Fig. 2

Simplified geological map and geological cross section of Epiligurian Vetto-Carpineti syncline outlier. In the geological cross sections and in the map the middle Enza Valley, the Rio Maillo and the Monte Faiedolo transversal tectonic structures, striking NE–SW, are evidenced. Modified after Papani et al. (1987) and De Nardo et al. (1991)