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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Native Gold from
Kevitsa Ni-Cu-PGE mine, Kevitsansarvi (Keivitsansarvi), Sodankylä, Lapland, Finland


Locality type:Mine
Classification
Species:Native Gold
Formula:Au
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Native Gold data
Locality Data:Click here to view Kevitsa Ni-Cu-PGE mine, Kevitsansarvi (Keivitsansarvi), Sodankylä, Lapland, Finland
Data Identifiers
Mindat Occurrence Record ID:1214811
Long-form Identifier:1:3:1214811:8
GUID (UUID V4):0
Nearest other occurrences of Native Gold
18.6km (11.6 miles) ⓘSakattilampi (Sakatti deposit), Viiankiaapa mire area, Sodankylä, Lapland, Finland
24.5km (15.2 miles) ⓘPahtavaara Au mine, Sodankylä, Lapland, Finland
38.2km (23.7 miles) ⓘKaaresselkä, Sodankylä, Lapland, Finland
48.1km (29.9 miles) ⓘIkkari deposit, Sodankylä, Lapland, Finland
53.8km (33.4 miles) ⓘKutuvuoma, Kittilä, Lapland, Finland
53.8km (33.4 miles) ⓘTankavaara, Sodankylä, Lapland, Finland
69.0km (42.9 miles) ⓘMäkärä, Sodankylä, Lapland, Finland
70.0km (43.5 miles) ⓘKittilä gold mine (Suurikuusikko mine; Rouravaara; Korkeakuusikko; Vuomajärvi), Kittilä, Lapland, Finland
70.6km (43.9 miles) ⓘRuoppapalo, Kittilä, Lapland, Finland
73.0km (45.4 miles) ⓘOiva dyke, Laanila, Inari, Lapland, Finland
References
Mutanen, Tapani (1997) Geology and ore petrology of the Akanvaara and Koitelainen mafic layered intrusions and the Keivitsa-Satovaara layered complex, northern Finland. Bulletin de la Commission Géologique de Finlande Vol. 395. Geological Survey of Finland
González-Pérez, Igor, Gervilla, Fernando, González-Jiménez, José M., Kojonen, Kari (2021) Genesis of an exotic platinum-group-mineral-rich and Mg-poor chromitite in the Kevitsa Ni-Cu-platinum-group-elements deposit. Mineralogy and Petrology, 115 (5) 535-555 doi:10.1007/s00710-021-00751-1
 
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