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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Microcline from
Undeland 02 Feldspar Quarry (Beryl quarry), Undeland, Evje og Hornnes, Agder, Norway


Locality type:Quarry
Classification
Species:Microcline
Formula:K(AlSi3O8)
Confirmation
Validity:Believed Valid
Associated Minerals Based on Photo Data:
Beryl5
Euxenite-(Y)4
Thortveitite2
Monazite-(Ce)2
Rutile2
- var Ilmenorutile2
Plagioclase2
Gadolinite-(Y)1
Ilmenite1
Dumortierite1
Thorite1
Muscovite1
Zircon1
Schorl1
Data
Mineral Data:Click here to view Microcline data
Locality Data:Click here to view Undeland 02 Feldspar Quarry (Beryl quarry), Undeland, Evje og Hornnes, Agder, Norway
Data Identifiers
Mindat Occurrence Record ID:691627
Long-form Identifier:1:3:691627:5
GUID (UUID V4):0
Nearest other occurrences of Microcline
0.2km (0.1 miles) ⓘUndeland 13 Feldspar Quarry, Undeland, Evje og Hornnes, Agder, Norway
0.4km (0.2 miles) ⓘUndeland 06 Feldspar Quarry, Undeland, Evje og Hornnes, Agder, Norway
0.4km (0.2 miles) ⓘUndeland 01 Feldspar Quarry, Undeland, Evje og Hornnes, Agder, Norway
0.4km (0.3 miles) ⓘUndeland 12 Feldspar Prospect, Undeland, Evje og Hornnes, Agder, Norway
0.4km (0.3 miles) ⓘBjorland 1 Feldspar Quarry, Evje og Hornnes, Agder, Norway
0.4km (0.3 miles) ⓘUndeland 10 Feldspar Quarry, Undeland, Evje og Hornnes, Agder, Norway
0.5km (0.3 miles) ⓘUndeland 07 Feldspar Quarry, Undeland, Evje og Hornnes, Agder, Norway
0.5km (0.3 miles) ⓘUndeland 04 Feldspar Quarry, Undeland, Evje og Hornnes, Agder, Norway
0.5km (0.3 miles) ⓘUndeland 09 Feldspar Prospect, Undeland, Evje og Hornnes, Agder, Norway
0.8km (0.5 miles) ⓘUndeland, Evje og Hornnes, Agder, Norway
References
Schetelig, Jakob (1922) Thortveitit, Gadolinit, Kainosit und Orthit, in Die Mineralien der südnorwegischen Granitpegmatitgänge. II. Silikate der seltenen Erde (Y-reihe und Ce-reihe). Videnskapsselskapet i Kristiania Skrifter - I Matematisk-naturvidenskabelig klasse, 1922 (1). 49-138
 
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