Parallel retreat of rock slopes underlain by alternation of strata
Characteristic landscapes (e.g., cuesta, cliff and overhang of caprock, or stepped terrain) formed by differential erosion can be found in areas composed of variable geology exhibiting different resistances to weathering. Parallel retreat of slopes, defined as recession of slopes without changes in...
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Published in | Geomorphology (Amsterdam, Netherlands) Vol. 238; pp. 27 - 36 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.06.2015
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Subjects | |
Online Access | Get full text |
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