The shape of the mountains depends on its natural surroundings, particularly on the hardness of the rock. The Grand Bec and the Pointe des Volnets are comprised of mica schist. The Aiguille de la Grande Glière, nicknamed the Matterhorn of Vanoise is comprised of very hard quartzite. The Épéna - the highest limestone cliff in France, with a vertical drop of 800 m - has a very sharp but very disintegrated summit ridge. The Grande Casse, comprised of black schistous limestone, has a highly ravined sloping north side.