Quaternary Evolution of the Lower Calore and Middle Volturno Valleys (Southern Italy)

The lower Calore and middle Volturno valleys preserve stratigraphical and morphological evidence and tephrostratigraphic markers particularly suitable for reconstructing the long-term geomorphological evolution of the central-southern Apennines. Aim of our study is to identify the main steps of the Quaternary landscape evolution of these valley systems and to improve knowledge about the relationships between fluvial processes and tectonics, volcanic activity, climatic and human influences. To this purpose, we carried out an integrated geomorphological and chrono-stratigraphical analysis of identified fluvial landforms and related deposits, integrated by Th-230/U-234 datings on travertines from the Telese Plain area. The study highlighted in particular: (1) fluvial sedimentation started in the Middle Pleistocene (similar to 650 ka) within valleys that originated in the lower Pleistocene under the control of high-angle faults; (2) extensional tectonics acted during the Middle and Upper Pleistocene, driving the formation of the oldest fluvial terraces and alluvial fans, and persisted beyond the emplacement of the Campanian Ignimbrite pyroclastic deposits (similar to 39 ka); and (3) from the late Upper Pleistocene onwards (<15 ka), the role of tectonics appears negligible, while climatic changes played a key role in the formation of three orders of valley floor terraces and the youngest alluvial fans.

Automated summary

The study focused on the lower Calore and middle Volturno valleys in the central-southern Apennines, aiming to reconstruct the long-term geomorphological evolution. The research identified the role of tectonics in the formation of fluvial terraces and alluvial fans during the Middle and Upper Pleistocene, while highlighting the increasing importance of climatic changes in shaping the landscape since the late Upper Pleistocene.