{"refrec":{"BRefID":257716,"RR":"<b>Rodriguez-Vidal, J.; Caceres, L.; Abad, M.; Ruiz, F.; Gonzalez-Regalado, M.; Finlayson, C.; Finlayson, G.; Fa, D.; Rodríguez-Llanes, J.M.; Bailey, G.</b> (2011). The recorded evidence of AD 1755 Atlantic tsunami on the Gibraltar coast. <i>Journal of Iberian Geology 37(2)</i>: 177-193. <a href=\"http://dx.doi.org/10.5209/rev_JIGE.2011.v37.n2.7\" target=\"_blank\">dx.doi.org/10.5209/rev_JIGE.2011.v37.n2.7</a>","BEntID":249726,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Journal of Iberian Geology 37(2)</i>: 177-193. <a href=\"https://dx.doi.org/10.5209/rev_JIGE.2011.v37.n2.7\" target=\"_blank\">https://dx.doi.org/10.5209/rev_JIGE.2011.v37.n2.7</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Rodriguez-Vidal, J.; Caceres, L.; Abad, M.; Ruiz, F.; Gonzalez-Regalado, M.; Finlayson, C.; Finlayson, G.; Fa, D.; Rodríguez-Llanes, J.M.; Bailey, G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Rodriguez-Vidal, J. <i>et al.</i>","Englishabstract":"Evidence of the AD 1755 tsunami consisting of the same type of accretions produced by the re-deposition of earlier sediments, has been recorded at three different height along the coast of Gibraltar: Along a shallow sandy shore, the tsunami wave reached a run-up of 2-3 m, whereas along steep, cliff-lined shores (Rosia Bay) it surpassed 5 m. An overwash deposit was also identified at the bottom of a lagoon (The Inundation), at 0.5 m b.s.l., on the isthmus that joins the Rock with the mainland. Southern submerged platforms (Vladi's Reef) were also affected by the erosional backwash to a depth of 22 m. The tsunamigenic sediments exhibit a bimodal granulometry, mainly composed of sands with a coarser fraction composed of marine faunal shells remains, together with larger clasts derived from the rocky substrate. 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