Las barras de arena infralitorales del Maresme: formación y cronología

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dc.contributor.authorSerra, Jordi
dc.contributor.authorSorribas, J.
dc.date.accessioned2017-08-16T11:34:23Z
dc.date.available2017-08-16T11:34:23Z
dc.date.issued1993
dc.description.abstractTwo different types of sand bodies characterize the Maresme Coast (NE Spain). A longshore submarine sand,bar built by theTordera river output is 6 km long and progressively deepens to 8 m depth. Four littoral bar systems have been generated at decresing depths following the sea level rise from the shelf. These sand bodies are generated by quite different processes: littoral drift; reflective storm waves and rip currents. C14 dating has enabled us to make a chronological frame work for both systemses_ES
dc.identifier.urihttp://hdl.handle.net/10272/14041
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSubmarine sand bares_ES
dc.subject.otherMaresme coastes_ES
dc.subject.otherCoastal evolutiones_ES
dc.titleLas barras de arena infralitorales del Maresme: formación y cronologíaes_ES
dc.titleOrigin and chronology ófthe submarine bars of the Maresme Coast (NE Spain)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 14, (1993)