Rollover Structure
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.
Reuse
Creative Commons Attribution-NonCommercial 3.0 Unported (CC BY-NC 3.0) (opens in a new window)Credit: David Tanner (distributed via imaggeo.egu.eu)
Properties
Type
Image
Format
JPG
Size
6.5 MB
Width
3648 px
Height
2736 px
Aspect
4:3
Brand
Canon
Model
PowerShot A2000 IS
Exposure
8 mm f/3.5 1/500 s ISO 80
Taken
5 June 2009
Coordinates
51.9341, 9.8722
Tint
Dark grayish yellow
Submitted
13 August 2014
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