Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4830
DC FieldValueLanguage
dc.contributor.authorallMelnik, O.; Institute of Mechanics, Moscow State University,en
dc.contributor.authorallSparks, R. S. J.; Earth Science Department, University of Bristol,en
dc.contributor.authorallCosta, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallBarmin, A.; Institute of Mechanics, Moscow State University,en
dc.date.accessioned2008-12-15T22:29:37Zen
dc.date.available2008-12-15T22:29:37Zen
dc.date.issued2008-07-04en
dc.identifier.urihttp://hdl.handle.net/2122/4830en
dc.description.abstractWe consider the process of slow extrusion of very viscous magma that forms lava domes. Dome-building eruptions are commonly associated with hazardous phenomena, in- cluding pyroclastic flows generated by dome collapses, explosive eruptions and volcanic blasts. These eruptions commonly display fairly regular alternations between pe- riods of high and low or no activity with time scales from hours to years. Usually hazardous phenomena are asso- ciated with periods of high magma discharge rate, thus, understanding the causes of pulsatory activity during ex- trusive eruptions is an important step towards forecasting volcanic behavior, especially the transition to explosive ac- tivity when magma discharge rate increases by a few orders of magnitude. In recent years the risks have increased be- cause the population density in the vicinity of many active volcanoes has increased.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofMeyers: Encyclopedia of Complexity and Systems Scienceen
dc.subjectVolcanic Eruptionsen
dc.subjectCyclicityen
dc.subjectDuring Lavaen
dc.titleVolcanic Eruptions:Cyclicity during Lava Dome Growthen
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.identifier.URLhttp://hdl.handle.net/2122/2887en
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.04. Thermodynamicsen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.description.obiettivoSpecifico3.6. Fisica del vulcanismoen
dc.description.fulltextopenen
dc.contributor.authorMelnik, O.en
dc.contributor.authorSparks, R. S. J.en
dc.contributor.authorCosta, A.en
dc.contributor.authorBarmin, A.en
dc.contributor.departmentInstitute of Mechanics, Moscow State University,en
dc.contributor.departmentEarth Science Department, University of Bristol,en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentInstitute of Mechanics, Moscow State University,en
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.openairetypebook chapter-
item.grantfulltextopen-
item.fulltextWith Fulltext-
item.languageiso639-1en-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.deptInst. Mechanics, Moscow State University, Moskow, Russia-
crisitem.author.deptDepartment of Earth Sciences, University of Bristol, Bristol, UK.-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptInstitute of Mechanics, Moscow State University, Russia-
crisitem.author.orcid0000-0002-4987-6471-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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