Identificador persistente para citar o vincular este elemento: https://accedacris.ulpgc.es/jspui/handle/10553/153373
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dc.contributor.authorLópez, C.en_US
dc.contributor.authorBlanco, M.J.en_US
dc.contributor.authorAbella, R.en_US
dc.contributor.authorBrenes, B.en_US
dc.contributor.authorCabrera Rodríguez, V.M.en_US
dc.contributor.authorCasas, B.en_US
dc.contributor.authorDomínguez Cerdea, I.en_US
dc.contributor.authorFelpeto, A.en_US
dc.contributor.authorDe Villalta, M.F.en_US
dc.contributor.authorDel Fresno, C.en_US
dc.contributor.authorGarcía Pérez, Olayaen_US
dc.contributor.authorGarcía-Arias, M.J.en_US
dc.contributor.authorGarcía-Cañada, L.en_US
dc.contributor.authorGomis Moreno, A.en_US
dc.contributor.authorGonzlez-Alonso, E.en_US
dc.contributor.authorGuzmn Pérez, J.en_US
dc.contributor.authorIribarren, I.en_US
dc.contributor.authorLópez-Díaz, R.en_US
dc.contributor.authorLuengo-Oroz, N.en_US
dc.contributor.authorMeletlidis, S.en_US
dc.contributor.authorMoreno, M.en_US
dc.contributor.authorMoure, D.en_US
dc.contributor.authorDe Pablo, J.P.en_US
dc.contributor.authorRodero, C.en_US
dc.contributor.authorRomero, E.en_US
dc.contributor.authorSainz-Maza, S.en_US
dc.contributor.authorSentre Domingo, M.A.en_US
dc.contributor.authorTorres, P.A.en_US
dc.contributor.authorTrigo, P.en_US
dc.contributor.authorVillasante-Marcos, V.en_US
dc.date.accessioned2025-12-11T14:41:40Z-
dc.date.available2025-12-11T14:41:40Z-
dc.date.issued2012en_US
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://accedacris.ulpgc.es/jspui/handle/10553/153373-
dc.description.abstractOn 10 October 2011, a submarine volcanic eruption started 2 km south from El Hierro Island (Spain). Since July 2011 a dense multiparametric monitoring network was deployed all over the island by Instituto Geográfico Nacional (IGN). By the time the eruption started, almost 10000 earthquakes had been located and the deformation analyses showed a maximum deformation of more than 5 cm. Earthquake migration from the north to the south of the island and acceleration of seismicity are in good correlation with changes in the deformation pattern as well as with some anomalies in geochemical and geomagnetic parameters. An earthquake of local magnitude 4.3 at 12 km depth (8 October 2011) and shallower seismicity a day after, preceded the onset of the eruption. This is the first time that a volcanic eruption is fully monitored in the Canary Islands. Data recorded during this unrest episode at El Hierro will contribute to understand reawakening of volcanic activity in this region and others of similar characteristics.en_US
dc.languageengen_US
dc.relation.ispartofGeophysical Research Lettersen_US
dc.sourceGeophysical Research Letters [ISSN 0094-8276], v. 39, n. 13 (Julio 2012)en_US
dc.subject250621 Vulcanologíaen_US
dc.titleMonitoring the volcanic unrest of El Hierro (Canary Islands) before the onset of the 2011-2012 submarine eruptionen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.identifier.doi10.1029/2012GL051846en_US
dc.identifier.scopus2-s2.0-84864049073-
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dc.identifier.issue13-
dc.relation.volume29en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.identifier.external198286326-
dc.description.numberofpages7en_US
dc.utils.revisionen_US
dc.date.coverdateJulio 2012en_US
dc.identifier.ulpgcNoen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr3,317
dc.description.jcr3,982
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.fulltextCon texto completo-
item.grantfulltextopen-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0009-0007-0184-7990-
crisitem.author.fullNameGarcía Pérez, Olaya-
Colección:Artículos
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