Zhangjiajie Geography

The geological formation of Zhangjiajie belongs to the New Cathaysian tectonic system. About three billion and eight thousand years ago, this place was a large patch of ocean. After a series of geological changes including Wuling-xuefeng, Indo-china, Yanshan, Himalayan and Neotectonic movements, the bottom of ocean rose out of the surface, and the quartzite sandstone pillars and peaks took shape after the gradual cutting, eroding and crumbling of Nature for millions of years.

The entire area is covered with towering cliffs of sandstone of quartz and dense unspoiled forests that conceal fantastic caves full of stalactites and stalagmites. The quartzite sandstone hills in Wulingyuan are unique in their large number and fairly pure composition (being 75-95% of quartz). With the changes of seasons and the weather, they constantly present different views to spectators. The highest peak in this area is Tuerwangyue Feng or Rabbit Watching the Moon Peak and Mt. Tianzi is particularly recommended for its good view.