Fig. 8From: Subaqueous morphology of Lake Lucerne (Central Switzerland): implications for mass movements and glacial historyReflection seismic profiles (pinger source) across “Nase moraine” (left) and “Chindli moraine” (right; see Fig. 7 for locations). Note the asymmetric distribution of the postglacial sedimentary drape. Vertical scales correspond to a sound velocity of vP = 1,500 m/sBack to article page