Fault scarp
Small vertical offset on the ground surface / From Wikipedia, the free encyclopedia
A fault scarp is a small step-like offset of the ground surface in which one side of a fault has shifted vertically in relation to the other.[1][2] The topographic expression of fault scarps results from the differential erosion of rocks of contrasting resistance and the displacement of land surface by movement along the fault.[3][4] Differential movement and erosion may occur either along older inactive geologic faults, or recent active faults.[5][6][7]
An eroded fault scarp from the Gobi Desert of Mongolia (left) and at Borah Peak in Idaho. The latter fault scarp (white line at the base of the tan hills) was formed in the 1983 Borah Peak earthquake