Funnel
by David Tanner, LIAG Institute for Applied Geophysics, Hannover, Germany
This funnel in glacial sands is caused by dewatering of the lower layer (along the thin pipe) and collapse of the top layer. Typically this process is due to sesimicity when material is still unconsolidated. Funnel is 15 cm wide at the top.
Categories
- Field (2899)
- Stratigraphy, Sedimentology and Palaeontology (529)
- Tectonics and Structural Geology (585)
Location
- Europe (3893)
- Western Europe (788)
- Germany (265)
- Exact location (9.6901 E, 51.8558 N)
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3648 × 2736 px;
image/jpeg; 9.2 MB
Camera:
Canon PowerShot A2000 IS
Taken on 5
June
2009
Submitted on 18 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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