Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8104
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dc.contributor.authorallBottari, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallUrbini, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallBianca, M.; Università della Basilicata, Dipartimento di Strutture, Geotecnica, Geologia applicata all'Ingegneria,en
dc.contributor.authorallD'Amico, M.; Università di Messina, Osservatorio sismologicoen
dc.contributor.authorallMarchetti, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallPizzolo, F.; Università di Messina, Osservatorio sismologicoen
dc.date.accessioned2012-10-09T09:08:05Zen
dc.date.available2012-10-09T09:08:05Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/8104en
dc.description.abstractIn recent years, detailed geoarcheological investigations have been carried out to search for traces of the ancient Tindari harbor (north-east Sicily, Italy). A digital terrain model supported the hypothesis that 2,000 yr ago the Oliveri Basin was a suitable landing place that was protected from prevailing winds. This model was generated from uplift data, sea level changes, historical cartographic data and three-dimensional reconstruction of the sedimentary succession of the cover. The present position of some historical buildings represent an archeological marker of the shoreline progression. Recent excavations during the construction of the Messina-to-Palermo motorway brought to light some portions of an ancient archeological complex. The thickness of the walls and the volume of the collected archeological material suggests dating between the 1st century BC and the 4th century AD. After that time, heavy environmental changes due to human activities in the area led to inaccurate underestimation of the role of Tindari harbor in the past. A geophysical investigation was carried out in the area surrounding the archeological complex to search for new buried structures related to the ancient settlement, and to be open to any results of the paleotopographic reconstruction of the area. The applied geophysical techniques included passive seismic and ground-penetrating radar. This survey indicates the presence of buried structures, such as walls and floors, that probably belong to a Roman villa. Furthermore, it defines the depth of the Holocene sedimentary cover of the Oliveri coastal plain, which strengthens the hypothesis formulated for its morphological evolution.en
dc.language.isoEnglishen
dc.publisher.nameIstituto Nazionale di Geofisica e Vulcanologiaen
dc.relation.ispartofAnnals of Geophysicsen
dc.relation.ispartofseries2/55 (2012)en
dc.subjectBuried harbor structures, Geophysical investigation, Horizontal-to-vertical spectra ratio method, Stratigraphy, Digital terrain modelen
dc.titleBuried archeological remains connected to the Greek-Roman harbor at Tindari (north-east Sicily): results from geomorphological and geophysical investigationsen
dc.title.alternativeGEOPHYSICAL INVESTIGATIONS AT TINDARIen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlUnreferreden
dc.description.pagenumber223-234en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.99. General or miscellaneousen
dc.identifier.doi10.4401/ag-4656en
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorBottari, C.en
dc.contributor.authorUrbini, S.en
dc.contributor.authorBianca, M.en
dc.contributor.authorD'Amico, M.en
dc.contributor.authorMarchetti, M.en
dc.contributor.authorPizzolo, F.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentUniversità della Basilicata, Dipartimento di Strutture, Geotecnica, Geologia applicata all'Ingegneria,en
dc.contributor.departmentUniversità di Messina, Osservatorio sismologicoen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentUniversità di Messina, Osservatorio sismologicoen
item.openairetypearticle-
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 OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptUniversità della Basilicata, Dipartimento di Strutture, Geotecnica, Geologia applicata all'Ingegneria,-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptUniversità di Messina, Osservatorio sismologico-
crisitem.author.orcid0000-0003-4371-6060-
crisitem.author.orcid0000-0002-8053-4197-
crisitem.author.orcid0000-0002-1677-1294-
crisitem.author.orcid0000-0002-9476-206X-
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.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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