Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Epidote from
Big Onion copper-molybdenum deposit, Smithers, Omineca Mining Division, British Columbia, Canada


Locality type:Deposit
Classification
Species:Epidote
Formula:(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Epidote data
Locality Data:Click here to view Big Onion copper-molybdenum deposit, Smithers, Omineca Mining Division, British Columbia, Canada
Data Identifiers
Mindat Occurrence Record ID:623677
Long-form Identifier:1:3:623677:9
GUID (UUID V4):0
Nearest other occurrences of Epidote
25.9km (16.1 miles) ⓘDavidson deposit, Omineca Mining Division, British Columbia, Canada
29.8km (18.5 miles) ⓘDuthie Mine, Smithers, Omineca Mining Division, British Columbia, Canada
46.4km (28.8 miles) ⓘOld Fort copper-molybdenum occurrence, Old Fort Mountain, Omineca Mining Division, British Columbia, Canada
47.6km (29.6 miles) ⓘBell Mine (Newman Mine), Granisle, Omineca Mining Division, British Columbia, Canada
49.7km (30.9 miles) ⓘGranisle mine, Granisle, Omineca Mining Division, British Columbia, Canada
56.6km (35.2 miles) ⓘMorrison Cu-Au deposit, Granisle, Omineca Mining Division, British Columbia, Canada
58.0km (36.1 miles) ⓘRed Rose Mine, Omineca Mining Division, British Columbia, Canada
58.2km (36.2 miles) ⓘSerb Creek prospect, Omineca Mining Division, British Columbia, Canada
58.2km (36.2 miles) ⓘRed Rose Mine, New Hazelton, Omineca Mining Division, British Columbia, Canada
59.7km (37.1 miles) ⓘFrench Peak silver-rich polymetallic occurrence, Fort Babine, Omineca Mining Division, British Columbia, Canada
References
Peatfield, Giles (n.d.) Personal communication.
Singer, D.A., Berger, V.I., Moring, B.C. (2008) Porphyry copper deposits of the world: Database and grade and tonnage models, 2008. Open-File Report 2008-1155
 
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