Formes terrestres, diposits eòlics i marins de la serra gelada

Authors

  • Vicent Esteban Chapapría
  • Vicenç M. Rosselló i Verger

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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How to Cite

Esteban Chapapría, . V., & Rosselló i Verger, . V. M. Formes terrestres, diposits eòlics i marins de la serra gelada. Cuadernos De Geografía De La Universitat De València. https://doi.org/10.7203/CGUV.14705
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Issue

NÚM. 60 (1996)

Section

Articles

License

Jornal licence: Creative Commons Reconocimiento-NoComercial-SinObraDerivada 4.0Internacional.

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The texts published in this journal are -if not indicated otherwise- under a Creative Commons license: Recognition-Non-Commercial-NoDerivative 4.0 International. The full license can be consulted at Creative Commons

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