“…Determining rates of occurrence tends to be more problematic for nonearthquake sources compared with earthquake sources because they often lack any clear time dependence, and source mechanisms can be strongly nonlinear. Probabilistic hazard assessments of tsunamis from submarine mass failures, some including the potential for earthquake triggering, have been undertaken for the U.S. Atlantic (Geist & Parsons, 2010;Grilli et al, 2009;Lynett & Martinez, 2012;Maretzki et al, 2007;ten Brink et al, 2009ten Brink et al, , 2014 and Pacific margins (Watts, 2004), the Canadian coast (Leonard et al, 2014), New Zealand coasts (Lane, Mountjoy, Power, & Mueller, 2016), and the Tyrrhenian Sea (e.g., Grezio et al, 2012Grezio et al, , 2015. Probabilistic analysis of meteotsunamis were introduced by and Šepić, Medugorac, et al (2016) for the northeast U.S. coastlines and the Balearic Islands, Spain, respectively.…”