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Escarpment

An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations.

Formation and description
, dip slopes facing left, and harder rocklayers in darker colors than softer ones Scarps are generally formed by one of two processes: by differential erosion of sedimentary rocks or by movement of the Earth's crust at a geologic fault. The former is the more common type: the escarpment is a transition from one series of sedimentary rocks to another series of a different age and composition. Escarpments are also frequently formed by faults. When a fault displaces the ground surface so that one side is higher than the other, a fault scarp is created. That can occur in dip-slip faults, a strike-slip fault that brings a piece of high ground adjacent to an area of lower ground. Earth is not the only planet with escarpments. They are believed to occur on other planets when the crust contracts, as a result of cooling. On other Solar System bodies such as Mercury, Mars, and the Moon, the Latin term rupes is used for an escarpment. ==Erosion==
Erosion
When sedimentary beds are tilted and exposed to the surface, erosion and weathering may occur. Escarpments erode gradually and over geological time. The mélange tendencies of escarpments results in varying contacts between a multitude of rock types. The different types of rock weather at different speeds, according to Goldich dissolution series, and so different stages of deformation can often be seen in the layers in which the escarpments have been exposed to the elements. ==See also==
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