building stones of eastern and central Ontario

Publication Number: OFR5585 Page: 233-5  Date: 1986

Author: Verschuren C.P., Papertzian V.C., Kingston P.W., Villard D.J.

Publisher Name: Ontario Geological Survey

Location:


Mono - Precambrian dolomite resources in southeastern Ontario

Publication Number: OFR5712 Page: 75-77  Date: 1990

Author: LeBaron P.S., MacKinnon A.

Publisher Name: Ontario Geological Survey

Location:


Mono - Wollastonite in southeastern Ontario

Publication Number: OFR5715 Page: 133-9  Date: 1990

Author: MacKinnon A.

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