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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Ilmenite from
Fjällbacka, Tanum, Västra Götaland County, Sweden


Classification
Species:Ilmenite
Formula:Fe2+TiO3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Ilmenite data
Locality Data:Click here to view Fjällbacka, Tanum, Västra Götaland County, Sweden
Data Identifiers
Mindat Occurrence Record ID:1245443
Long-form Identifier:1:3:1245443:5
GUID (UUID V4):0
Nearest other occurrences of Ilmenite
54.8km (34.1 miles) ⓘThe monolith quarry, Idd, Halden, Østfold, Norway
77.6km (48.2 miles) ⓘKjela, Yxney, Østerøya, Sandefjord, Vestfold, Norway
79.8km (49.6 miles) ⓘTveitan, Vesterøya, Sandefjord, Vestfold, Norway
82.6km (51.3 miles) ⓘØsterøyveien, Søndre Sunde, Østerøya, Sandefjord, Vestfold, Norway
83.4km (51.8 miles) ⓘKariåsen, Vesterøya, Sandefjord, Vestfold, Norway
84.4km (52.5 miles) ⓘKamfjord Quarry, Vesterøya, Sandefjord, Vestfold, Norway
85.0km (52.8 miles) ⓘVadholmen, Fredriksvern Verft, Stavern (Fredriksvärn), Larvik Commune, Vestfold, Norway
85.6km (53.2 miles) ⓘHjertnesåsen (Ranvikmyra), Sandefjord, Vestfold, Norway
86.5km (53.7 miles) ⓘJahren Feldspar Quarry (Jaren Feldspar Quarry), Jahren pegmatite, Stavern (Fredriksvärn), Larvik Commune, Vestfold, Norway
86.5km (53.7 miles) ⓘJahrehagen cottage grounds, Jahren pegmatite, Stavern (Fredriksvärn), Larvik Commune, Vestfold, Norway
References
Petersson, Jesper, Eliasson, Thomas (1997) Mineral evolution and element mobility during episyenitization (dequartzification) and albitization in the postkinematic Bohus granite, southwest Sweden. Lithos, 42 (1) 123-146 doi:10.1016/s0024-4937(97)00040-6
Petersson, Jesper, Fallick, Anthony E., Broman, Curt, Eliasson, Thomas (2014) Imprints of multiple fluid regimes on episyenites in the Bohus granite, Sweden. Lithos, 196. 99-114 doi:10.1016/j.lithos.2014.02.025
 
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