Английская Википедия:Hohe Tauern window

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Версия от 09:55, 22 марта 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} {{Short description|Austrian Central Eastern Alps region with exposed Penninic nappes}} {{Refimprove|date=December 2009}} {{Geology of the Alps}} {{coord|47|00|N|12|30|E|region:AT_type:mountain_source:kolossus-dewiki|display=title}} The '''Hohe Tauern window''' is a geological structure in the Austrian Central Eastern Alps. It is a window (in German...»)
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The Hohe Tauern window is a geological structure in the Austrian Central Eastern Alps. It is a window (in German fenster) in the Austroalpine nappes where high-grade metamorphic rocks of the underlying Penninic nappes crop out. The structure is caused by a large dome-like antiform in the nappe stacks of the Alps.

Файл:Nationalpark Hohe Tauern - Gletscherweg Innergschlöß - 44 - Weg über den Gletscherschliff.jpg
Detersion of the Schlatenkees glacier on visible parts of the Hohe Tauern window

The relatively hard rocks of the Hohe Tauern window are more resistant to erosion, so the window has a high relief. The mountain chains thus formed are called the Hohe Tauern. Most of Austria's highest mountains are in the Hohe Tauern, among them the Großglockner (3798 m) and Großvenediger (3674 m).[1]

See also

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