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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11908
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dc.date.accessioned2018-07-16T06:13:50Zen
dc.date.available2018-07-16T06:13:50Zen
dc.date.issued2018-07-12en
dc.identifier.urihttp://hdl.handle.net/2122/11908en
dc.description.abstractFogo volcano erupted in 2014–2015 producing an extensive lava flow field in the summit caldera that destroyed two villages, Portela and Bangaeira. The eruption started with powerful explosive activity, lava fountains, and a substantial ash column accompanying the opening of an eruptive fissure. Lava flows spreading from the base of the eruptive fissure produced three arterial lava flows. By a week after the start of the eruption, a master lava tube had already developed within the eruptive fissure and along the arterial flow. In this paper, we analyze the emplacement processes based on observations carried out directly on the lava flow field, remote sensing measurements carried out with a thermal camera, SO2 fluxes, and satellite images, to unravel the key factors leading to the development of lava tubes. These were responsible for the rapid expansion of lava for the ~7.9 km length of the flow field, as well as the destruction of the Portela and Bangaeira villages. The key factors leading to the development of tubes were the low topography and the steady magma supply rate along the arterial lava flow. Comparing time-averaged discharge rates (TADR) obtained from satellite and Supply Rate (SR) derived from SO2 flux data, we estimate the amount and timing of the lava flow field endogenous growth, with the aim of developing a tool that could be used for hazard assessment and risk mitigation at this and other volcanoes.en
dc.description.sponsorshipThis research received no external funding.en
dc.language.isoEnglishen
dc.relation.ispartofRemote Sensingen
dc.relation.ispartofseries/10(2018)en
dc.subjectFogo volcanoen
dc.subjectlava flow inflationen
dc.subjectlava tubesen
dc.subjecttime averaged discharge rateen
dc.subjectmagma supply rateen
dc.titleSatellite and Ground Remote Sensing Techniques to Trace the Hidden Growth of a Lava Flow Field: The 2014-15 Effusive Eruption at Fogo Volcano (Cape Verde)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1115en
dc.subject.INGVvolcanic hazarden
dc.subject.INGVremote sensing monitoringen
dc.subject.INGVeffusive eruptionen
dc.identifier.doi10.3390/rs10071115en
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dc.description.obiettivoSpecifico6V. Pericolosità vulcanica e contributi alla stima del rischioen
dc.description.journalTypeJCR Journalen
dc.contributor.authorCalvari, Soniaen
dc.contributor.authorGanci, Gaetanaen
dc.contributor.authorVictória, Sónia Silvaen
dc.contributor.authorHernandez, Pedro A.en
dc.contributor.authorPerez, Nemesio M.en
dc.contributor.authorAlfama, Veraen
dc.contributor.authorBarrancos, Joséen
dc.contributor.authorCabral, Jeremiasen
dc.contributor.authorCardoso, Nadiren
dc.contributor.authorDionis, Samaraen
dc.contributor.authorFernandes, Pauloen
dc.contributor.authorMelian, Gladysen
dc.contributor.authorPereira, Joséen
dc.contributor.authorSemedo, Hélioen
dc.contributor.authorPadilla, Germánen
dc.contributor.authorRodriguez, Fátimaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
item.openairetypearticle-
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptEnvironmental Research Division, ITER, Tenerife/Spain-
crisitem.author.deptEnvironmental Research Division, ITER, Tenerife/Spain-
crisitem.author.deptEnvironmental Research Division, ITER, Tenerife/Spain-
crisitem.author.deptEnvironmental Research Division, ITER, Tenerife/Spain-
crisitem.author.orcid0000-0001-8189-5499-
crisitem.author.orcid0000-0002-9914-1107-
crisitem.author.orcid0000-0003-4707-515X-
crisitem.author.orcid0000-0003-1418-6152-
crisitem.author.orcid0000-0002-4555-8484-
crisitem.author.orcid0000-0003-2604-2375-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.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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