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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Chalcopyrite from
Unnamed quarry, Neustadt in Sachsen, Sächsische Schweiz-Osterzgebirge, Saxony, Germany


Classification
Species:Chalcopyrite
Formula:CuFeS2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Chalcopyrite data
Locality Data:Click here to view Unnamed quarry, Neustadt in Sachsen, Sächsische Schweiz-Osterzgebirge, Saxony, Germany
Data Identifiers
Mindat Occurrence Record ID:1287005
Long-form Identifier:1:3:1287005:9
GUID (UUID V4):0
Nearest other occurrences of Chalcopyrite
1.7km (1.0 miles) ⓘGrenzland I quarry, Neustadt in Sachsen, Sächsische Schweiz-Osterzgebirge, Saxony, Germany
2.7km (1.6 miles) ⓘValtengrund quarry, Neustadt in Sachsen, Sächsische Schweiz-Osterzgebirge, Saxony, Germany
10.3km (6.4 miles) ⓘSulphide deposit (Sohlander Bergsegen), Sohland an der Spree, Bautzen District, Saxony, Germany
13.5km (8.4 miles) ⓘFrisch Glück mine, Šluknov, Děčín District, Ústí nad Labem Region, Czech Republic
14.1km (8.8 miles) ⓘHölle quarry, Schönberg, Cunewalde, Bautzen District, Saxony, Germany
27.7km (17.2 miles) ⓘGröditz, Weißenberg, Bautzen District, Saxony, Germany
33.6km (20.9 miles) ⓘFluorite deposit, Jílové, Děčín District, Ústí nad Labem Region, Czech Republic
34.6km (21.5 miles) ⓘBerggießhübel (Berggiesshübel), Bad Gottleuba-Berggießhübel, Sächsische Schweiz-Osterzgebirge, Saxony, Germany
35.2km (21.9 miles) ⓘOßling Quarry, Oßling, Bautzen District, Saxony, Germany
35.6km (22.1 miles) ⓘDubring quarry, Wittichenau, Bautzen District, Saxony, Germany
References
Sandmann, D., & Gutzmer, J. (2015). Nature and distribution of PGE mineralisation in gabbroic rocks of the Lusatian Block, Saxony, Germany Art und Verbreitung der PGE-Mineralisation in den gabbroiden Gesteinen des Lausitzer Blocks, Sachsen, Deutschland. Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 166(1), 35-53.
 
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