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- Horst and graben | Faulting, Tectonics & Geomorphologygraben. horst and graben, elongate fault blocks of the Earth’s crust that have been raised and lowered, respectively, relative to their surrounding areas as a direct effect of faulting. Horsts and grabens may range in size from blocks a few centimetres wide to tens of kilometres wide; the vertical movement may be up to several thousand feet.
- Horst | SpringerLinkA horst is a fault block, generally elongate, that has been raised relative to the blocks on either side without major tilting or folding. The bordering faults, or fault zones, are usually of near-parallel strike and are steeply dipping, along which the vertical displacement has been approximately equal. Although horsts vary greatly in size ...
- Horst and graben - WikipediaHorst and graben. In geology, horst and graben (or range and valley) refers to topography consisting of alternating raised and lowered fault blocks known as horsts and grabens. The features are created by normal faulting and rifting caused by crustal extension. [1] Horst and graben are formed when normal faults of opposite dip occur in pairs ...
- How do horsts form? | AZGSThe rocks of Earth's crust accommodates extension by breaking into discreet blocks along planes of weakness - fault s. With extension, alternating blocks (graben) physically subside while the intervening blocks remain in place, but are now relatively higher than the grabens. Arrows along the faults illustrate the 'relative' motion of the block ...
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