
handle: 10553/16720
Hace cinco millones de años, en los inicios de los tiempos pliocenos, el mar dejó sus arenas y gravas conteniendo multitud de conchas y caparazones de aquella época sobre la costa oeste de Fuerteventura. Hoy estos depósitos de areniscas y conglomerados están a una altura que varía entre los 10 y los 60 metros.
24 Ciencias de la vida, Plioceno, 2416 Paleontología
24 Ciencias de la vida, Plioceno, 2416 Paleontología
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