Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7445
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dc.contributor.authorallDe Martini, Paolo Marco; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallSmedile, Alessandra; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallPantosti, Daniela; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.editorallBriand, Frédréricen
dc.date.accessioned2012-01-22T19:39:11Zen
dc.date.available2012-01-22T19:39:11Zen
dc.date.issued2011-02-02en
dc.identifier.urihttp://hdl.handle.net/2122/7445en
dc.description.abstractWe present the geological evidence for a 4000 year-long record of repeated tsunami events along the coast of the Augusta Bay derived from the combination of inland and offshore cores data. The research was carried out through a multi-theme approach which benefited from an long historical record that we used to guide detailed geomorphologic, geologic, and geophysical surveys,that were performed both inland and offshore. These surveys served to locate and characterize the best sites were to perform the coring collection that where studied through and several laboratory analyses. The Augusta Bay represents a unique case study because besides showing a long record of paleotsunami events, it contains the first inland and offshore evidence for the Crete AD 365, and Santorini Late Minoan tsunamis in the central-western Mediterranean area.en
dc.language.isoEnglishen
dc.publisher.nameCIESM, Monacoen
dc.relation.ispartofCIESM, 2011- Marine geo-hazards in the Mediterraneanen
dc.subjecttsunami depositsen
dc.subjectEastern Sicilyen
dc.titleCombining inland and offshore paleotsunamis evidence: the Augusta Bay (eastern Sicily, ITALY) case studyen
dc.typeConference paperen
dc.description.statusPublisheden
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismologyen
dc.description.ConferenceLocationNicosia (Cipro)en
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.fulltextopenen
dc.contributor.authorDe Martini, Paolo Marcoen
dc.contributor.authorSmedile, Alessandraen
dc.contributor.authorPantosti, Danielaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.editorBriand, Frédréricen
item.openairetypeConference paper-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-3598-5191-
crisitem.author.orcid0000-0002-2938-4816-
crisitem.author.orcid0000-0001-7308-9104-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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