Reconstructing the landscape evolution of the Apennines peri-Adriatic belt requires separating climatic and tectonic signals within its fluvial terrace record, a task so far limited by sparse chronological constraints. Here, we mapped terrace features from three rivers draining the peri-Adriatic belt by combining semiautomatic extraction of tread surfaces from high-resolution digital terrain models with detailed mapping of associated basal strath surfaces using the 1:10,000 geological map. Nine