Playa system of the eastern Juyanze Basin
by Kaifeng Yu, RWTH Aachen University, Aachen, Germany
The former lacustrine sediments are deflated partically, rendering the formation of yardangs. Due to high salinity of the sediments, light color is commonly observed. Quasi-paralleled sand riples can be seen and dunes are accumulated at the down wind direction after the plants.
Taken on 25
Submitted on 27 February 2016
Credit: Kaifeng Yu (distributed via imaggeo.egu.eu)
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