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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.

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  • Bratschen (de)
  • Bratschen (en)
  • Bratschen (pt)
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  • Bratschen sind Verwitterungsformen, die durch Frost und äolische Auswehung fast ausschließlich auf den Kalkglimmerschiefer der in den Hohen Tauern entstehen.Der Kalkglimmerschiefer, der im frischen Bruch blaugrau ist, verwittert gelb bis braun und zerblättert oberflächlich eben zu den Bratschen.Diese bilden bis zu 40° steile, felsige und kaum bewachsene Bergflanken mit einer eigenartigen, in der Winderosion begründeten, rauen Oberfläche. Bratschen finden sich z. B. am Fuscherkarkopf, den Bärenköpfen, am Kitzsteinhorn, am oder an den – danach heißenden – Bratschenköpfen. (de)
  • 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. (en)
  • Bratschen (empréstimo do alemão) são materiais meteorizados que ocorrem como resultado da de eólica quase que exclusivamente nos calcoxistos do Manto de Ardósia Superior (Obere Schieferhülle) nas montanhas do , na Áustria. (pt)
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  • 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. (en)
  • Bratschen sind Verwitterungsformen, die durch Frost und äolische Auswehung fast ausschließlich auf den Kalkglimmerschiefer der in den Hohen Tauern entstehen.Der Kalkglimmerschiefer, der im frischen Bruch blaugrau ist, verwittert gelb bis braun und zerblättert oberflächlich eben zu den Bratschen.Diese bilden bis zu 40° steile, felsige und kaum bewachsene Bergflanken mit einer eigenartigen, in der Winderosion begründeten, rauen Oberfläche. Bratschen finden sich z. B. am Fuscherkarkopf, den Bärenköpfen, am Kitzsteinhorn, am oder an den – danach heißenden – Bratschenköpfen. (de)
  • Bratschen (empréstimo do alemão) são materiais meteorizados que ocorrem como resultado da de eólica quase que exclusivamente nos calcoxistos do Manto de Ardósia Superior (Obere Schieferhülle) nas montanhas do , na Áustria. O calcoxisto, que possui uma aparência azul-esverdeada quando quebrado, meteoriza para uma cor amarela ou marrom e se fragmenta na superfície formando o Bratschen.Os bratschen formam desfilareiros íngremes (possuindo inclinação maior que 40°), rochosos, e quase sem vegetação, com uma superfície áspera, causada pela erosão do vento. Bratschen são encontrados nas montanhas , , , Schwerteck, ou na epônima – . (pt)
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