Mapping the slip rate, tip propagation, geometry and tectonic geomorphology of the Aremogna Fault, central Apennines, Italy

Abstract

In order to understand the seismic hazard posed by an active faults it is necessary to know (i) the long-term rate of movement of the fault; (ii) the geometry of the fault; and (iii) the time that has elapsed since the last earthquake occurred on the fault. This study aimed to improve the information known about the Aremogna-Cinque Miglia Fault in the central Apennines, Italy.