Rollover Structure
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
June
2009
Submitted on Aug. 13, 2014
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Location
- Europe (3535)
- Western Europe (709)
- Germany (250)
- Exact location (9.8722 E, 51.9341 N)
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Canon PowerShot A2000 IS
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Credit: David Tanner (distributed via imaggeo.egu.eu)
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