Fig. 7From: Subaqueous morphology of Lake Lucerne (Central Switzerland): implications for mass movements and glacial historyBathymetric maps (shaded relief, colour indicating depth) of a “Nase moraine” and b “Chindli moraine”, with visible erosional channels, a secondary crest (A), a fan-shaped deposit on the external slope (B) and traces of mass movements (e.g. C). Dashed white lines indicate location of seismic profiles in Fig. 8 Back to article page