

The cliff that dominates the Règue valley is made of limestone. It outcrops westward almost continuously, on nearly 15km until Vaugines, through Cucuron. Geologists have called this geological formation the Molasse de Cucuron. This rock is very rich in sand grains, gravel and fossil remains (scallops, oysters, corals ...). Fossils evidence the presence of a warm sea right here, about 10 million years ago.