Physical modelling of fault scarp degradation under freeze-thaw cycles
Physical modelling has been developed in order to simulate the effects of periglacial erosion processes on the degradation of slopes and scarps. Data from 41 experimental freeze–thaw cycles are presented. They attest to the efficiency of periglacial processes that control both erosion and changes in...
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Veröffentlicht in: | Earth surface processes and landforms 2006-12, Vol.31 (14), p.1731-1745 |
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Format: | Artikel |
Sprache: | eng |
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