A part of old county town of Hanyuan, Shaanxi Province lied on the front accumulation body of the Beihoushan Mountain landslide. The geomorphology, strata, type of rock and soil, geologic structures in the Beihoushan Mountain area were investigated. An old landslide in the Beihoushan Mountain was revealed. The boundary of old landslide was delimited. And effects of old landslide on earthquake damage of old Hanyuan County were analyzed. The predominant periods of the Beihoushan Mountain landslide were estimated using ADINA. The predominant periods of strong ground motion records near old Hanyuan County were closed to those of the old landslide.