Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI000000002028

Record: MDI000000002028

General

Mineral Record Identification
Record Name(s) Gunnard Project - 2015, Gagnon Falls - 1967, G. Noyes - 1967, West Pit - 1976
Related Record Type
Related Record(s)
Record Status Producing Mine
Date Created 2016-Oct-19
Date Last Modified 2022-Feb-24
Created By
Revised By

Commodities

Primary Commodities: Amethyst



Location

Township or Area: McTavish

Latitude: 48° 41' 26.44"    Longitude: -88° 41' 48.6"

UTM Zone: 16    Easting: 375125   Northing: 5394460    UTM Datum: NAD83

Resident Geologist District: Thunder Bay South

NTS Grid: 52A10NE

Point Location Description: Visible on Google Earth

Location Method: Field Visit with GPS

Access Description: Turn left onto Road #5 North in the community of Pearl, cross the railway tracks, and then proceed left for 1.9 km kilometres turning left again traveling northwesterly along a 4x4 gravel road for 3 km to the access to the quarry on the right. You have travelled to far north if you encounter a hydro tranmission corridor.



Exploration History

1967: staked by G. Noyes, who carried out stripping and trenching. 1970: G. Noyes carried out stripping and trenching. 1977: claims brought to lease. 2015: Operated under the authority of MNR Aggregate Permit No.625989, which allows for the extraction of up to 500 t/year from a quarry area of 58 ha. 2012: M. Noyes carried out prospecting. 2015-17: Mitchell and Martin Noyes carried out prospecting, stripping, and trenching.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
2.57500 20000013541 20000013541
2.54522 20000009097 20000009097

Geology

Province: Superior

Subprovince: Quetico

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Breccia-unsubdivided 1 Is
Quartz Monzonite 1 Contains

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1AmethystEconomicOre
2GalenaEconomicOre
3ChalcopyriteEconomicOre
4PyriteEconomicOre

Mineralization Comments

Feb 25, 2020 (Therese Pettigrew) - The property is located on the east half of Concession V and north half of Lot 4, McTavish Township. The first occurrence is in the bed of a creek near a set of falls (4.5 m high) and was described by Kustra (1969): “this amethyst occurrence occupies a vertically dipping fault zone, striking N70E, at the contact between red Archean granitic rock and dolomite and argillite of the Sibley Formation. A trench, 18 m long, 2 m to 3 m wide and 2 m deep exposes a network of white quartz and amethyst veins, approximately 2 m wide. Locally the amethyst veins attain a width of 1 m and where the material forms vugs, crystals up to 7 cm in diameter occur. Angular fragments of dolomite and granite are enclosed by vein matter. A very minor amount of pyrite, chalcopyrite and galena also occurs. Adjacent to the fault, the granite is altered and epidotized and has a radioactive count of not more than 1.5 times background.” The breccia zone contains 20-30% quartz, 70-80% angular granitic clasts up to 3 cm in size, 5-10% vugs commonly filled with clay. Amethyst is pale lavender to black. The West Pit occurrence (location of this MDI) is 300 m west of the Falls occurrence and occurs in the side of a 9 m hill. The trench is 25 m x 4.5 m x 2.4 m. Two vein breccia zones 80/80 degrees and 50/90 degrees are exposed. The 80/90 zone cuts the 50/90 zone. Both are 1 m to 2 m wide, hosted in a quartz monzonite (red, medium-grained, 10-20% quartz, 85% red feldspar, minor amphibole). The zone contains 35-60% angular fragments of monzonite, 30-40% white quartz and 10-15% vugs; most are lined with 1 cm or less white, smokey to light purple amethyst. Where the two zones intersect, two large vugs 0.6 x 1 x 2 m and 1 x 1 x 1 m occur. The vugs are partially clay-filled and lined with 8 cm crystals, some are hematite coated. The Hydroline Occurrence is reached by following the bush road 30 m west where the road branches (north and south), take the southern branch for 425 m to the powerline. The occurrence is on the north side of the outcrop on a 6 m cliff face. A series of quartz veins 8 cm to 40 cm wide across a zone 40 m wide. The zone strikes 119/90 degrees. Sections contain vugs from 30 to 60 cm across, clay-filled lined with dark purple amethyst up to 30 cm across, often hematite coated. The host rock is quartz monzonite (Thunder Bay mineral deposit files).



Mineral Record Details

References

Map - Geological series, McTavish Township (west part of north half), District of Thunder Bay

Publication Number: P0720 Scale: 1:15,840    Date: 1997

Author: McIlwaine W.H.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Mono - Amethyst deposits of Ontario

Publication Number: GB05 Scale:     Date: 1998

Author: Vos M.A.

Publisher Name: Ontario Division of Mines

Location:


Article - Port Arthur District

Publication Number: MP023.003 Scale:     Date: 1997

Author: Kustra C.R.

Publisher Name: Ontario Dept. of Mines

Location:


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For detailed information regarding this mineral record please contact the Thunder Bay South Resident Geologist District Office