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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Calcite from
Forster Prospect, Weld river district, Huon-Channel region, Huon Valley municipality, Tasmania, Australia


Locality type:Prospect
Classification
Species:Calcite
Formula:CaCO3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Calcite data
Locality Data:Click here to view Forster Prospect, Weld river district, Huon-Channel region, Huon Valley municipality, Tasmania, Australia
Data Identifiers
Mindat Occurrence Record ID:428912
Long-form Identifier:1:3:428912:8
GUID (UUID V4):0
Nearest other occurrences of Calcite
3.4km (2.1 miles) ⓘEddy Creek quarry, Weld River district, Huon-Channel region, Huon Valley municipality, Tasmania, Australia
14.7km (9.1 miles) ⓘRussell Road Quarry, Lonnavale, Huon-Channel region, Huon Valley municipality, Tasmania, Australia
14.8km (9.2 miles) ⓘWyena Rd Quarry, Geeveston, Huon-Channel region, Huon Valley municipality, Tasmania, Australia
24.7km (15.4 miles) ⓘDuggans Cradoc quarry, Cradoc, Huon-Channel region, Huon Valley municipality, Tasmania, Australia
30.3km (18.8 miles) ⓘCygnet district, Huon-Channel region, Huon Valley municipality, Tasmania, Australia
30.8km (19.1 miles) ⓘGold Creek Quarry, Maydena district, Derwent Valley municipality, Tasmania, Australia
33.2km (20.6 miles) ⓘMaynes Hill quarry, Maydena district, Derwent Valley municipality, Tasmania, Australia
38.1km (23.6 miles) ⓘLongley, Kingborough municipality, Tasmania, Australia
39.8km (24.7 miles) ⓘMcCarthy's Quarry, Longley, Kingborough municipality, Tasmania, Australia
40.5km (25.2 miles) ⓘAllanfield quarry, Leslie Vale, Kingborough municipality, Tasmania, Australia
References
Bottrill, Ralph S.; Baker, William. E. (2008) Geological Survey of Tasmania Bulletin - A Catalogue of the Minerals of Tasmania No. 73. Mineral Resources Tasmania. 254 pp.
 
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