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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Quartz from
Blue Jacket Tin Mine (Blue Jacket Reef), Glen Valley, East Gippsland Shire, Victoria, Australia


Locality type:Mine
Classification
Species:Quartz
Formula:SiO2
Confirmation
Validity:Believed Valid
Associated Minerals Based on Photo Data:
Lepidolite1
Albite1
Cassiterite1
Data
Mineral Data:Click here to view Quartz data
Locality Data:Click here to view Blue Jacket Tin Mine (Blue Jacket Reef), Glen Valley, East Gippsland Shire, Victoria, Australia
Data Identifiers
Mindat Occurrence Record ID:959507
Long-form Identifier:1:3:959507:1
GUID (UUID V4):0
Nearest other occurrences of Quartz
1.0km (0.6 miles) ⓘKnocker dyke (South Blue Jacket), Glen Valley, East Gippsland Shire, Victoria, Australia
1.0km (0.7 miles) ⓘKnocker Tract, Glen Valley, East Gippsland Shire, Victoria, Australia
1.7km (1.1 miles) ⓘMt Wills mining district, Glen Valley, East Gippsland Shire, Victoria, Australia
2.7km (1.7 miles) ⓘSoft Lode, Glen Wills, East Gippsland Shire, Victoria, Australia
3.4km (2.1 miles) ⓘLease 922, Glen Wills, East Gippsland Shire, Victoria, Australia
4.1km (2.6 miles) ⓘDemocrat mine, Sunnyside goldfield, Glen Wills, East Gippsland Shire, Victoria, Australia
4.3km (2.6 miles) ⓘLivingstone mine, Sunnyside goldfield, Glen Wills, East Gippsland Shire, Victoria, Australia
4.6km (2.9 miles) ⓘUnited Brothers mine, Sunnyside goldfield, Glen Wills, East Gippsland Shire, Victoria, Australia
4.7km (2.9 miles) ⓘMeerschaum mine, Sunnyside goldfield, Glen Wills, East Gippsland Shire, Victoria, Australia
4.8km (3.0 miles) ⓘSmile of Fortune mine, Sunnyside goldfield, Glen Wills, East Gippsland Shire, Victoria, Australia
References
Eagle, Ryan M.; Birch, William D.; McKnight, Stafford (2015) Phosphate minerals in granitic pegmatites from the Mount Wills District, north-eastern Victoria. Proceedings of the Royal Society of Victoria, 127 (2). 55-68 doi:10.1071/rs15018
 
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