“…When considering tsunami risk, communities along active margins, such as the Cascadian, Alaskan, and Japanese margins, are typically considered to be at higher risk than passive margin communities (Lemke, 1967;Von Huene and Lallemand, 1990;Bardet et al, 2003;Finn, 2003;Yalçıner et al, 2003;Bondevik et al, 2005;Fine et al, 2005;Bernard et al, 2006;Hornbach et al, 2007;Mcadoo et al, 2008;Tappin et al, 2008;Moscardelli et al, 2010b;Garces et al, 2010;Loveless and Meade, 2010;Harbitz et al, 2014a;Scholz et al, 2016;Fujiwara et al, 2017;Strasser et al, 2019;Imai et al, 2019;Goda et al, 2019;Sun and Leslie, 2020;Ikehara et al, 2021;Matti et al, 2023). However, tsunamigenic landslides occur along passive margins, and these failures are generally larger than on active margins and can generate large tsunamis (Kvalstad et al, 2005;Urlaub et al, 2012;Harbitz et al, 2014a;Løvholt et al, 2019;Paris et al, 2019).…”