How to buy student tickets for Wugong Mountain

Student tickets for Wugong Mountain can be purchased directly at the ticket office with your student ID card.

Wugong Mountain is located in the northern section of the Luoxiao Mountains, spanning the two provinces of Hunan and Jiangxi. In history, it was as famous as Hengshan Mountain and Lushan Mountain, and was also known as the three famous mountains in the south of the Yangtze River. The main peak, Jinding Baihe Peak, is 1,918.3 meters above sea level. It is a large-scale mountainous natural scenic area integrating sightseeing, leisure vacation, religious tourism and popular science education.

Wugong Mountain Scenic Area is famous for its strange peaks, dangerous rocks, dangerous rocks, strange pines, vast grass, soul of clouds, ease of fog, rapid waterfalls, secluded pools and strange caves. , famous for its delicacies. In particular, the alpine meadows among the clouds, the Red Rock Valley Waterfalls, and the Jinding Ancient Altar Group are the three most stunning sights in the south of the Yangtze River and are fascinating. So far, hundreds of thousands of acres of primary forest and secondary forest remain, including more than 2,000 species of seed plants, ferns, mosses, large fungi, and rare tree species such as luminous trees, ginkgo, and yew.

The address composition of Wugong Mountain

The Wugong Mountain area is located on the northern edge of the South China Plate and borders the Yangtze Plate to the north. The exposed strata in the area include the Sinian Yangjiaqiao Group Gujia Formation and Xiafang Formation. Formation and Dashajian Formation, Lechangxia Group Bali Formation and Laohutang Formation, Early Cambrian Bacun Group Niujiaohe Formation, Gaotan Formation, Shuishi Formation and Wentangyan Formation are mainly composed of ferrosilicon-like flysch structures .

The Devonian strata are a combination of clastic rocks and carbonate rocks, and are overlain by regional unconformity on the pre-Devonian shallow metamorphic rock series strata; the early Triassic strata are composed of carbonate rocks. Mainly composed of rocks, intercalated with clastic rocks and late Triassic age, the Jurassic strata developed coal-bearing clastic rock series and clastic rock series, and the late Cretaceous strata were a set of continental red rock series.