Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/8152
DC Field | Value | Language |
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dc.contributor.authorall | Cubellis, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.authorall | Delizia, I.; Università di Napoli Federico II | en |
dc.contributor.authorall | Luongo, G.; Università di Napoli Federico II | en |
dc.contributor.authorall | Obrizzo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.editorall | Critelli, Salvatore | en |
dc.contributor.editorall | Muto, Francesco | en |
dc.contributor.editorall | Perri, Francesco | en |
dc.contributor.editorall | Petti, Fabio M | en |
dc.contributor.editorall | Sonnino, Maurizo | en |
dc.contributor.editorall | Zuccari, Alessandro | en |
dc.date.accessioned | 2012-10-11T09:38:14Z | en |
dc.date.available | 2012-10-11T09:38:14Z | en |
dc.date.issued | 2012-09-18 | en |
dc.identifier.uri | http://hdl.handle.net/2122/8152 | en |
dc.description.abstract | Ground deformations in active volcanoes are considered precursors of eruptions according to the most tested models; therefore monitoring networks of ground deformations are installed on inhabited dangerous volcanoes. Direct measurements of such deformations are carried out since 1861 when Luigi Palmieri monitored the eruption at Mt. Vesuvius with levelings along the shoreline near the town of Torre del Greco. Relative sea level changes were measured at Serapeo in Pozzuoli in the middle of 19th century to record soil uplifts which are locally known as bradyseism. To enlarge the time series of data on these phenomena it is necessary to utilize historical and prehistorical informations on the location of shore-line of human settlements. As regards the regions of active volcanoes as the Neapolitan one three processes contribute to sea level changes as eustatism, regional tectonics and local intrusive and effusive phenomena. Therefore at the same time the relative sea level should be different at far-away places only few kilometres according to the volcanic activity. In fact eustatic and tectonic processes contribute to sea level changes with very lesser rates than volcanic activity. The Neapolitan region for its geological history is an excellent laboratory for testing the validation of new paradigms for some natural phenomena. | en |
dc.language.iso | English | en |
dc.relation.ispartof | 86° Congresso Nazionale della Società Geologica Italiana | en |
dc.subject | Bay of Naples, Ground deformations, Human | en |
dc.title | Sea level changes, ground deformations, human settlements in the bay of Naples | en |
dc.type | Extended abstract | en |
dc.description.status | Published | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous | en |
dc.identifier.doi | ISSN 2035-8008 | en |
dc.description.ConferenceLocation | Arcavacata di Rende (Cosernza) | en |
dc.relation.references | REFERENCES BARRA D., CINQUE A., ITALIANO A., SCORZIELLO R. (1992) - Il pleistocene superiore marino di Ischia: paleoecologia e rapporti con l’evoluzione tettonica recente. Studi Geologici Camerti, Special Vol. (1992/1), 231–243. BERRINO G., CORRADO G., LUONGO G., TORO B. ( 1984) - Ground deformation and gravity changes accompanying the 1982 Pozzuoli uplift. Bull. Volcanol. 47, 187-200. BUCHNER G. (1986) - Eruzioni vulcaniche e fenomeni vulcanotettonici di età preistorica e storica nell’isola d’Ischia. Bibl. de l’Institut Francais de Naples, Deuxième serie, Vol. VII. Pubbl. du Centre Jean Berard, Naples, 145-188 CARLINO S., CUBELLIS E., LUONGO G., OBRIZZO F. (2006) - On the mechanics of caldera resurgence of Ischia Island. Geol. Soc. London Special Pubblication, 269, 181-193. CUBELLIS E., LUONGO G., MARTURANO A. (2007) - Seismic hazard assessment at Mt. Vesuvius: Maximum expected magnitude. J. Volcanol. Geotherm. Res. 162, 139-148 D’ARGENIO A., PESCATORE T., SENATORE M.R. (2004) - Sealevel change and volcano-tectonic interplay. The Gulf of Pozzuoli (Campi Flegrei, Eastern Tyrrhenian Sea) during the last 39 ka. J. Volcanol. Geotherm. Res. 133, 105-121. GÜNTER R.T. (1903) - Contributions to the study of earth movements in the Bay of Naples. Oxford. LAMBECK K., ANTONIOLI F., PURCELL A., SILENZI S. (2004) - Sea level change along the Italian coast for the past 10,000 yrs. Quat. Sc. Rev. 23, 1567-1598. LUONGO G., CUBELLIS E., OBRIZZO F., PETRAZZUOLI S.M. (1991a) - A physical model for the origin of volcanism of the Tyrrhenian margin: the case of the Neapolitan area. J. Volcanol. Geotherm. Res. 48 (1/2): 173-185. LUONGO G., CUBELLIS E., OBRIZZO F., PETRAZZUOLI S.M. (1991b) - The mechanics of the Campi Flegrei resurgent caldera - a model. J.Volcanol. Geotherm. Res. 45, 161-172. LYELL C. (1872) - Principles of Geology. London, John Murray, Albemarie Street, 2, pp.652 FRIEDLAENDER I. (1938) - Sui bradisismi dell'isola d'Ischia e sulla Grotta del Mago. Boll . Soc. Geogr. It 7 (3), 44-54. OBRIZZO F., CUBELLIS E., LUONGO G. (1991) - Strutture tettoniche attive nella caldera flegrea. Boll. Soc. Geol. It. 110, 333-349. SHACKLETON N. J. (1987) - Oxygen isotopes, ice volume, and sea level. Quat. Sci. Rev. 6, 183–190. TIBALDI A. & VEZZOLI L. (2004) - A new type of volcano flank failure: the resurgent caldera sector collapse, Ischia, Italy. Geophysical Research Letters, 31, L14605 doi: 10.1029/2004GL020419. | en |
dc.description.obiettivoSpecifico | 3.6. Fisica del vulcanismo | en |
dc.publisher | Società Geologica Italiana | en |
dc.description.fulltext | open | en |
dc.contributor.author | Cubellis, E. | en |
dc.contributor.author | Delizia, I. | en |
dc.contributor.author | Luongo, G. | en |
dc.contributor.author | Obrizzo, F. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.department | Università di Napoli Federico II | en |
dc.contributor.department | Università di Napoli Federico II | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.editor | Critelli, Salvatore | en |
dc.contributor.editor | Muto, Francesco | en |
dc.contributor.editor | Perri, Francesco | en |
dc.contributor.editor | Petti, Fabio M | en |
dc.contributor.editor | Sonnino, Maurizo | en |
item.openairetype | Extended abstract | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.dept | Università di Napoli Federico II | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.orcid | 0000-0002-2222-5134 | - |
crisitem.author.orcid | 0000-0002-9282-2786 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Conference materials |
Files in This Item:
File | Description | Size | Format | |
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Cubellis_ROL_Vol. 21_part 1_2012.pdf | Extended Abstract | 4.15 MB | Adobe PDF | View/Open |
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