Quantitative study on the geomorphic indices has been carried out on five gullies in the middle of northern front of Liulengshan Mountains. The abnormal values of the indices, including stream length-gradient index (SL index), hypsometric integral (HI), and index of drainage basin shape (Bs), reveal that the evolution of the five gullies has obvious relationship with the neotectonic movement along the northern front of Liulengshan Mountains and the drainage basins are currently in the mature period of geomorphic evolution. The field investigation of the Qiulin gully tests demonstrates the Late Quaternary activities of the fault along the northern front of Liulengshan Mountains.