Access: From La Stanga to La Muda bridge, along the SS road 203 "Agordina", with short lateral detours (entrance of Val di Piero, Agre, entrance of Val Pegolera)
A "channel" connecting the Dolomites with the Alpine Foothills
Val Cordevole, narrow and deep "channel" connecting lower Bellunese area with Agordino area, is a very ancient transverse valley crossing (transversally) the whole chain of Dolomiti Bellunesi. As it is often true for ancient valleys, it is a complex environmental system, whose morphological evolution depended on glaciers, watercourses, the slopes degradation processes (landslides and erosion) and, locally, karst corrosion. The glacial action carried out by the ancient Cordevole valley glacier during the glacial period can be recognized for the slightly U-shape of the transversal silhouette (rather large valley bottom and rather steep slopes). Of particular charm the stretch between La Stanga and Castei, a deep gorge dug into the stratified rocks in subhorizontal banks of Dolomia Principale (karst canyon).
The main valley is completed by a system of narrow/deep lateral valleys and gorges, some of which clearly situated along important faults (Val di Piero, Val Vescovà, Val Pegolera). With short detours from the main road, it is possible to enter and explore very charming and interesting micro-environments: