Vote for your favorite mineral in #MinCup26! - Sphalerite vs. Anorthite
Both zinc ore Sphalerite and calcium plagioclase feldspar Anorthite have perfect cleavage that will split cleanly if you hit them with a hammer, but only one can claim a larger split of your votes!
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Epididymite from
Husebyåsen prospect, Vesterøya, Sandefjord, Vestfold, Norway


Locality type:Prospect
Classification
Species:Epididymite
Formula:Na2Be2Si6O15 · H2O
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Epididymite data
Locality Data:Click here to view Husebyåsen prospect, Vesterøya, Sandefjord, Vestfold, Norway
Data Identifiers
Mindat Occurrence Record ID:255407
Long-form Identifier:1:3:255407:5
GUID (UUID V4):0
Nearest other occurrences of Epididymite
0.2km (0.1 miles) ⓘKariåsen, Vesterøya, Sandefjord, Vestfold, Norway
1.5km (0.9 miles) ⓘBuer, Vesterøya, Sandefjord, Vestfold, Norway
4.4km (2.7 miles) ⓘVøra, Vesterøya, Sandefjord, Vestfold, Norway
11.3km (7.0 miles) ⓘHedrum Quarry, Lågendalen, Hedrum, Larvik Commune, Vestfold, Norway
14.3km (8.9 miles) ⓘBratthagen 1, Lågendalen, Hedrum, Larvik Commune, Vestfold, Norway
17.7km (11.0 miles) ⓘVardåsen Quarry, Malerød, Larvik Commune, Vestfold, Norway
18.0km (11.2 miles) ⓘMidtfjellet Quarry, Malerød, Larvik Commune, Vestfold, Norway
18.6km (11.6 miles) ⓘBakkane Quarry, Brunlanes, Larvik Commune, Vestfold, Norway
19.5km (12.1 miles) ⓘJahrehagen cottage grounds, Jahren pegmatite, Stavern (Fredriksvärn), Larvik Commune, Vestfold, Norway
19.5km (12.1 miles) ⓘJahren pegmatite, Stavern (Fredriksvärn), Larvik Commune, Vestfold, Norway
References
Engvoldsen, Tom, Andersen, Frode, Berge, Svein A., Burvald, Ingulv (1991) Pegmatittmineraler fra Larvik ringkompleks [Pegmatite minerals from the Larvik ring complex], in Mineraler fra Larvikittområdet. STEIN. Nordisk magasin for populær geologi, 18 (1) 15-71
Berge, Svein Arne (2013) Mineralene i Husebyåsen feltspatbrudd, Vesterøya, Sandefjord [The minerals of Husebyåsen feldspar quarry, Vesterøya, Sandefjord]. Norsk Bergverksmuseum Skrift, 50. 93-99
 
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