Introducció les eolianites de les Penyes de l'Albir
DOI:
https://doi.org/10.7203/CGUV..14703
Abstract
Las eolianitas de les Penyes de l'Albir han inmovilizado un volumen de cerca de 16 hm sobre el flanco marítimo de la Serra Gelada en una secuencia cuaternaria de llamativas formas relictas donde interfieren procesos marinos, eólicos y propios de ladera. Parece haber pesado más la anchura y naturaleza de la plataforma marina que los repetidos cambios de nivel que apenas han dejado huella. Las dunas adosadas rampantes pertenecen a diversos sistemas -tres al menos- que tratamos de individualizar, así como unas formaciones encostradas de ladera muy significativas.
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