The dammed lake of la Sassière was completed in 1953 in place of a natural lake. It is a “gravity” dam, the mass of materials is opposed to the surge of the water. The rock used for the dyke is quartzite, as at the Verrou du Saut, but it comes from glacial moraines located under the Pointe de la Baillettaz, in front of you. The truck path now serves as a... trail to reach the Col de la Baillettaz.