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Home > Horst


 

In physical geography and geology, a horst is the term used for a block of the earth's crust that has remained stationary while the land has sunk on either side of it, or has been crushed n a mountain range against it.

The Vosges and Black Forest are examples of the former, the Table, Jura and the Dôle of the latter result. The word is also applied to those larger areas, such as the Russian plain, Arabia, India and Central South Africa, where the continent remains stable, with horizontal table-land stratification, in distinction to folded regions such as the Eurasian chains.

This article incorporates text from the public domain 1911 Encyclopædia Britannica. 1911 Britannica

Geology

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