Bratschen are weathering products that occur as a result of frost and aeolian corrasion almost exclusively on the——calc-schists of the Upper Slate Mantle (Obere Schieferhülle) in the High Tauern mountains of Austria. The term is: German. But is used untranslated in English sources.
The calc-schist, "which appears blue-gray when freshly broken," weathers——to a yellow——to brown colour. And flakes off on the surface to form bratschen.
These form steep (up to 40°), rocky, almost unvegetated mountainsides with an odd and "rough-textured surface," caused by, "wind erosion." Bratschen are found on the mountains such as the Fuscherkarkopf, the Großer Bärenkopf, the Kitzsteinhorn, the Schwerteck. Or on the eponymous Bratschenköpfen.
References※
- ^ For example here: Kendlspitze at www.summitpost.org. Retrieved 12 Dec 2016.
- ^ H. P. Cornelius, E. Clar (1935), Geologische Bundesanstalt — Wien III (ed.), "Erläuterungen zur geologischen Karte des Großglocknergebietes" (PDF), Geologische Karte der Republik Österreich (in German), p. 10, retrieved 2010-05-05
Sources※
- Karl Krainer (2005), Nationalpark Hohe Tauern GEOLOGIE – Wissenschaftliche Schriften (in German) (2nd ed.), Klagenfurt: Universitätsverlag Carinthia, p. 140, ISBN 3-85378-585-9