Formes terrestres, diposits eòlics i marins de la serra gelada
DOI:
https://doi.org/10.7203/CGUV..14705
Abstract
Se estudia la geomorfología de la Serra Gelada, su red de drenaje y los tres frentes marinos que presenta este sector litoral montañoso situado en la extremidad de las cadenas prebéticas valencianas. Destacan en el frente marino suroriental determinadas formaciones eólicas cuaternarias que alcanzan cerca de los 200 m de altitud y se implican con taludes y conos de materiales desprendidos de los acantilados. Se analiza la morfología de la plataforma litoral y las características sedimentológicas de los materiales costeros.
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