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Fig. 2 | Swiss Journal of Geosciences

Fig. 2

From: Subaqueous landslide-triggered tsunami hazard for Lake Zurich, Switzerland

Fig. 2

Zones with a high failure probability upon earthquake occurrence (PoFeo) and corresponding potential failure depths for peak ground accelerations with an exceedance period in 50 years of a 10%, b 2% and c 0.5% (Strupler et al. 2018). Slopes < 1° are here considered stable (to avoid large unstable volumes on the terraces of the escarpment structure), although the model of Strupler et al. (2018) considers such slopes (i.e., > 0.01°–1°) as unstable for strong earthquake accelerations, such as assumed for an EP50 of 0.5%

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