Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/82517
Share/Export:
logo share SHARE logo core CORE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE
DC FieldValueLanguage
dc.contributor.authorCastañeda del Álamo, Carmen-
dc.contributor.authorGracia, Francisco Javier-
dc.contributor.authorMeyer, Anika-
dc.contributor.authorRomeo Gamarra, Raquel-
dc.date.accessioned2013-09-23T10:23:20Z-
dc.date.available2013-09-23T10:23:20Z-
dc.date.issued2013-08-09-
dc.date.issued2013-10-02-
dc.identifier.citationCastañeda C, Gracia FJ, Meyer A, Romeo R. Coastal landforms and environments in the central sector of Gallocanta saline lake (Iberian Range, Spain). Journal of Maps 9 (4): 584-589 (2013)es_ES
dc.identifier.issn1744-5647-
dc.identifier.urihttp://hdl.handle.net/10261/82517-
dc.description12 Págs., 3 Figs. This is an Author's Accepted Manuscript of an article published in Castañeda C, Gracia FJ, Meyer A, Romeo R. Coastal landforms and environments in the central sector of Gallocanta saline lake (Iberian Range, Spain) as published in the Journal of Maps, 2013. Available online 9 August 2013. Copyright Taylor & Francis, available online at: http://www.tandfonline.com/10.1080/17445647.2013.829413es_ES
dc.description.abstractGallocanta Lake (NE Spain), with a high ecological value, is the largest and best preserved saline lake in Western Europe. The aim of this study is to map the landforms developed in the margins of the central sector of Gallocanta Lake, at adequate scale for the study of soils and habitats, which is needed for the delineation, management and protection of the wetland. Photointerpretation was combined with topographical, geological, and satellite data in a geographical information system. This study, applied in two selected areas of the central body of the lake, allowed the identification of contrasting landforms and processes in the lake margins. The southern margin, which receives most of the fluvial materials in the zone exhibits coastal progradation by means of barrier-island generation and sedimentation in the resulting coastal lagoon, a process that can be inferred from the map presented in this work and was confirmed by comparison of aerial photographs taken in different decades. With virtually no sediment supply on the margin, coastal erosion and shoreline retreat prevail. In summary, coastal landforms are a result of a complex combination of fluvial and lacustrine processes operating during high and low water-level periods.es_ES
dc.language.isoenges_ES
dc.publisherTaylor & Francises_ES
dc.rightsopenAccesses_ES
dc.subjectLake geomorphologyes_ES
dc.subjectMappinges_ES
dc.subjectSaline lakees_ES
dc.subjectSaline soilses_ES
dc.subjectWetlandes_ES
dc.titleCoastal landforms and environments in the central sector of Gallocanta saline lake (Iberian Range, Spain)es_ES
dc.typeartículoes_ES
dc.identifier.doi10.1080/17445647.2013.829413-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1080/17445647.2013.829413es_ES
dc.embargo.terms2014-08-10-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.openairetypeartículo-
item.grantfulltextopen-
item.cerifentitytypePublications-
Appears in Collections:(EEAD) Artículos
Files in This Item:
File Description SizeFormat
CastañedaC_JMaps_2013.pdf1,08 MBAdobe PDFThumbnail
View/Open
Show simple item record

Google ScholarTM

Check

Altmetric

Dimensions


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