Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/117899
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dc.contributor.authorCarracedo Gomez, Juan Carlosen_US
dc.contributor.authorTroll, Valentin R.en_US
dc.contributor.authorDay, James M.D.en_US
dc.contributor.authorGeiger, Harrien_US
dc.contributor.authorAulinas, Meritxellen_US
dc.contributor.authorBru Soler, Vicenten_US
dc.contributor.authorDeegan, Frances M.en_US
dc.contributor.authorPérez Torrado, Francisco Joséen_US
dc.contributor.authorGisbert, Guillemen_US
dc.contributor.authorGazel, Estebanen_US
dc.contributor.authorRodríguez González, Alejandroen_US
dc.contributor.authorAlbert, Helenaen_US
dc.date.accessioned2022-09-05T11:07:21Z-
dc.date.available2022-09-05T11:07:21Z-
dc.date.issued2022en_US
dc.identifier.issn0266-6979en_US
dc.identifier.otherScopus-
dc.identifier.urihttp://hdl.handle.net/10553/117899-
dc.description.abstractAlmost exactly half a century after the eruption of the Teneguía Volcano on La Palma (26 October to 28 November 1971), a new eruption occurred on the island and lasted for 85 days from 19 September until 13 December 2021. This new eruption opened a volcanic vent complex on the western flank of the Cumbre Vieja rift zone, the N-S elongated polygenetic volcanic ridge that has developed on La Palma over the last c. 125 ka. The Cumbre Vieja ridge is the volcanically active region of the island and the most active one of the Canary Islands, hosting half of all the historically recorded eruptive events in the archipelago. The 2021 La Palma eruption has seen no direct loss of human life, thanks to efficient early detection and sensible management of the volcanic crisis by the authorities, but more than 2800 buildings and almost 1000 hectares of plantations and farmland were affected by lava flows and pyroclastic deposits. Satellite surveillance enabled accurate mapping of the progressive buildup of the extensive and complex basaltic lava field, which together with monitoring of gas emissions informed the timely evacuation of local populations from affected areas. Lava flows that reached the sea constructed an extensive system of lava deltas and platforms, similar to events during earlier historical eruptions such as in 1712, 1949 and 1971. Long-term challenges in the aftermath of the eruption include protection of drainage systems from potential redistribution of tephra during high rainfall events, the use of the large surplus quantities of ash in reconstruction of buildings and in agriculture, and the crucial concerns of where and how rebuilding should and could occur in the aftermath of the eruption. Finally, there remain strong financial concerns over insurance for properties consumed or damaged by the eruption in the light of future volcanic hazards from the Cumbre Vieja volcanic ridge.en_US
dc.languageengen_US
dc.relation.ispartofGeology Todayen_US
dc.sourceGeology Today [ISSN 0266-6979], v. 38 (3), p. 94-107, (Mayo 2022)en_US
dc.subject250621 Vulcanologíaen_US
dc.titleThe 2021 eruption of the Cumbre Vieja volcanic ridge on La Palma, Canary Islandsen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1111/gto.12388en_US
dc.identifier.scopus85132817915-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
dc.contributor.orcidNO DATA-
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dc.contributor.orcidNO DATA-
dc.contributor.authorscopusid55663151400-
dc.contributor.authorscopusid6602449850-
dc.contributor.authorscopusid57764238600-
dc.contributor.authorscopusid57189242224-
dc.contributor.authorscopusid22984147500-
dc.contributor.authorscopusid7003697579-
dc.contributor.authorscopusid36141545000-
dc.contributor.authorscopusid6602207526-
dc.contributor.authorscopusid36786616900-
dc.contributor.authorscopusid12785643800-
dc.contributor.authorscopusid25959720400-
dc.contributor.authorscopusid56688253900-
dc.identifier.eissn1365-2451-
dc.description.lastpage107en_US
dc.identifier.issue3-
dc.description.firstpage94en_US
dc.relation.volume38en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.utils.revisionen_US
dc.date.coverdateMayo 2022en_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr0,119
dc.description.sjrqQ4
dc.description.miaricds10,0
item.grantfulltextopen-
item.fulltextCon texto completo-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Didácticas Específicas-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0002-4282-2796-
crisitem.author.orcid0000-0002-4644-0875-
crisitem.author.orcid0000-0003-0688-0531-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.fullNameCarracedo Gomez,Juan Carlos-
crisitem.author.fullNameBru Soler, Vicent-
crisitem.author.fullNamePérez Torrado, Francisco José-
crisitem.author.fullNameRodríguez González, Alejandro-
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