Fig. 6From: Traces of a prehistoric and potentially tsunamigenic mass movement in the sediments of Lake Thun (Switzerland)Source of the digital elevation model: Swisstopo, Federal Office of TopographyOff- and on-shore thickness maps. a Off-shore thickness map of the seismic facies related to the rockslide-induced deposit (with basin plain sediments). The limits of the amphitheatre structure are shown with a black dashed line. b On-shore thickness map of the potentially terrestrial failed mass as the difference between the present and reconstructed topography. Negative thickness values are due to extrapolation uncertainties.Back to article page