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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Euxenite-(Y) from
Mørefjær Feldspar Quarry (Mörefjer), Stokken, Arendal, Agder, Norway


Locality type:Quarry
Classification
Species:Euxenite-(Y)
Formula:(Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6
Confirmation
Validity:Believed Valid
Associated Minerals Based on Photo Data:
Monazite-(Ce)1
Data
Mineral Data:Click here to view Euxenite-(Y) data
Locality Data:Click here to view Mørefjær Feldspar Quarry (Mörefjer), Stokken, Arendal, Agder, Norway
Data Identifiers
Mindat Occurrence Record ID:649064
Long-form Identifier:1:3:649064:5
GUID (UUID V4):0
Nearest other occurrences of Euxenite-(Y)
0.9km (0.5 miles) ⓘHella 1 Feldspar Quarry, Helle, Stokken, Arendal, Agder, Norway
3.2km (2.0 miles) ⓘAlve Feldspar Quarry, Tromøy, Arendal, Agder, Norway
8.7km (5.4 miles) ⓘGloserheia, Froland, Agder, Norway
9.0km (5.6 miles) ⓘLandbø Mine, Landbø, Austre Moland, Arendal, Agder, Norway
30.3km (18.8 miles) ⓘLindstøl Feldspar Quarry, Søndeled, Risør, Agder, Norway
32.0km (19.9 miles) ⓘRandvik Mine, Risør, Agder, Norway
50.3km (31.3 miles) ⓘKjelevann, Birkenes, Agder, Norway
50.8km (31.6 miles) ⓘSjåen feldspar Mine, Sjåen, Kragerø, Telemark, Norway
50.9km (31.6 miles) ⓘTangen Feldspar Mine, Kragerø, Telemark, Norway
50.9km (31.7 miles) ⓘLindvikskollen Quarry, Lindvikskollen-Kalstadgangen pegmatite, Kragerø, Telemark, Norway
References
Forbes, David, Dahll, T. (1857) Mineralogiske Iagttagelser omkring Arendal og Kragerø (Fortsættelse) [Mineralogical Observations around Arendal and Kragerø (Continuation)]. Nyt magazin for naturvidenskaberne [New magazine for the natural sciences], 9. 14-20
Brøgger, W. C. (1906) Die Mineralien der Südnorwegischen Granit-Pegmatitgänge - I. Niobate, Tantalate, Titanate und Titanoniobate [The minerals of the South Norwegian granite pegmatite dikes - I. Niobates, tantalates, titanates and titanoniobates]. Videnskabsselskabet i Christiania Skrifter - I Mathematisk-naturvidenskabelig klasse, 1906 (6). 1-162p.109
 
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