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  • and elementary valley dynamics, while the harsh environment limits human disturbance. The geomorphic analysis is supplemented with a palynological analysis of the valley fills to identify the environmental causes of this alternation.
  • 2000
  • . The dynamics are mainly the result of the action of the particularly aggressive climatic factors (such as the Mediterranean rainfall regime) on weak substrata. The morphogenetic activity is not only limited to channel erosion, but it is also due to repeated
  • 2000