The responding to neotectonic movement in Wujiawan River, which runs through transition area of two geomorphic units of Taihang Mountains and the North China Plain, is more sensitively than other water systems in Taihang Mountains, so it can record the history of uplift better. By the field investigation of sequence and sedimentary features, dating of optical stimulated luminescence (OSL), the conclusions can be reached that there are four levels of river terraces in Pingdian River. This study is of great value, which provides actual material for the research of river terrace and neotectonic movement on the southern margin of Taihang Mountains.