Fig. 8From: The Oeschinensee rock avalanche, Bernese Alps, Switzerland: a co-seismic failure 2300 years ago? a Thickness of deposits calculated by subtracting the recreated base of slide surface from present-day topography. The deposit extent is outlined in orange, red line is the failure scarp. b Cross-section showing the modern and pre-failure topographies, and thickness of deposits and source along the main trajectory of runoutBack to article page