Caracteres sedimentológicos y geomorfológicos del Alto Nivel Aluvial cuaternario en el litoral de Huelva
Loading...
Publication date
Advisors
Department
Research group
Center
Metrics
Export
Abstract
El Alto nivel aluvial, en este sector del litoral de Huelva, es el pri¬mer indicador de la instauración de la red fluvial cuaternaria; con ríos de cursos entrelazados, mayoritariamente, y variaciones locales de tipo meandriforme condicionadas por el paleorrelieve previo.
The upper alluvial level from Hueiva littoral, southern Spain, re¬presents the first indication of a fluvial quaternary environment, with platform and terrace landforms. This deposit lies over the pliocene paleorelief, which shows an alteration phenomenon with laterite pro¬files. The fluvial deposits are mainly braided with channel and bar facies although some meandering sequences may be formed as result of a topographic control.
The upper alluvial level from Hueiva littoral, southern Spain, re¬presents the first indication of a fluvial quaternary environment, with platform and terrace landforms. This deposit lies over the pliocene paleorelief, which shows an alteration phenomenon with laterite pro¬files. The fluvial deposits are mainly braided with channel and bar facies although some meandering sequences may be formed as result of a topographic control.
Keywords
Unesco Subjects
Bibliographic citation
Pendón Martín, J.G., Rodríguez Vidal, J.: "Caracteres sedimentológicos y geomorfológicos del Alto Nivel Aluvial cuaternario en el litoral de Huelva". Acta Geológica Hispánica. T. 21-22, págs. 107-111. (1986-1987). ISSN 0567-7505
Collections
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España