The river geomorphology
Lungo il path can be recognized glacial action, the sites that hosted the paleolaghi (two in one historical period and in prehistoric times) and hydro-geomorphological evidence from the valley and the valley, one can identify the causes of barriers and we understand that the lake is a ephemeral element of the landscape, assessing the future evolution of the recognition of areas subject to landslides, avalanches and areas of the sites in accelerated erosion and anthropogenic changes.
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