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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10396
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dc.contributor.authorallSulpizio, R.; Dipartimento Geomineralogico, Università di Bari, via Orabona 4, 70100 Bari, Italyen
dc.contributor.authorallZanchetta, G.; Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 56, 56126 Pisa, Italyen
dc.contributor.authorallDemi, F.; Istituto di Geoscienze e Georisorse—CNR, via Moruzzi 1, 56100 Pisa, Italyen
dc.contributor.authorallDi Vito, M. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallPareschi, M. T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallSantacroce, R.; Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 56, 56126 Pisa, Italyen
dc.date.accessioned2016-11-21T10:04:43Zen
dc.date.available2016-11-21T10:04:43Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/10396en
dc.description.abstractVolcaniclastic debris fl ows generated in drainage basins of the Apennine mountains of southern Campania in response to pyroclastic fall deposition from four Holocene eruptions of Somma-Vesuvius: Avellino (3.8 ka), A.D. 79, A.D. 472, and A.D. 1631. These syneruptive debris fl ows are lithologically homogeneous and contain more than 90% of material from the parental eruption. They differ from inter-eruptive debris fl ows recognized in the area, which contain mixed lithologies of juvenile material (i.e., volcanic material from different eruptions). Diffuse rill erosion generated fi nesrich volcaniclastic fl ows (mudfl ows), whereas partial saturation of coarse ash and lapilli generated coarser-grained debris fl ows. Lithofacies analysis shows that debris fl ows predominate versus hyperconcentrated fl ows and normal stream-fl ow deposits. Debris-fl ow deposits are massive, matrix supported, and have a gravelly-sandy texture. Large blocks are scarce due to their absence in the pyroclastic source material. Lithofacies association indicates that volcaniclastic debris-fl ow deposits aggraded rapidly by superimposition of different surges that spontaneously developed within the fl ow. Bulk-fl ow density ranges from 1840 to 2260 kg/m3 (mean 2035 ± 207 kg/m3). Geological data supported some considerations of hazard assessment in the study area and indicate that the syneruptive volcaniclastic fl ows stopped distally on active alluvial fans.en
dc.language.isoEnglishen
dc.publisher.nameGeological Society of Americaen
dc.relation.ispartofGeological Society of America Special Papersen
dc.relation.ispartofseries/402(2006)en
dc.subjectvolcanic hazarden
dc.subjectvolcaniclastic debris fl owen
dc.subjectvolcaniclastic sedimentationen
dc.subjectHoloceneen
dc.titleThe Holocene syneruptive volcaniclastic debris fl ows in the Vesuvian area: Geological data as a guide for hazard assessmenten
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber217-235en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneousen
dc.identifier.doi10.1130/2006.2402(10)en
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dc.description.obiettivoSpecifico1V. Storia e struttura dei sistemi vulcanicien
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextrestricteden
dc.relation.issn0072-1077en
dc.contributor.authorSulpizio, R.en
dc.contributor.authorZanchetta, G.en
dc.contributor.authorDemi, F.en
dc.contributor.authorDi Vito, M. A.en
dc.contributor.authorPareschi, M. T.en
dc.contributor.authorSantacroce, R.en
dc.contributor.departmentDipartimento Geomineralogico, Università di Bari, via Orabona 4, 70100 Bari, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 56, 56126 Pisa, Italyen
dc.contributor.departmentIstituto di Geoscienze e Georisorse—CNR, via Moruzzi 1, 56100 Pisa, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 56, 56126 Pisa, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptCIRISIVU, c/o Dipartimento Geomineralogico, Universita' di Bari-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pisa-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Pisa, Italy-
crisitem.author.orcid0000-0002-3930-5421-
crisitem.author.orcid0000-0002-7080-9599-
crisitem.author.orcid0000-0002-7913-9149-
crisitem.author.orcid0000-0001-7424-8429-
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-
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