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... The main outcropping lithological units are limestone (at Mt. Maggiore and Caserta Mountains foothills), followed by the CI (in the northern part of the study area) and by the alluvial material derived from the Volturno river ( Fig. 1a).Moreover, an arenaceous-clayey flysch formation made of mixed conglomerates, sandstones, marls and clays outcrops in the external margins of the chain, with an average thickness of a few hundred meters (Budetta et al., 1993). The study area shows different land uses and even in this case no changes have been highlighted analyzing the CLC over the time. ...
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