Red triassic sandstone (Orcombe Rocks, East Devon)
by Sarah Weick, KIT, Germany
The three main horizons differ: the upper horizon and the lowest horizon are nearly horizontal while the layers in the centre are oblique and an excellent example of cross-bedding, where coarse material has cascaded down the foresets.
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4000 × 3000 px;
image/jpeg; 3.1 MB
Camera:
Canon Digital IXUS 200 IS
Taken on 21
September
2014
Submitted on 2 October 2014
Licence
Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported (CC BY-NC-ND 3.0)
Credit
Sarah Weick (distributed via imaggeo.egu.eu)
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