Early Pleistocene (Santernian: MNN 19b-c Nannofossil Zones) coastal marine deposits related to rocky coast evolution have been described in a wide area near Orvieto (Umbria, Central Italy). Sediments range from boulders and blocks, to rounded
The presence of ammonites in the Bonarelli Level (uppermost Cenomanian) of the Umbria-Marche Succession is reported here for the first time. The horizon studied has been recognised near Serra S. Abbondio, on the external limb of the Mt. Catria
The Umbria-Marche 1997 seismic sequence occurred in a region of the Northern Apennines (Italy) that has been under extension since the Late Pliocene. This sequence activated normal faults and high-angle faults inherited from an earlier contractional