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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Covellite from
Kružberk quarry, Kružberk, Opava District, Moravian-Silesian Region, Czech Republic


Locality type:Quarry
Classification
Species:Covellite
Formula:CuS
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Covellite data
Locality Data:Click here to view Kružberk quarry, Kružberk, Opava District, Moravian-Silesian Region, Czech Republic
Data Identifiers
Mindat Occurrence Record ID:605430
Long-form Identifier:1:3:605430:4
GUID (UUID V4):0
Nearest other occurrences of Covellite
15.3km (9.5 miles) ⓘHorní Benešov mines, Horní Benešov, Bruntál District, Moravian-Silesian Region, Czech Republic
15.9km (9.9 miles) ⓘJakubčovice nad Odrou quarry, Jakubčovice nad Odrou, Nový Jičín District, Moravian-Silesian Region, Czech Republic
19.6km (12.2 miles) ⓘDomašov nad Bystřicí quarry (Domstadtl quarry), Domašov nad Bystřicí (Domstadtl), Olomouc District, Olomouc Region, Czech Republic
27.3km (16.9 miles) ⓘHrabůvka quarry, Hrabůvka, Přerov District, Olomouc Region, Czech Republic
33.8km (21.0 miles) ⓘNová Ves deposit, Nová Ves, Dolní Moravice, Bruntál District, Moravian-Silesian Region, Czech Republic
42.5km (26.4 miles) ⓘVidly deposit, Vidly, Vrbno pod Pradědem, Bruntál District, Moravian-Silesian Region, Czech Republic
46.8km (29.1 miles) ⓘTieschitz meteorite, Těšetice, Olomouc District, Olomouc Region, Czech Republic
49.4km (30.7 miles) ⓘAnna mine (Anna adit), Zlaté Hory, Jeseník District, Olomouc Region, Czech Republic
57.3km (35.6 miles) ⓘŘepová mine, Řepová, Mohelnice, Šumperk District, Olomouc Region, Czech Republic
60.2km (37.4 miles) ⓘSmrčník hill, Lipová-lázně, Jeseník District, Olomouc Region, Czech Republic
References
Klomínský, J.: Nový výskyt chalkopyritu v severomoravském kulmu. Přírodovědný časopis Slezský, 1960, roč. 21, č. 1, s. 122-123.
 
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