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
Kujnišova dolina ore occurrence, Mníšek nad Hnilcom, Gelnica District, Košice Region, Slovakia


Locality type:Occurrence
Classification
Species:Quartz
Formula:SiO2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Quartz data
Locality Data:Click here to view Kujnišova dolina ore occurrence, Mníšek nad Hnilcom, Gelnica District, Košice Region, Slovakia
Data Identifiers
Mindat Occurrence Record ID:1543516
Long-form Identifier:1:3:1543516:7
GUID (UUID V4):0
Nearest other occurrences of Quartz
1.0km (0.6 miles) ⓘMníšek nad Hnilcom quartz deposit, Mníšek nad Hnilcom, Gelnica District, Košice Region, Slovakia
1.3km (0.8 miles) ⓘČertovo uhlisko vein, Mníšek nad Hnilcom, Gelnica District, Košice Region, Slovakia
1.4km (0.9 miles) ⓘHlboký potok veins, Mníšek nad Hnilcom, Gelnica District, Košice Region, Slovakia
3.0km (1.9 miles) ⓘMníšek nad Hnilcom Cu-Pb-Zn-S deposit, Mníšek nad Hnilcom, Gelnica District, Košice Region, Slovakia
3.0km (1.9 miles) ⓘJozef vein, Slovinky, Spišská Nová Ves District, Košice Region, Slovakia
3.6km (2.3 miles) ⓘDošťavná vein, Slovinky, Spišská Nová Ves District, Košice Region, Slovakia
3.7km (2.3 miles) ⓘBanské antimony deposit, Helcmanovce, Gelnica District, Košice Region, Slovakia
4.1km (2.5 miles) ⓘJašterica copper deposit, Mníšek nad Hnilcom, Gelnica District, Košice Region, Slovakia
4.2km (2.6 miles) ⓘPrakovce Cu-Pb-Zn-S deposit, Prakovce, Gelnica District, Košice Region, Slovakia
4.3km (2.7 miles) ⓘBiela vein, Helcmanovce Cu-Fe deposit, Helcmanovce, Gelnica District, Košice Region, Slovakia
References
Kúšik, D., Bancík, T., Toth, P., Sakmár, J. (2021) Hydrothermal Bi-Te-(Hg) mineralization with coloradoite (HgTe) in the Kujnišova dolina valley, Mníšek nad Hnilcom, Gemeric Unit, W. Carpathians. Mineralia Slovaca, 53 (2). 91-102
 
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