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Piano di Campotenese
WI_e2139_003.JPG MormannoThumbnailsMorano Calabro and Monte Pollino

View from the southern slopes of Monte Pollino in southwestern direction to the Orsomarso Mountains. The depression of the Piano di Campotenese is most likely related to tectonic structures on the one hand, and to karst processes on the other hand. It is often referred to as a polje, a large-scale karstic hollow.

Created
Tuesday 3 April 2012 by Martin Mergili in Europe / Italy (2453 visits)