Cap Ventós surprises us with its enormous cliffs of up to a hundred metres in height, formed by Lower Jurassic limestones, Limestones appear well stratified in layers of metric top of a stratigraphical unit or stratigraphical sequence. </p></div>">thickness, very affected by folds and large faults, as Cap de Morobutí.
The impressive cliffs of Cap Ventós display numerous faults that cut through the strata of the Lower Jurassic.
Towards the Cap de Sa Carabassa the faults give way to the gigantic folds visible from the sea.
