“…The Elafiti Islands form a chain of islands and islets (Šipan Island, Koločep Island, Lopud Island, Jakljan Island, Olipa Island, Tajan Islet, Crkvina Islet, Ruda Islet, Kosemč Islet, and Ruda Islet) that extend in a NW-SE direction. The wider region is tectonically active and characterized by moderate-to-strong earthquakes [14,25,26]. One of the most widespread and successful research methods in the study of the Quaternary sediment successions is the application of acoustic mapping techniques using a sub-bottom profiler [29][30][31][32].…”