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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Serpentine Subgroup from
Almklovdalen, Vanylven, Møre og Romsdal, Norway


07557160017362273008358.jpg
Antigorite, etc.

Gusdal Olivine Pit, Almklovdalen, Vanylven, Møre og Romsdal, Norway
07557160017362273008358.jpg
Antigorite, etc.

Gusdal Olivine Pit, Almklovdalen, Vanylven, Møre og Romsdal, Norway
02144780017272728563601.jpg
Antigorite, etc.

Gusdal Olivine Pit, Almklovdalen, Vanylven, Møre og Romsdal, Norway
Locality type:Valley
Classification
Species:'Serpentine Subgroup' (not an IMA approved species)
Formula:D3[Si2O5](OH)4
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Serpentine Subgroup data
Locality Data:Click here to view Almklovdalen, Vanylven, Møre og Romsdal, Norway
Data Identifiers
Mindat Occurrence Record ID:697169
Long-form Identifier:1:3:697169:4
GUID (UUID V4):0
Localities for Serpentine Subgroup in this Region
Gusdal Olivine Pit (Åheim Olivine Pit), Almklovdalen, Vanylven, Møre og Romsdal, Norway
Nearest other occurrences of Serpentine Subgroup
0.4km (0.3 miles) ⓘGusdal Olivine Pit (Åheim Olivine Pit), Almklovdalen, Vanylven, Møre og Romsdal, Norway
18.1km (11.3 miles) ⓘKleberga Serpentine Deposits, Bremanger, Vestland, Norway
25.8km (16.0 miles) ⓘDeknepollen, Vågsøy, Kinn, Vestland, Norway
95.1km (59.1 miles) ⓘUglvik peridotite body, Uglvik, Otrøya, Midsund, Molde, Møre og Romsdal, Norway
References
Kostenko, O., ,Jamtveit, Bjørn, Austrheim, H., Pollok, K., Putinis, C. (2002) The mechanism of fluid infiltration in peridotites at Almklovdalen, western Norway. Geofluids, 2. 203-215 doi:10.1046/j.1468-8123.2002.00038.x
 
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