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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Dolomite from
Zenderling Hg deposit, Gelnica, Gelnica District, Košice Region, Slovakia


Locality type:Mine
Classification
Species:Dolomite
Formula:CaMg(CO3)2
Confirmation
Validity:Believed Valid
Associated Minerals Based on Photo Data:
Marrucciite1
Boulangerite1
Cinnabar1
Quartz1
Data
Mineral Data:Click here to view Dolomite data
Locality Data:Click here to view Zenderling Hg deposit, Gelnica, Gelnica District, Košice Region, Slovakia
Data Identifiers
Mindat Occurrence Record ID:765272
Long-form Identifier:1:3:765272:1
GUID (UUID V4):0
Nearest other occurrences of Dolomite
1.7km (1.1 miles) ⓘOtakar vein, Perlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
1.8km (1.1 miles) ⓘKarol vein, Perlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
2.0km (1.2 miles) ⓘJozef-Michal vein, Perlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
2.0km (1.2 miles) ⓘSlovenské cechy, Krížová vein, Gelnica, Gelnica District, Košice Region, Slovakia
2.0km (1.3 miles) ⓘRoberti vein, Gelnica, Gelnica District, Košice Region, Slovakia
2.1km (1.3 miles) ⓘAlbrecht vein, Perlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
2.2km (1.4 miles) ⓘGregori-Liborni vein, Perlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
2.4km (1.5 miles) ⓘPerlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
2.5km (1.5 miles) ⓘKoloman vein, Perlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
2.6km (1.6 miles) ⓘMarkus vein, Perlová dolina, Gelnica, Gelnica District, Košice Region, Slovakia
References
Sejkora, J., Ozdín, D., Laufek, F., Plášil, J., Litochleb, J. (2011) Marrucciite, a rare Hg-sulfosalt from the Gelnica ore deposit (Slovak Republic), and its comparison with the type occurrence at Buca della Vena mine (Italy) Journal of GEOsciences, 56 (4) 399-408
 
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