by David Tanner, Leibniz Institute for Applied Geophysics (LIAG), Hannover, Germany
In these unconsolidated Pleistocene glacial sands, faults are common. In this example, a listric fault causes strong rollover of the hanging-wall. Width of view ca. 25 cm.
Taken on 5
Submitted on 13 August 2014
Credit: David Tanner (distributed via imaggeo.egu.eu)
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