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Flirsch ski hut, Flirsch, Stanz valley, North Tyrol, Tyrol, Austria

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Latitude & Longitude (WGS84): 47° 8' 56'' North , 10° 26' 36'' East
Latitude & Longitude (decimal): 47.14889,10.44361
Köppen climate type:Dfc : Subarctic climate
Name(s) in local language(s):Flirscher Skihütte, Flirsch, Stanzer Tal, Nordtirol, Tirol, Österreich
Other regions containing this locality:The Alps, Europe


Minor hydrothermal fahlore mineralisation in alpine sandstone/quartzite ('Alpiner Buntsandstein') about 30 m above the Flirsch ski hut (1872 m).
Small, 3 m long adit and outcrop (high rock wall).

Mineral List


37 valid minerals.

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Unknown
Ma



ID: 2347668
Metamorphe Gesteine, meist Metasedimente

Age: Anthropocene ( Ma)

Lithology: Metamorphic rocks, mostly metasedimentary

Reference: Geological Institute. Geological Map of Switzerland 1:500,000. isbn: 3906723399. University of Bern. [49]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

- Vohryzka, K. (1968): Die Erzlagerstätten von Nordtirol und ihr Verhältnis zur alpinen Tektonik. Jb. Geol. B.-A., 111, 3-88.
- KRAINER, K. (1982): Zur Sedimentologie und Vererzung der "Hangendquarzite" im Stanzer Tal / Arlberg (Tirol). Geol. Paläontol. Mitteilungen, Innsbruck, 12, 81-94.
- MOSTLER, H., KRAINER, K. & STINGL, V. (1982): Erzlagerstätten in der postvariszischen Trangressionsserie im Arlberggebiet. Arch. f. Lagerstättenforsch. Geol. B.-A., 2, 131-136.
- STINGL, V. (1982): Sedimentologie und Vererzung des Alpinen Verrucano im Stanzertal (Tirol). Geol. Paläont. Mitt. Innsbruck, 12, 71-80.
- HADITSCH, J. G. & KRAINER, K. (1993): Permoskytische Sandsteinvererzungen aus den Ost- und Südalpen Österreichs. Arch. f. Lagerstättenforsch. Geol. B.-A., 16, 13-28.
- J. Gröbner, U. Kolitsch, R. Poeverlein & M. Strasser (2009): Ein ungewöhnliches Fahlerzvorkommen bei der Flirscher Schihütte im Stanzer Tal, Tirol. Lapis 34, 13-19; 58.

Mineral and/or Locality  
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