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  • After outlining the geological, structural and geomorphological features of the area, the AA. discuss the morphological changes which occurred in the Sangro River pattern and its alluvial plain from 1875 to 1992 as a result of construction of major
  • been formed during Middle-Upper Pliocene, after the end of the main tectogenetic phases of the Apennine chain. In order to outline the geomorphologic evolution of the area, detailed geological and geomorphologic investigations have been carried out