by David Tanner, Leibniz Institute for Applied Geophysics (LIAG), Hannover, Germany
This harpoon structure is caused by inversion of normal fault movement on this listric fault in unconsolidated glacial sands. Trowel is 12cm long.
Taken on 5
Submitted on 13 August 2014
Credit: David Tanner (distributed via imaggeo.egu.eu)
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