Quaternary morphoevolution of Central-Southern Italy

What is it about?

In this foreword the editors present a collection of papers illustrating the geological and geomorphological features of a significant number of Pliocene to Quaternary intermontane basins of the central-southern Apennines. Such basins, not strictly coeval, are the result of a common morphotectonic evolution, albeit with a variable organization of the local structures.

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Why is it important?

Availability of papers related to a wide geographic layout of intermontane basins spanning from central to southern segments of the Italian Apennines orogenic chain.

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