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Nature » Geology

Rivers and Streams

Val Cordevole is a very ancient transverse valley. Valley glaciers, streams, degradation of the valley slopes, and karstic erosion have contributed to its morphologic evolution (karstic canyon)The valleys are the most typical morphological expression of the erosion activity carried out by watercourses. Valleys are almost always complex systems, in which the erosive action of a watercourse, affecting only the riverbed and the river banks (lateral cutting and erosion) interacts with the degradation of the slopes (landslides, erosions, disintegration) leads to the morphological evolution of the valley slopes. Among the river formations characterizing the landscape of the Park there are narrow ravines, waterfalls, and potholes.The spectacular Cadini del Brenton, in Val del Mis, are potholes hollowed out in rocks by whirling water and transported debris

 

 

 

 

 

 

Rivers and Streams
Glacial Formations
Karstic Morphology
Geological History 1
Geological History 2
Geological History 3

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