Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9971
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dc.contributor.authorallLautze, N.; Hawaii Institute of Geophysics and Planetology, University of Hawaii–Manoa, 1680 East West Road, Honolulu, Hawaii 96825, USA, and Department of Seismology and Tectonophysics, Istituto Nazionale di Geofi sica e Vulcanologia, Via di Vigna Murata 605, 00143 Rome, Italyen
dc.contributor.authorallTaddeucci, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallAndronico, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallHoughton, B.; Department of Geology and Geophysics, University of Hawaii–Manoa, 1680 East West Road, Honolulu, Hawaii 96825, USAen
dc.contributor.authorallNiemeijer, A.; Utrecht University, Faculty of Geosciences–High Pressure and Temperature Laboratory, Budapestlaan 4, 3584 CD, Utrecht, the Netherlandsen
dc.contributor.authorallScarlato, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2015-06-15T07:35:34Zen
dc.date.available2015-06-15T07:35:34Zen
dc.date.issued2013-12-29en
dc.identifier.urihttp://hdl.handle.net/2122/9971en
dc.description.abstractRapid characterization of tephra from ongoing explosive eruptions can provide valuable insights into eruptive mechanisms, especially when integrated with data from other monitoring systems. Here we gain perspective on Stromboli’s eruptive processes by linking the characteristics of ash collected in real-time with videos of each explosion. A 3 day, multifaceted fi eld campaign at Stromboli was undertaken by Italy’s Istituto Nazionale di Geofi sica e Vulcanologia in October 2009. At this time, activity was at a moderately intense level, with the occurrence of an average of 4– 5 explosions per hour at each of the SW and NE craters. Eight ash samples were analyzed using binocular and scanning electron microscopes to gain data on the components, grain size and morphology distributions, and surface chemistry of ash particles within each sample. Monitoring video of each explosion enabled an estimation of the duration and height of each sampled explosion. In each sample, the proportion of fl uidal, glassy sideromelane (as opposed to blocky, microcrystalline tachylite plus lithics), the degree of “chemical freshness” (as opposed to alteration), and the average size of particles appear to correlate with the explosion “type” described in previous studies, and the maximum launch height of the corresponding explosion. Our observations suggest that more violent explosions (i.e., those driven by the liberation of larger and/or more pressurized gas volumes) can be associated with type 2a conditions and the fragmentation of hot and low- viscosity magma, while weaker type 2b explosions erupt predominantly ash-sized particles derived from the fragmentation of colder, more outgassed magma and passive integration of lithic wall debris. The formation of fl uidal sideromelane ash particles (up to Pele’s hair) requires the aerodynamic deformation of a relatively low-viscosity magma and demonstrates unequivocally that ash at Stromboli is not derived entirely from wall rock and/or brittle fragmentation of stagnant magma. We suggest that this ash-sized material forms through rapid acceleration and breakup of larger magma fragments, as supported by evidence from high-speed video of two of the sampled explosions.en
dc.language.isoEnglishen
dc.relation.ispartofThe Geological Society of America special paper 498en
dc.relation.ispartofseriesSpecial Paper 498en
dc.subjectStrombolien
dc.subjectvolcanic ashen
dc.subjectsideromelaneen
dc.subjecttachyliteen
dc.titleInsights into explosion dynamics and the production of ash at Stromboli from samples collected in real-time, October 2009en
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlUnreferreden
dc.description.pagenumber125-139en
dc.subject.INGV05. General::05.02. Data dissemination::05.02.03. Volcanic eruptionsen
dc.identifier.doi10.1130/2013.2498(08)en
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dc.description.obiettivoSpecifico3V. Dinamiche e scenari eruttivien
dc.description.fulltextreserveden
dc.contributor.authorLautze, N.en
dc.contributor.authorTaddeucci, J.en
dc.contributor.authorAndronico, D.en
dc.contributor.authorHoughton, B.en
dc.contributor.authorNiemeijer, A.en
dc.contributor.authorScarlato, P.en
dc.contributor.departmentHawaii Institute of Geophysics and Planetology, University of Hawaii–Manoa, 1680 East West Road, Honolulu, Hawaii 96825, USA, and Department of Seismology and Tectonophysics, Istituto Nazionale di Geofi sica e Vulcanologia, Via di Vigna Murata 605, 00143 Rome, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentDepartment of Geology and Geophysics, University of Hawaii–Manoa, 1680 East West Road, Honolulu, Hawaii 96825, USAen
dc.contributor.departmentUtrecht University, Faculty of Geosciences–High Pressure and Temperature Laboratory, Budapestlaan 4, 3584 CD, Utrecht, the Netherlandsen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypebook chapter-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextreserved-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversity of Hawaii, Manoa, Department of Geology and Geophysics, United States-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptDepartment of Geology and Geophysics, SOEST, University of Hawaii, Honolulu, USA-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-0516-3699-
crisitem.author.orcid0000-0002-8333-1547-
crisitem.author.orcid0000-0003-1933-0192-
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.parent05. General-
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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