Rollover Structure
by David Tanner, LIAG Institute for Applied Geophysics, 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.
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Location
- Europe (3876)
- Western Europe (787)
- Germany (264)
- Exact location (9.8722 E, 51.9341 N)
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3648 × 2736 px;
image/jpeg; 6.5 MB
Camera:
Canon PowerShot A2000 IS
Taken on 5
June
2009
Submitted on 13 August 2014
Licence
Creative Commons Attribution-NonCommercial 3.0 Unported (CC BY-NC 3.0)
Credit
David Tanner (distributed via imaggeo.egu.eu)
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