English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/77877
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorRodríguez-González, A.-
dc.contributor.authorFernandez-Turiel, J. L.-
dc.contributor.authorPérez-Torrado, F. J.-
dc.contributor.authorParis, Raphael-
dc.contributor.authorGimeno, D.-
dc.contributor.authorCarracedo, Juan Carlos-
dc.contributor.authorAulinas, M.-
dc.date.issued2012-
dc.identifierdoi: 10.1016/j.geomorph.2011.08.023-
dc.identifierissn: 0169-555X-
dc.identifier.citationGeomorphology 136: 31- 44 (2012)-
dc.identifier.urihttp://hdl.handle.net/10261/77877-
dc.description.abstractA detailed morphometric analysis was performed on the 24 Holocene eruptions of Gran Canaria, a nearly circular island located at the centre of the Canary Islands (Spain), developed as result of the eastward movement of the African plate over a mantle hotspot. Rigorous field work was carried out to generate a palaeogeomorphological reconstruction of the Holocene eruptions of Gran Canaria to obtain pre- and post-eruption digital terrain models (DTMs). These eruptions were of Strombolian monogenetic basaltic volcanism style. With respect to the cones, feeder fissures determine their location and some morphological features as crater openings which are usually perpendicular to the slope direction. In addition, the trade winds influence the final volcanic edifice shape and the extent of the pyroclastic sheet-like fall deposits. For the lava flows, the most significant controls are the eruption rate, affecting the maximum distance travelled, and the gully slope and shape that condition their flow path. Concerning volcanic hazard and risk assessment, the applied methodology has led to a better understanding of the recent eruptions and foresees the location and nature of future eruptions. © 2011 Elsevier B.V.-
dc.description.sponsorshipThis work was partially funded by Project PI2002/148 of the Canary Islands Government and by Project GRANCA, Spanish Ministry of Education and Science (Ref. CGL2004-04039/BTE). This work was carried out in the framework of the Research Consolidated Groups GEOVOL and PEGEFA (AGAUR2005 SGR 795 and 2009 SGR 972, Generalitat de Catalunya).-
dc.language.isoeng-
dc.publisherElsevier-
dc.rightsclosedAccess-
dc.subjectDTM-
dc.subjectMorphometry-
dc.subjectVolcano-
dc.subjectHolocene-
dc.subjectGran Canaria-
dc.titleFactors controlling the morphology of monogenetic basaltic volcanoes: The Holocene volcanism of Gran Canaria (Canary Islands, Spain)-
dc.typeartículo-
dc.identifier.doi10.1016/j.geomorph.2011.08.023-
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.geomorph.2011.08.023-
dc.date.updated2013-06-10T11:11:30Z-
dc.description.versionPeer Reviewed-
Appears in Collections:(Geo3Bcn) Artículos
Files in This Item:
File Description SizeFormat 
accesoRestringido.pdf15,38 kBAdobe PDFThumbnail
View/Open
Show simple item record
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.