Constructive and destructive episodes in the building of a young Oceanic Island, La Palma, Canary Islands, and genesis of the Caldera de Taburiente

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dc.contributor.authorAncochea Soto, Eumenio
dc.contributor.authorHernán Reguera, Francisco
dc.contributor.authorCendrero, Antonio
dc.contributor.authorCantagrel, Jean Marie
dc.contributor.authorFúster, José Maria
dc.contributor.authorIbarrola, Elisa
dc.contributor.authorCoello, Juan
dc.date.accessioned2023-06-20T20:20:48Z
dc.date.available2023-06-20T20:20:48Z
dc.date.issued1990
dc.description.abstractThe results of new field observations, 23 new K-Ar determinations and sixteen previously published determinations provide the basis for the reconstruction of the subaerial volcanic history of the island of La Palma, after the seamount activity represented by the materials of the Basal Complex. An eruptive phase between 2.0 and 1.3 Ma formed a large shield. A period of volcanic quiescence followed, until around 1 Ma, during which a large lateral collapse partly destroyed the former edifice. Between 1.05 and 0.7 Ma, activity was renewed in the shield and a N-S ridge was built in the southern part of the island. Around 0.7 Ma, two new large lateral collapses affected the western part of both edifices, and they were followed by eruptions between 0.71 and 0.65 Ma which built a new edifice that partly filled the depressions thus created. The Caldera de Taburiente constitutes the eroded remnants of the depression formed in the northern shield. From 0.65 Ma to present, activity has been restricted to the N-S ridge, which has continued to grow southwards. There was a general N-S migration of volcanic activity with time, but in the shield the trend was northwest to southeast. Eruptive rates seem to have been fairly constant during the different eruptive phases considered, between 0.15 and 0.37 km3/ka. A very similar succession of constructive and destructive episodes has been obtained for the neighboring island of Hierro, but in this case the activity started around 0.8 Ma and eruptive rates were about 0.5 km3/ka.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipCICYT
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/42518
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dc.identifier.issn0377-0273
dc.identifier.officialurlhttp://www.sciencedirect.com/science/journal/03770273
dc.identifier.urihttps://hdl.handle.net/20.500.14352/60124
dc.journal.titleJournal of Volcanology and Geothermal Research
dc.language.isospa
dc.page.final262
dc.page.initial243
dc.publisherElsevier Science B.V.
dc.relation.projectID1771
dc.rights.accessRightsrestricted access
dc.subject.cdu551.21
dc.subject.ucmGeodinámica
dc.subject.ucmPetrología
dc.subject.ucmSismología (Geología)
dc.subject.unesco2507 Geofísica
dc.subject.unesco2507.05 Sismología y Prospección Sísmica
dc.titleConstructive and destructive episodes in the building of a young Oceanic Island, La Palma, Canary Islands, and genesis of the Caldera de Taburiente
dc.typejournal article
dc.volume.number60
dspace.entity.typePublication
relation.isAuthorOfPublication5a353ace-8a94-4f6e-8a98-20878931274b
relation.isAuthorOfPublication.latestForDiscovery5a353ace-8a94-4f6e-8a98-20878931274b
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