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In physical geography and geology, a horst is a raised fault block bounded by normal faults. Horsts are typically found together with grabens . While a horst is lifted or remains stationary, the grabens on either side subside . [2]
A horst is a block of the earth's crust separated by faults from adjacent relatively depressed blocks. Learn the etymology, first known use, and examples of horst from Merriam-Webster dictionary.
Horst é a designação dada em geologia estrutural e em geografia física a um bloco de território elevado em relação ao território vizinho, devido ao movimento combinado de placas geológicas paralelas, cujo movimento provoca o rebaixamento de terrenos vizinhos de elevação de uma faixa de elevação entre elas.
A horst is a section of crust that has been lifted relative to the blocks on either side, which is a result of its bounding faults dipping away from each other. Horsts can form features such as plateaus, mountain ranges or ridges on either side of the valleys.
Horst and graben are elongate fault blocks of the Earth's crust that have been raised and lowered, respectively, by faulting. Learn about their formation, features, and examples, such as the Jordan–Dead Sea depression and the Vosges Mountains.
- The Editors of Encyclopaedia Britannica
A usually elongated block of rock that is bounded by parallel geologic faults along its two longest sides and has a higher elevation than the rock at its sides. Horsts form where rock is being compressed by tectonic forces.
A horst is a fault block that has been raised relative to the blocks on either side without major tilting or folding. Learn about the general features, origin, and references of horsts from this reference work entry by David L. Giles.
