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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Skarn from
Prosetín Quarry, Prosetín, Žďár nad Sázavou District, Vysočina Region, Czech Republic


Locality type:Quarry
Classification
Type:Skarn
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Skarn data
Locality Data:Click here to view Prosetín Quarry, Prosetín, Žďár nad Sázavou District, Vysočina Region, Czech Republic
Data Identifiers
Mindat Occurrence Record ID:1583440
Long-form Identifier:1:3:1583440:1
GUID (UUID V4):0
Nearest other occurrences of Skarn
6.5km (4.0 miles) ⓘKozlov, Bystřice nad Pernštejnem, Žďár nad Sázavou District, Vysočina Region, Czech Republic
33.7km (20.9 miles) ⓘHedenbergite skarn, Svratouch, Chrudim District, Pardubice Region, Czech Republic
50.0km (31.1 miles) ⓘMoravské Bránice vesuvianite occurrence (České Bránice vesuvianite occurrence; Mährisch Branitz vesuvianite occurrence; Böhmisch Branitz vesuvianite occurrence), Moravské Bránice (České Bránice; Mährisch Branitz; Böhmisch Branitz), Brno-Country District, South Moravian Region, Czech Republic
72.2km (44.9 miles) ⓘJezuitský rybník, Golčův Jeníkov, Havlíčkův Brod District, Vysočina Region, Czech Republic
90.6km (56.3 miles) ⓘHolý vrch deposit, Moldanubian Zone pegmatites, Vlastějovice, Kutná Hora District, Central Bohemian Region, Czech Republic
91.5km (56.9 miles) ⓘNosatá skála pegmatite, Moldanubian Zone pegmatites, Vlastějovice, Kutná Hora District, Central Bohemian Region, Czech Republic
91.7km (57.0 miles) ⓘBřezina pegmatite, Moldanubian Zone pegmatites, Vlastějovice, Kutná Hora District, Central Bohemian Region, Czech Republic
References
Bačík, P., Uher, P., Cempírek, J., Vaculovič, T. (2012) Magnesian tourmalines from plagioclase-muscovite-scapolite metaevaporite layers in dolomite marble near Prosetín (Olešnice Unit, Moravicum, Czech Republic) Journal of GEOsciences, 57 (3) 143-153
 
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