Through constraining the surface slip distribution of displaced landforms along a fault, we can gain important insights into the earthquake rupture histories and recurrence characteristics, thus enabling us to estimate the potential time and magnitude of future earthquakes on the fault. In this study, we constrained the surface slip distribution of displaced landforms along the Sertengshan Piedmont Fault in Northern China based on 1-m-resolution airborne Light Detection and Ranging (LiDAR) data. A total of 600 vertical displacement measurements were acquired along about 185 km stretch of the fault. Through statistically analyzing the displacement observations, we conclude that at least five to seven large surface-rupturing earthquakes have occurred on the Sertengshan Piedmont Fault, displaying a characteristic recurrence pattern with a remarkably regular slip increment of ∼2 m.