Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8212
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dc.contributor.authorallGerardi, F.; Università di Cataniaen
dc.contributor.authorallSmedile, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallPirrotta, C.; Università di Cataniaen
dc.contributor.authorallBarbano, M. S.; Università di Cataniaen
dc.contributor.authorallDe Martini, P. M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallPinzi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallGueli, A. M.; Università di Cataniaen
dc.contributor.authorallRistuccia, G. M.; Università di Cataniaen
dc.contributor.authorallStella, G.; Università di Cataniaen
dc.contributor.authorallTroja, S. O.; Università di Cataniaen
dc.date.accessioned2012-10-16T10:20:56Zen
dc.date.available2012-10-16T10:20:56Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/8212en
dc.description.abstractAnalysis of tsunami deposits from the Pantano Morghella area provided geological evidence for two inundations occurred along the south-eastern Ionian coast of Sicily. Pantano Morghella is a large pond characterised by a finegrained sedimentation indicating a low-energy depositional environment. Two anomalous yellow sandy layers found at different depths indicate the occurrence of high-energy marine inundations. We studied sedimentological and paleontological features of the anomalous deposits as well as their spatial distribution observing the following properties: different facies with respect to the local stratigraphic sequence; erosive bases, rip-up clasts and broken elements testifying violent deposition mechanisms; macro and micro fauna of marine environment; relatively constant thickness throughout most of the depositional zone with thinning at the distal end; large sand sheets that extend inland. These observations, jointly with their infrequency in the sedimentary record and the age indicating a fast deposition, provided strong evidence for tsunami inundations. Correlations between anomalous layers and historical tsunamis are supported by radiocarbon and OSL dating results. The younger deposit is likely due to the 1908 near-source tsunami, whereas the flooding of the oldest event is most likely associated with a far and large source, the Crete 365AD earthquake.en
dc.language.isoEnglishen
dc.publisher.nameCopernicus Publications on behalf of the European Geosciences Unionen
dc.relation.ispartofNatural Hazards and Earth System Sciencesen
dc.relation.ispartofseries/12 (2012)en
dc.subjectTsunami depositsen
dc.subject1908 AD tsunamien
dc.subject365 AD tsunamien
dc.subjectcoastal hazarden
dc.subjecteastern Sicilyen
dc.titleGeological record of tsunami inundations in Pantano Morghella (south-eastern Sicily) both from near and far-field sourcesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1185-1200en
dc.identifier.URLhttp://www.nat-hazards-earth-syst-sci.net/12/1185/2012/en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transporten
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.10. Stratigraphyen
dc.identifier.doi10.5194/nhess-12-1185-2012en
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorGerardi, F.en
dc.contributor.authorSmedile, A.en
dc.contributor.authorPirrotta, C.en
dc.contributor.authorBarbano, M. S.en
dc.contributor.authorDe Martini, P. M.en
dc.contributor.authorPinzi, S.en
dc.contributor.authorGueli, A. M.en
dc.contributor.authorRistuccia, G. M.en
dc.contributor.authorStella, G.en
dc.contributor.authorTroja, S. O.en
dc.contributor.departmentUniversità di Cataniaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniversità di Cataniaen
dc.contributor.departmentUniversità di Cataniaen
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.departmentUniversità di Cataniaen
dc.contributor.departmentUniversità di Cataniaen
dc.contributor.departmentUniversità di Cataniaen
dc.contributor.departmentUniversità di Cataniaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze Geologiche, Università degli Studi di Catania, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptDipartimento di Scienze Geologiche, Università di Catania, Catania, Italy-
crisitem.author.deptUniversità di Catania, Dip. Scienze Geologiche-
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.deptUniversità di Catania-
crisitem.author.deptUniversità di Catania-
crisitem.author.deptUniversità di Catania-
crisitem.author.deptUniversità di Catania-
crisitem.author.orcid0000-0002-2938-4816-
crisitem.author.orcid0000-0003-2407-3207-
crisitem.author.orcid0000-0002-3598-5191-
crisitem.author.orcid0000-0002-6068-1333-
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.classification.parent04. Solid Earth-
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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