Hohe Tauern window
id:
hohe-tauern-window-276-17336986
title:
Hohe Tauern window
text:
The Hohe Tauern window is a geological structure in the Austrian Central Eastern Alps. It is a window 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. 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 mo
brand slug:
wiki
category slug:
encyclopedia
description:
Austrian Central Eastern Alps region with exposed Penninic nappes
original url:
https://en.wikipedia.org/wiki/Hohe_Tauern_window
date created:
date modified:
2024-04-22T08:01:47Z
main entity:
{"identifier":"Q1983348","url":"https://www.wikidata.org/entity/Q1983348"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/1/10/Alps_geology_map_en.jpg","width":3338,"height":1607}
fields total:
13
integrity:
15