The Mont Aiguille, from its 2087 meters, is a mound of the eastern barrier of the Vercors. Indeed, the Mount is composed of the same materials as the rest of the plateau (limestones and marls deposited by the sea before the rising of the Alps) to which it was formerly attached. The most tender limestones and the presence of numerous faults facilitated the dissolution of the limestone over time, leading to the isolation of Mount.