No.13

Located on the ridge between Renshenguo Flat in Shuangqiao Valley and Lianghekou in Changping Valley, with the highest point at an altitude of 5430 m. Tectonic activity, lithological differences, and differential erosion formed the tilted syncline represented by Wuse Mountain, a typical example of the smaller curvature syncline mountains in the Xiaojin Arc Structural Belt.