The Alluvial Marls of the Roussillon Plain
During the Quaternary period, alternating cold cycles, known as "glacial" periods, and temperate or warm cycles, known as "interglacial" periods, have sculpted the region’s landscape. In the Roussillon plain, valleys were carved by rivers flowing down the mountains through the Pliocene sediment layers, forming alluvial terraces on which the 26 hectares adjacent to the estate are situated.