“…Importantly, some studies reported storm-generated features composed of sand or of coral debris (Scoffin, 1993;Morton et al, 2008;Caron, 2011), as illustrated by the remarkable storm rampart generated by TC Bebe in October 1972 on Funafuti, Tuvalu (Maragos et al, 1973;Baines et al, 1974;Baines and McLean, 1976). Furthermore, cyclonic waves can transfer sediments to inner land areas over great distances (Duvat and Pillet, 2017;Rey et al, 2017). For example, overwash processes led to the deposition of sand, coral debris and blocks over distances that reached up to 70 m from the pre-cyclone vegetation line on Tubuai and Reunion islands, respectively in 2010 (TC Oli; Etienne, 2012) and 2014 (TC Bejisa; .…”