Indicators of former sea‐levels are recognised on the emergent portion of Lipari, Aeolian Islands. They correlate with three raised shorelines, located at elevations of 43–45 m above present sea‐level (I), 23–27 m (II) and about 12 m (III). According to stratigraphical constraints, these shorelines correlate with the sea‐level highstands corresponding to marine oxygen isotope substages 5e (124 ka), 5c (100 ka) and 5a (81 ka),...