THE GEOLOGICAL VARIETY OF THE COAST OF CABRERA

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The Lower Jurassic limestones of Cap Falcó are replaced westwards to the stratified limestones of the Middle-Upper Jurassic and the grey marls of the Lower Cretaceous (pelagic unit).

Near of the Ansiola lighthouse, it is remarkable a large front of a thrust, which overlap a Lower Jurassic limestones over grey marls, possibly from the Lower Cretaceous. 


Geological interpretation of the cliffs of the south coast of Cabrera, in the vicinity of the Punta des Calamars.