Fig. 7From: Messinian or Pleistocene valley incision within the Southern AlpsDifferent estimates of total accumulated rock uplift since Messinian assuming steady state, i.e. erosion is balanced by uplift (Fig. 3). Note that an assumption of local isostasy would be 20% lower. The Trento-Cles and the Periadriatic Faults have no described vertical offset in the post Messinian period in the study areaBack to article page