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dc.contributor.authorGalparsoro, Ibon
dc.contributor.authorBorja, Angel
dc.contributor.authorLegorburu, Irati
dc.contributor.authorHernandez, Carlos
dc.contributor.authorChust, Guillem
dc.contributor.authorLiria, Pedro
dc.contributor.authorUriarte, Adolfo
dc.date.accessioned2019-05-31T08:50:37Z-
dc.date.available2019-05-31T08:50:37Z-
dc.date.issued2010
dc.identifierISI:000277904600008
dc.identifier.citationGEOMORPHOLOGY, 2010, 118, 314-329
dc.identifier.issn0169-555X
dc.identifier.urihttp://dspace.azti.es/handle/24689/726-
dc.description.abstractThis contribution integrates and analyzes data from high-resolution multibeam, seismic profiles, bathymetric LiDAR, and surficial sediment data for the geomorphological seascapes characterisation and process-description of the Basque inner and middle continental shelf (northern Spain). From the data obtained, the Basque shelf is characterised by a heterogeneous seafloor where, on a small spatial scale, different morphologies and sedimentary processes can be observed. Tectonic activity and sea-level changes, together with present processes of sediment supply and climatic conditions, have a critical influence on the present configuration of the continental shelf and the distribution of seafloor types. On the basis of all of the datasets, seafloor classification, bedform analysis, long-term sea-level change-induced seafloor features and anthropogenic features over the seafloor, are described. As a result, three distinct zones have been identified for the Basque shelf, related to the main geomorphological features and seascapes, as summarised below. (i) A western part, with a northwestern orientation, which coincides with the prevailing wave direction. This zone is characterised by a predominantly rocky substrate, except within the mouth of the Nervion estuary, where sandy sediments appear to infill a paleo-channel. (ii) A central part, which is oriented towards the northeast and receives less wave energy. Within this zone, a sedimentary seabed is predominant. Sorted bedforms are well developed and can be detected in water depths in excess of 90 m. (iii) An eastern zone, which is characterised by sedimentary seafloor and shore terraces; here, a flat rocky seafloor is covered by a thin layer of sediments. Throughout the study area, the bathymetry and sedimentary features of the shoreface and inner shelf are controlled mainly by climatic conditions, coastal dynamics and the underlying geological framework. The integration of these data sets, together with their interpretation, is a valuable source of information for Integrated Coastal Zone Management (ICZM) and constitutes a useful tool for implementing various European Directives. (C) 2010 Elsevier B.V. All rights reserved.
dc.language.isoeng
dc.publisherELSEVIER SCIENCE BV
dc.subjectSeafloor cartography
dc.subjectGeomorphology
dc.subjectSeascape
dc.subjectMultibeam echosounder
dc.subjectBathymetric LiDAR
dc.subjectIntegrated Coastal Zone Management
dc.subjectBasque shelf
dc.subjectSEA-FLOOR CHARACTERIZATION
dc.subjectRIPPLED SCOUR DEPRESSIONS
dc.subjectLONG-TERM DEVELOPMENT
dc.subjectGALICIA BANK
dc.subjectSEDIMENTARY PROCESSES
dc.subjectSORTED BEDFORMS
dc.subjectIBERIAN MARGIN
dc.subjectINNER-SHELF
dc.subjectMETHODOLOGICAL APPROACH
dc.subjectMULTIBEAM BATHYMETRY
dc.titleMorphological characteristics of the Basque continental shelf (Bay of Biscay, northern Spain); their implications for Integrated Coastal Zone Management
dc.typeArticle
dc.identifier.journalGEOMORPHOLOGY
dc.format.page314-329
dc.format.volume118
dc.contributor.funderDepartment of Environment, Land Use, Agriculture and Fisheries, of the Basque Government
dc.contributor.funderEuropean Commision
dc.contributor.funderFundacion Centros Tecnologicos
dc.identifier.doi10.1016/j.geomorph.2010.01.012
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