The Neolithic site of Maddalena di Muccia (Umbria-Marche Apennine, Italy): a tip to reconstruct the geomorphological evolution and human occupation during the Late Pleistocene and the Holocene

The resumption of linear erosion coincided with the natural erosion of the dams previously caused by landslides, and above all, (starting from about 4500 yr BP) with the rapid decline of the travertine deposition due mainly to climatic conditions.