Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8038
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dc.contributor.authorallMonecke, T.; Department of Geology and Geological Engineering, Coloradoen
dc.contributor.authorallPetersen, S.; GEOMAR, Helmholtz Centre for Ocean Research Kielen
dc.contributor.authorallHannington, M.; Department of Earth Sciences, University of Ottawaen
dc.contributor.authorallAnzidei, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallEsposito, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallGiordano, G.; Dipartimento Scienze Geologiche, Universita Roma TRE,en
dc.contributor.authorallGarbe-Schönberg, D; Institute of Geosciences, University of Kielen
dc.contributor.authorallAugustin, N; GEOMAR, Helmholtz Centre for Ocean Research Kielen
dc.contributor.authorallMelchert, B.; GEOMAR, Helmholtz Centre for Ocean Research Kiel,en
dc.contributor.authorallHocking, M.en
dc.date.accessioned2012-09-07T13:03:43Zen
dc.date.available2012-09-07T13:03:43Zen
dc.date.issued2012-11en
dc.identifier.urihttp://hdl.handle.net/2122/8038en
dc.description.abstractExplosions of hot water, steam, and gas are common periodic events of subaerial geothermal systems. These highly destructive events may cause loss of life and substantial damage to infrastructure, especially in densely populated areas and where geothermal systems are actively exploited for energy. We report on the occurrence of a large number of explosion craters associated with the offshore venting of gas and thermal waters at the volcanic island of Panarea, Italy, demonstrating that violent explosions similar to those observed on land also are common in the shallow submarine environment. With diameters ranging from 5 to over 100 m, the observed circular seafloor depressions record a history of major gas explosions caused by frequent perturbation of the submarine geothermal system over the past 10,000 years. Estimates of the total gas flux indicate that the Panarea geothermal system released over 70 Mt of CO2 over this period of time, suggesting that CO2 venting at submerged arc volcanoes contributes significantly to the global atmospheric budget of this greenhouse gas. The findings at Panarea highlight that shallow submarine gas explosions represent a previously unrecognized volcanic hazard around populated volcanic islands that needs to be taken into account in the development of risk management strategies.en
dc.language.isoEnglishen
dc.publisher.nameSpringer-Verlagen
dc.relation.ispartofBullettin of Volcanolgyen
dc.relation.ispartofseries/74 (2012)en
dc.subjectGas explosions .en
dc.subjectGeothermal systemsen
dc.subjectSubmarine gas ventingen
dc.subjectVolcanic CO2 fluxen
dc.subjectVolcanic hazardsen
dc.subjectPanarea islanden
dc.titleExplosion craters associated with shallow submarine gas venting off Panarea island, Italyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1937-1944en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.identifier.doi10.1007/s00445-012-0651-8en
dc.description.obiettivoSpecifico1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attiveen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.contributor.authorMonecke, T.en
dc.contributor.authorPetersen, S.en
dc.contributor.authorHannington, M.en
dc.contributor.authorAnzidei, M.en
dc.contributor.authorEsposito, A.en
dc.contributor.authorGiordano, G.en
dc.contributor.authorGarbe-Schönberg, Den
dc.contributor.authorAugustin, Nen
dc.contributor.authorMelchert, B.en
dc.contributor.authorHocking, M.en
dc.contributor.departmentDepartment of Geology and Geological Engineering, Coloradoen
dc.contributor.departmentGEOMAR, Helmholtz Centre for Ocean Research Kielen
dc.contributor.departmentDepartment of Earth Sciences, University of Ottawaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.departmentDipartimento Scienze Geologiche, Universita Roma TRE,en
dc.contributor.departmentInstitute of Geosciences, University of Kielen
dc.contributor.departmentGEOMAR, Helmholtz Centre for Ocean Research Kielen
dc.contributor.departmentGEOMAR, Helmholtz Centre for Ocean Research Kiel,en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Geology and Geological Engineering, Colorado-
crisitem.author.deptGEOMAR, Helmholtz Centre for Ocean Research Kiel-
crisitem.author.deptDepartment of Earth Sciences, University of Ottawa-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptUniversità degli Studi di Roma Tre-
crisitem.author.deptInstitute of Geosciences, University of Kiel-
crisitem.author.deptGEOMAR, Helmholtz Centre for Ocean Research Kiel-
crisitem.author.deptGEOMAR, Helmholtz Centre for Ocean Research Kiel,-
crisitem.author.orcid0000-0003-1935-1049-
crisitem.author.orcid0000-0002-9456-8101-
crisitem.author.orcid0000-0002-5819-443X-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
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