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About: Scarp retreat     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatEscarpments, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: yago:Escarpment109274152yago:GeologicalFormation109287968yago:Object100002684yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntityElectionyago:Slope109437454yago:WikicatEscarpments New Facet based on Instances of this Class

Scarp retreat is a geological process through which the location of an escarpment changes over time. Typically the cliff is undermined, rocks fall and form a talus slope, the talus is chemically or mechanically weathered and then removed through water or wind erosion, and the process of undermining resumes. Scarps may retreat for tens of kilometers in this way over relatively short geological time spans, even in arid locations.