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Globe Graphite mine, Elmsley Township, Lanark County, Ontario, Canadai
Regional Level Types
Globe Graphite mineMine
Elmsley TownshipTownship
Lanark CountyCounty
OntarioProvince
CanadaCountry

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Latitude & Longitude (WGS84):
44° 51' 34'' North , 76° 9' 35'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Perth6,481 (2008)8.4km
Smiths Falls10,553 (2018)11.9km
Carleton Place9,743 (2008)30.5km
Ashton200 (2013)33.8km
Brockville23,886 (2013)47.8km
Mindat Locality ID:
234546
Long-form identifier:
mindat:1:2:234546:1
GUID (UUID V4):
48416147-d254-4bcf-aa26-9c57fb5c178a


This was the first graphite mine in Ontario.
History:
1871-5 - the International Mining Co.
1893 - Northern Graphite Co.
1901 - R.A. Pyne
1902-3 - R. McConnell
1908-11 - Globe Refining Co.
1915-1916 - Globe Graphite Refining and Milling Co.
1916-1919 - Globe Graphite Mining and Refining Co.
1983-4 : Black Gregor Explorations Inc (Bowdidge and Associates) carried out geology, mag, E.M., an SP survey and drilling (4 DDH, 1,099 ft) on the property.

Workings consisted of the main pit, 400 x 10-30 ft; a shaft which was sunk at the NE end of the pit (250 ft deep with 4 levels at 100, 150, 200 and 250 ft. These extended about 200 ft in each direction along strike); a second shaft (1916) which was sunk to 106 ft at a point 400 ft NW of the main shaft. Some drifting was carried out at 50 and 1000 ft. There was also a third pit.

Geology:

The property is located within an inlier of Grenville rocks surrounded by Paleozoic sandstone. The deposit is hosted in marble (white, well-banded) and calc-silicates (diopside-pyroxenite to diopside and calcite-bearing feldspathic gneisses). The orebody forms a saddle-shaped mass in highly silicated marble intruded by pegmatites (gabbro to syenite) and may be the result of contact metamorphism. Graphite content increases with silicates. The main ore zone has been traced for 400 ft on the dragfolded N limb of a steeply plunging antiform. The ore appears to occur in 2 lens-like bodies (1942), the E one being about 250 x 7-10 ft and nearly 40 ft thick on the crest of the antiform. The W lens is 4 ft thick for about 70 ft then 8 ft thick for 90 ft. The zone S of the pit is structurally complex. The graphite is predominantly flake (0.5-1.0 mm) with small bodies of ' needle ' flake. There may be 4 zones of mineralization where up to 20 % graphite is separated by medium to low grade bands. Mineralization extends to at least 300 ft deep, but the thickness, strike length and grade appear to be somewhat less than at surface where up to 15 % graphite was reported over 40 ft.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Graphite1.CB.05aC
Group 2 - Sulphides and Sulfosalts
β“˜Pyrite2.EB.05aFeS2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
Group 9 - Silicates
β“˜Titanite9.AG.15CaTi(SiO4)O
β“˜Diopside9.DA.15CaMgSi2O6
Unclassified
β“˜'Feldspar Group'-

List of minerals for each chemical element

CCarbon
Cβ“˜ CalciteCaCO3
Cβ“˜ GraphiteC
OOxygen
Oβ“˜ CalciteCaCO3
Oβ“˜ DiopsideCaMgSi2O6
Oβ“˜ TitaniteCaTi(SiO4)O
MgMagnesium
Mgβ“˜ DiopsideCaMgSi2O6
SiSilicon
Siβ“˜ DiopsideCaMgSi2O6
Siβ“˜ TitaniteCaTi(SiO4)O
SSulfur
Sβ“˜ PyriteFeS2
CaCalcium
Caβ“˜ CalciteCaCO3
Caβ“˜ DiopsideCaMgSi2O6
Caβ“˜ TitaniteCaTi(SiO4)O
TiTitanium
Tiβ“˜ TitaniteCaTi(SiO4)O
FeIron
Feβ“˜ PyriteFeS2

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References

 
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