Fig. 4From: Subaqueous morphology of Lake Lucerne (Central Switzerland): implications for mass movements and glacial historyShaded relief map of a part of the Weggis slide complex near Weggis village (see Fig. 1 for location). The inset map shows the identified morphological features: shaded exposed sliding surface below headwall; horizontally lined sediment slabs within transit area; solid lines on the basin plain—deformational bulges. The solid grey line descending on the slope denotes a glacial ridge. The dashed lines indicate the reflection seismic profiles shown on Fig. 5 Back to article page