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dc.rights.licenseopenen_US
hal.structure.identifierLIttoral ENvironnement et Sociétés [LIENSs]
dc.contributor.authorRIOU, Brieuc
hal.structure.identifierLIttoral ENvironnement et Sociétés [LIENSs]
dc.contributor.authorCHAUMILLON, Eric
hal.structure.identifierSchool of Biological, Earth and Environmental Sciences [Sydney] [BEES]
dc.contributor.authorCHAGUÉ, Catherine
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCORREGE, Thierry
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorBUJAN, Stephane
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHNEIDER, Jean-Luc
dc.date.accessioned2025-04-04T12:19:59Z
dc.date.available2025-04-04T12:19:59Z
dc.date.issued2024-01-05
dc.identifier.issn0037-0738en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/205980
dc.description.abstractEnAlthough research dealing with the geological evidence of past tsunamis has increased significantly in the last two decades, studies of tsunami deposits emplaced during the backwash phases are still underrepresented. Here, we provide the first investigation of tsunami backwash deposits all around an island (Tutuila Island, American Samoa), in the southwest of the Pacific Ring of Fire. We decipher the sedimentary record preserved offshore an open bay (Fagafue) and within a sheltered bay (Masefau) on the north shore of Tutuila. Backwash deposits of three historic tsunamis, namely the 2009 South Pacific, 1960 Valdivia and 1917 Tonga Trench tsunamis, were identified in sediment cores, based on sedimentological, geochemical and chronological data. Deposits were characterized by a geochemical terrestrial signature (Ti/Ca and K), while the grain size characteristics differed, being finer offshore the open bay and coarser within the sheltered bay. The 2009 South Pacific and the 1960 Valdivia tsunamis are recorded on both the north (Masefau and off Fagafue bays) and south (Pago Pago Bay) shores of Tutuila, providing the first correlation of tsunami backwash deposits all around an island. Furthermore, the present study presents the first geological evidence of backwash associated with a large 15-16th century tsunami, which also affected many parts of the South Pacific, as well as that of an older event between the 11th and 14th century. Studies of tsunami backwash deposits provide means to extend the geological record of these high energy events, due to the generally good preservation potential of the deposits.
dc.language.isoENen_US
dc.subject.enTsunami
dc.subject.enBackwash deposit
dc.subject.enCore correlation
dc.subject.en15th century tsunami
dc.subject.enEvidence of local and far-field tsunamis
dc.title.enOffshore evidence of historic and prehistoric tsunamis on the north shore of Tutuila (American Samoa)
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.sedgeo.2023.106572en_US
dc.subject.halSciences de l'environnementen_US
dc.subject.halPlanète et Univers [physics]en_US
bordeaux.journalSedimentary Geologyen_US
bordeaux.page106572en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04393934
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Sedimentary%20Geology&rft.date=2024-01-05&rft.spage=106572&rft.epage=106572&rft.eissn=0037-0738&rft.issn=0037-0738&rft.au=RIOU,%20Brieuc&CHAUMILLON,%20Eric&CHAGU%C3%89,%20Catherine&SCHMIDT,%20Sabine&CORREGE,%20Thierry&rft.genre=article


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