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Geological Scenic Spots in Tiantai Mountain Park Area------ Duitain Valley

This scenic spot is located in Tiantai Mountain Scenic Spot of Tiantai Mountain Park Area, with an elevation of 343m and an area of 15000. The Neoproterozoic Qingbaikou system Baiyun albite quartz schist is developed on both sides of the valley. Duitian Valley is formed and developed under the action of water erosion. The water flow and Duitian Valley wind ups and downs, the aged-pines grow on the cliff and the stream and dangerous shoal are main features of this scenic spot; at the same time, the sediment erosion makes river valley downcut and the lateral erosion of the water flow makes valley slope eroded and retreated, including sheet erosion, gully erosion, block body collapse on the valley slope. The headward erosion makes the valley extend upward and lengthen.


Ministry of Land and Resources P.R. ChinaDepartment of Land and Resources of Hubei ProvincePeople’s Government of HuanggangHuanggang Municipal Bureau of Land and ResourcesGlobal Geoparks NetworkNational Geopark of China The Geological Museum of ChinaHong Kong UNESCO Global GeoparkShennongjia Global GeoparkTianzhushan Global Geopark




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