摘要
The Tianmushan Mountain, running SW-NE, is situated along the Anhui-Zhejiang and Anhui-Jiangsu provincial borders. The main peaks such as Mt. East Tianmushan, Mr. West Tianmushan and Mt. Qingliang (1787m a.s.l.) are all higher than 1500 m a.s.l. The mountain range, acted by orogeny and the Quatèrnary glaciation, became the
