Vertacomicorii, or Vertacomocorii), meaning excellent troops or troops of the summit. Modern inhabitants are referred to as Vertacomiriens. Prior to the 1900s, the name Vercors referred to the upper valleys of the Vernaison near the township of La Chapelle-en-Vercors. At the beginning of the 20th century, Henri Ferrand explored the massif, taking numerous photographs, publishing books, and describing the geology of the mountains. Ferrand was the first to use the term Vercors in its contemporary sense. The geographers Raoul Blanchard and Jules Blache, popularised the term in the late 1920s and early 1930s. By the 1950s, the term was ubiquitous. Geography Location The Vercors Massif lies in the Prealps, in the south-east France, straddling the departments of Drôme and Isère, both of which are part of the Rhône-Alpes region, about south-east of Lyon. The massif covers with a north-south length of and an east-west width of . The massif is surrounded by the Chartreuse Mountains to the north, the Matheysine area of the Dauphiné Alps to the east, and the Diois Massif to the south. In the far south-east, the massif joins with the col de Menée. The massif is drained in the north-east and the north-west by the Isère, in the east by the Drac, and in the south by the Drôme. The western side overlooks the Rhône Valley. Topography Geomorphology The Vercors Massif is known as the fortress or as the French dolomites because of its geomorphology. The massif is likened to a plateau: the fall from the massif to its inner valleys is a few hundred metres, while the fall to the surrounding areas is between and . The crest of the eastern edge has several summits over . The interior varies between and . The massif also has wide valleys including the valley of Lans-en-Vercors, the regions around Autrans, and La Chapelle-en-Vercors, and plateaus including forêt des Coulmes, forêt de Lente, and the high plateau. There are a number of deeply incised gorges, including the Bourne and Furon Gorges. These have imposing cliffs often exceeding such as the Combe Laval and the Cirque d'Archiane. Mont Aiguille stands apart from the rest of the massif as the result of erosion. Other parts are isolated from the rest of the massif due to its relief. For example, to reach Gresse-en-Vercors in the south, one must travel via the col de Rousset or journey via Saint-Nizier-du-Moucherotte in the north.