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dc.contributor.authorVergara Dal Pont, Iván P.-
dc.contributor.authorCaselli, Alberto Tomás-
dc.contributor.authorMoreiras, Stella M.-
dc.contributor.authorLauro, Carolina-
dc.date.accessioned2020-05-28T13:12:57Z-
dc.date.available2020-05-28T13:12:57Z-
dc.date.issued2017-11-
dc.identifier.citationVergara Dal Pont, Iván P., Caselli, Alberto T., Moreiras, Stella M. y Lauro, Carolina (2017). Recent Coastal Geomorphological Evolution in the Negro River’s Mouth (418S), Argentinean Patagonia. Coastal Education & Research Foundation; Journal of Coastal Research; 33 (6); 1367–1375es_ES
dc.identifier.issn0749-0208es_ES
dc.identifier.urihttps://rid.unrn.edu.ar/jspui/handle/20.500.12049/5132-
dc.description.abstractThis paper analyzes the geomorphological evolution of the Negro River's mouth to understand how aerodynamic and hydrodynamic states of the Atlantic coast have developed to this date. Accordingly, the morphometry of the beach and the historical river flow record were studied. The results indicate a dichotomous state for this coast. The SW area is characterized by cliffs with an average recession rate of 0.69 m/y during the 1959-2011 period, whereas the NE area is characterized by beaches in stable and accretion states. In the latter zone, a relatively fast coastal accretion was corroborated with the advance of a berm of up to 170 m between 1986 and 2014; furthermore, the beach extension grew to 760 m during 1986-2004. Since 1936, a completely new phenomenon was observed at the Negro River's mouth: the displacement and accretion of intertidal banks toward the coast provoked the closure of the channels of fluvial discharge and tidal currents. This activity at the Negro River's mouth could be due to the reduction of river discharge during the 20th century, which increased the preponderance of littoral current over the river discharge.es_ES
dc.format.extentp. 1367–1375es_ES
dc.format.mediumdigitales_ES
dc.language.isoenes_ES
dc.publisherCoastal Education & Research Foundationes_ES
dc.titleRecent Coastal Geomorphological Evolution in the Negro River’s Mouth (418S), Argentinean Patagoniaes_ES
dc.typeArticuloes_ES
dc.rights.licensehttps://creativecommons.org/licenses/by-nc-sa/4.0/es_ES
dc.description.filiationFil: Vergara Dal Pont, Iván P. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Mendoza, Argentina.es_ES
dc.description.filiationFil: Caselli, Alberto Tomás Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Laboratorio de Estudio y Seguimiento de Volcanes Activos. Río Negro, Argentina.es_ES
dc.description.filiationFil: Moreiras, Stella M. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Mendoza, Argentina.es_ES
dc.description.filiationFil: Lauro, Carolina. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Mendoza, Argentina.es_ES
dc.description.filiationFil: Vergara Dal Pont, Iván P. Consejo Nacional de Investigaciones Científicas y Técnicas. Mendoza, Argentina.es_ES
dc.description.filiationFil: Caselli, Alberto Tomás Consejo Nacional de Investigaciones Científicas y Técnicas. Río Negro, Argentina.es_ES
dc.description.filiationFil: Moreiras, Stella M. Consejo Nacional de Investigaciones Científicas y Técnicas. Mendoza, Argentina.es_ES
dc.description.filiationFil: Lauro, Carolina. Consejo Nacional de Investigaciones Científicas y Técnicas. Mendoza, Argentina.es_ES
dc.subject.keywordCoastal Processeses_ES
dc.subject.keywordGeomorphologyes_ES
dc.subject.keywordBeach Geodynamices_ES
dc.subject.keywordLandscape Evolutiones_ES
dc.type.versioninfo:eu-repo/semantics/publishedVersiones_ES
dc.origin.lugarDesarrolloUniversidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología.es_ES
dc.relation.journalissue33 (6)es_ES
dc.description.reviewtruees_ES
dc.description.resumenThis paper analyzes the geomorphological evolution of the Negro River's mouth to understand how aerodynamic and hydrodynamic states of the Atlantic coast have developed to this date. Accordingly, the morphometry of the beach and the historical river flow record were studied. The results indicate a dichotomous state for this coast. The SW area is characterized by cliffs with an average recession rate of 0.69 m/y during the 1959-2011 period, whereas the NE area is characterized by beaches in stable and accretion states. In the latter zone, a relatively fast coastal accretion was corroborated with the advance of a berm of up to 170 m between 1986 and 2014; furthermore, the beach extension grew to 760 m during 1986-2004. Since 1936, a completely new phenomenon was observed at the Negro River's mouth: the displacement and accretion of intertidal banks toward the coast provoked the closure of the channels of fluvial discharge and tidal currents. This activity at the Negro River's mouth could be due to the reduction of river discharge during the 20th century, which increased the preponderance of littoral current over the river discharge.es_ES
dc.identifier.doihttps://doi.org/10.2112/JCOASTRES-D-16-00060.1-
dc.relation.journalTitleJournal of Coastal Researches_ES
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