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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Fluorite from
Flecktrog Alp mine, Scharnbachgraben, Hollersbach im Pinzgau, Zell am See District, Salzburg, Austria


Locality type:Mine
Classification
Species:Fluorite
Formula:CaF2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Fluorite data
Locality Data:Click here to view Flecktrog Alp mine, Scharnbachgraben, Hollersbach im Pinzgau, Zell am See District, Salzburg, Austria
Data Identifiers
Mindat Occurrence Record ID:265558
Long-form Identifier:1:3:265558:1
GUID (UUID V4):0
Nearest other occurrences of Fluorite
0.5km (0.3 miles) ⓘAchsel Alp mine, Scharnbachgraben, Hollersbach im Pinzgau, Zell am See District, Salzburg, Austria
3.1km (1.9 miles) ⓘRussland, Hollersbach im Pinzgau, Zell am See District, Salzburg, Austria
3.1km (1.9 miles) ⓘSchafkopf east slope, Hollersbach im Pinzgau, Zell am See District, Salzburg, Austria
5.3km (3.3 miles) ⓘSedl, Nasenkopf mountain, Bramberg am Wildkogel, Zell am See District, Salzburg, Austria
7.0km (4.4 miles) ⓘWestern ore field, Mittersill Scheelite deposit, Mittersill, Zell am See District, Salzburg, Austria
7.0km (4.4 miles) ⓘMittersill Scheelite deposit, Mittersill, Zell am See District, Salzburg, Austria
7.3km (4.6 miles) ⓘWildenkar, Bramberg am Wildkogel, Zell am See District, Salzburg, Austria
8.0km (5.0 miles) ⓘBreitfuß west slope, Ascham Alp - Breitfuß - Sonntagskopf area, Neukirchen am Großvenediger, Zell am See District, Salzburg, Austria
8.1km (5.0 miles) ⓘKyanite-Quartzite outcrops, Leutachkopf - Stocker Alp area, Neukirchen am Großvenediger, Zell am See District, Salzburg, Austria
8.1km (5.1 miles) ⓘPopberg Alp (Poppberg Alp), Neukirchen am Großvenediger, Zell am See District, Salzburg, Austria
References
Exel, Reinhard (1993) Die Mineralien und Erzlagerstätten Österreichs. Eigenverlag R. Exel. p.1-447.
 
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