Fig. 9
(adapted from Leithold et al., 2019)
Maximum run-up height Rmax versus landslide volume \(\rlap{--} V_{s}\). Data are composed of Lake Thun mass movement (grey: Rmax = 34…84 m, \(\rlap{--} V_{s}\) = 20 × 106 … 35 × 106 m3; dotted) and historical cases as compiled by Clark et al. (2015) and Leithold et al. (2019) including (1) Haeussler et al., (2018), (2) Evans (1989), (3) Hancox et al., (2003), (4) Hansen et al., (2016), (5) Jørstad (1968), (6) Miller (1960), (7) Naranjo et al., (2009), (8) Norwegian Water Resources and Energy Directorate (2016), (9) Roberts et al., (2013), (10) Watt et al., (2009), (11) Wiles and Calkin (1992), (12) Zaniboni and Tinti (2014)