(Sedl, Leckbachgraben (Leckbachrinne), Nasenkopf, Habachtal, Hohe Tauern, Salzburg, Österreich)
Mineralizations in ultrabasic rocks (rodingite, serpentinite), biotite schists and chlorite schists. Friedrichite was first discovered in sulphide-bearing quartzite boulders, which probably originate from the Leckbachscharte and were deposited at their present location by rockslides. This also compares well to a recent find in screes in the upper Leckbachgraben. However, friedrichite does possibly also occur as an associate of the sulphide mineralizations in rodingite.
Located a few hundred meters below the emerald deposit.
References:
- A. Strasser: Die Minerale Salzburgs (1989)
- Bayerl, R. (2004): Krupkait, ein Erstfund aus dem Habachtal. Lapis 29 (7-8), 54-56. (in German)
Mineral List:31 entries listed. 28 valid minerals. 1 type locality (valid mineral).
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