Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/2232
DC Field | Value | Language |
---|---|---|
dc.contributor.authorall | Acocella, V.; Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
dc.contributor.authorall | Porreca, M.; Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
dc.contributor.authorall | Neri, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Mattei, M.; Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
dc.contributor.authorall | Funiciello, R.; Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
dc.date.accessioned | 2007-07-03T07:59:50Z | en |
dc.date.available | 2007-07-03T07:59:50Z | en |
dc.date.issued | 2006 | en |
dc.identifier.uri | http://hdl.handle.net/2122/2232 | en |
dc.description.abstract | Fissure eruptions may provide important information on the shallow propagation of dikes at volcanoes. Somma-Vesuvius (Italy) consists of the active Vesuvius cone, bordered to the north by the remnants of the older Somma edifice. Historical chronicles are considered to define the development of the 37 fissure eruptions between A.D. 1631 and 1944. The 1631 fissure, which reopened the magmatic conduit, migrated upward and was the only one triggered by the subvertical propagation of a dike. The other 25 fissure eruptions migrated downward, when the conduit was open, through the lateral propagation of radial dikes. We suggest two scenarios for the development of the fissures. When the summit conduit is closed, the fissures are fed by vertically propagating dikes. When the summit conduit is open, the fissures are fed by laterally propagating dikes along the volcano slopes. Consistent behaviors are found at other composite volcanoes, suggesting a general application to our model, independent of the tectonic setting and composition of magma. At Vesuvius, the historical data set and our scenarios are used to predict the consequences of the emplacement of fissures after the opening of the conduit. The results suggest that, even though the probability of opening of vents within the inhabited south and west slopes is negligible, the possibility that these are reached by a lava flow remains significant. | en |
dc.format.extent | 308433 bytes | en |
dc.format.mimetype | application/pdf | en |
dc.language.iso | English | en |
dc.publisher.name | Geological Society of America | en |
dc.relation.ispartof | Geology | en |
dc.relation.ispartofseries | 8/34 (2006) | en |
dc.subject | fissures | en |
dc.subject | dike propagation | en |
dc.subject | conduit | en |
dc.subject | Vesuvius | en |
dc.title | Fissure eruptions at Mount Vesuvius (Italy):insights on the shallow propagation of dikes at volcanoes | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 673-676 | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.09. Structural geology | en |
dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics | en |
dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.05. Stress | en |
dc.identifier.doi | 10.1130/G22552.1 | en |
dc.relation.references | Acocella, V., and Neri, M., 2003, What makes flank eruptions? The 2001 Mount Etna eruption and its possible triggering mechanisms: Bulletin of Volcanology, v. 65, p. 517–529, doi: 10.1007/s00445-003-0280-3. Acocella, V., and Tibaldi, A., 2005, Dike propagation driven by volcano collapse: A general model tested at Stromboli, Italy: Geophysical Research Letters, v. 32, p. L08308, doi: 10.1029/2004GL022248. Behncke, B., Neri, M., and Nagay, A., 2005, Lava flow hazard at Mount Etna (Italy): New data from a GIS-based study, in Manga, M., and Ventura, G., eds., Kinematics and dynamics of lava flows: Geological Society of America Special Paper 396, p. 187–205, doi: 710.1130/2005.2396(13). Bianco, F., Castellano, M., Milano, G., Ventura, G., and Vilardo, G., 1998, The Somma-Vesuvius stress field induced by regional tectonics: Evidences from seismological and mesostructural data: Journal of Volcanology and Geothermal Research, v. 82, p. 199–218, doi: 10.1016/S0377-0273(97) 00065-6. Bruno, P.P., and Rapolla, A., 1999, Study of the sub-surface structure of Somma- Vesuvius (Italy) by seismic reflection data: Journal of Volcanology and Geothermal Research, v. 92, p. 373–387, doi: 10.1016/S0377-0273(99) 00093-1. Cioni, R., Santacroce, R., and Sbrana, A., 1999, Pyroclastic deposits as a guide for reconstructing the multi-stage evolution of the Somma-Vesuvius caldera: Bulletin of Volcanology, v. 61, p. 207–222, doi: 10.1007/ s004450050272. Cortini, M., and Scandone, R., 1982, The feeding system of Vesuvius between 1754 and 1944: Journal of Volcanology and Geothermal Research, v. 12, p. 393–400, doi: 10.1016/0377-0273(82)90036-1. Decker, R.W., 1987, Dynamics of Hawaiian volcanoes: An overview: U.S. Geological Survey Professional Paper, v. 1350, p. 997–1018. Gasparini, P., and Musella, S., 1991, Un Viaggio al Vesuvio: Napoli, Liguori Editore, 307 p. Gudmundsson, A., 2002, Emplacement and arrest of sheets and dikes in central volcanoes: Journal of Volcanology and Geothermal Research, v. 116, p. 279–298, doi: 10.1016/S0377-0273(02)00226-3. Lanzafame, G., Neri, M., Acocella, V., Billi, A., Funiciello, R., and Giordano, G., 2003, Structural features of the July–August 2001 Mount Etna eruption: Evidence for a complex magma supply system: Geological Society [London] Journal, v. 160, p. 531–544. Lockwood, J.P., and Lipman, P.W., 1987, Holocene eruptive history of Mauna Loa volcano: U.S. Geological Survey Professional Paper, v. 1350, p. 509–535. McClelland, L., Simkin, T., Summers, M., Nielsen, E., and Stein, T.C., 1989, Global volcanism 1975–1985: Englewood Cliffs, New Jersey, Prentice Hall, 657 p. Nazzaro, A., 1997, Il Vesuvio. Storia eruttiva e teorie vulcanologiche: Napoli, Liguori Editore, 380 p. Neri, M., Acocella, V., Behncke, B., Maiolino, V., Ursino, A., and Velardita, R., 2005, Contrasting triggering mechanisms of the 2001 and 2002–2003 eruptions of Mount Etna (Italy): Journal of Volcanology and Geothermal Research, v. 144, p. 235–255, doi: 10.1016/j.jvolgeores.2004.11.025. Palmieri, L., 1880, Il Vesuvio e la sua storia: Milano, Tipografia Faverio, 79 p. Rosi, M., Principe, C., and Vecci, R., 1993, The 1631 Vesuvius eruption. A reconstruction based on historical and stratigraphical data: Journal of Volcanology and Geothermal Research, v. 58, p. 151–182, doi: 10.1016/ 0377-0273(93)90106-2. Santacroce, R., 1983, A general model for the behaviour of the Somma Vesuvius volcanic complex: Journal of Volcanology and Geothermal Research, v. 17, p. 237–248, doi: 10.1016/0377-0273(83)90070-7. Santacroce, R., 1987, Somma Vesuvius: Rome, C.N.R. Roma, 251 p. Santacroce, R., and Sbrana, A., (eds.), 2003, Carta Geologica del Vesuvio, Volume 1: Florence, Italy, SELCA, scale 1:15,000. Scandone, R., 1976, Il rischio da colate di lava ed implicazioni socioeconomiche: Proceedings, I vulcani attivi dell’area napoletana, Napoli 23– 25 June 1977, p. 103–106. Scandone, R., Giacomelli, L., and Gasparini, P., 1993, Mount Vesuvius: 2000 years of volcanological observations: Journal of Volcanology and Geothermal Research, v. 58, p. 4–25. Sorrentino, I., 1734, Istoria del Monte Vesuvio: Naples, Italy, Severini, 224 p. Tedesco, D., 2002, The January 2002 eruption of Mount Nyiragongo DRC: Dynamics and hazard: Proceedings, European Geophysical Society meeting, Nice, France, April 2002 [abs.]: p. 111. | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Acocella, V. | en |
dc.contributor.author | Porreca, M. | en |
dc.contributor.author | Neri, M. | en |
dc.contributor.author | Mattei, M. | en |
dc.contributor.author | Funiciello, R. | en |
dc.contributor.department | Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
dc.contributor.department | Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
dc.contributor.department | Dipartimento di Scienze Geologiche, Universita` degli Studi di Roma Tre | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Università Roma Tre, Dipartimento di Scienze Geologiche, Rome, Italy | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Università degli studi di Roma TRE | - |
crisitem.author.orcid | 0000-0001-8628-606X | - |
crisitem.author.orcid | 0000-0002-5890-3398 | - |
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.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
Files in This Item:
WEB OF SCIENCETM
Citations
50
24
checked on Feb 7, 2021
Page view(s) 50
256
checked on Apr 24, 2024
Download(s)
33
checked on Apr 24, 2024