Towns & Places

Cascate della Volpara e Selvagrande


The falls are situated in the northern sector of the massif. The Laga is covered with clayey-arenaceous layers, yet its heart is made of calcareous stone and dates back to the end of the Miocene. In this environment erosive phenomena are very clear, and are determined both by the Quaternary glaciations and by the waters.

 | Map  |  Print  |