Located in central Europe at the junction of the Southern Alps and the Dinarides, the ≈100km long Idrija fault, striking N310 and dipping ≈80°NE is often considered as the potential source of the historical 1511 earthquake (estimated macroseismic magnitude: Mm 6.8). Using 1/25,000 to 1/5000 topographical maps, satellite images (SPOT5), 12.5m illuminated DEM and airborne LiDAR data-derived 1-m-DEM, we examined in detail the Idrija fault trace along a 20-km-long swath in the central portion of the fault. Combining topographic and remote sensing data allows characterizing the recent activity along the Idrija fault and estimating its cumulative displacement along strike. Between Tolmin and Godovič, the fault trace is mostly linear but appears divided into three disconnected segments of 11–20-km-long. Morphological evidences such as offset streams and ridges and major drainage abandonments suggest ongoing movement. At three sites, field observations and LiDAR-DEM analysis allow measuring cumulative dextral offsets comprised between 35 and 65m. We found two larger offsets of ≈140m and ≈360m at the southeasternmost site. The vertical component is significant and revealed by a rake ranging from 0 to 33°. The derived N303–N310 striking slip-vector is in agreement with the motion along this fault as suggested by the geodesy. Assuming that the smallest measured offsets have been recorded after the last glacial maximum (LGM, about 20ka ago), the minimum slip-rate for the Idrija fault is about 1.5mm/yr over this period of time. •We provide a detailed mapping of the central portion of the Idrija fault trace.•We quantified cumulative offsets along the fault ranging between 35 and 360m.•A significant vertical component has been found beside the main horizontal motion.•The calculated slip-vector across the fault is in agreement with geodetic data.•The estimated Idrija fault slip-rate is comprised between 1.8 and 3.9mm/yr.