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Geological Scenic Spots in Tiantai Mountain Park Area----- Qingbaikou System Wudang Quartz Plate Rock (Rocks) Group

This scenic spot is at the side of the road about 50m far away from the gate of Tiantai Mountain Scenic Spot of Tiantai Mountain Park Area, with an elevation of 164.3m and an area of 100. It belongs to ancient metamorphic strata section (scientific investigation line). The metamorphic strata is Neoproterozoic Wudang (Rock) Group, the lithology is mainly Baiyun albite quartz schist epidote Baiyun albite schist, is the volcanic sedimentary formation focused on acidic volcanic eruption and has medium-fine grained structure and gneissic structure. Before the period of Qingbaikou, the Yangtze plate and the North China plate are separated by Paleo-China Ocean and finally complete the combination after long-term collection. During this period, the tree land parcels interact with each other and form a set of middle-shallow metamorphic sedimentary volcanic rock series- Wudang Rock Group. In the formation process, it experiences three stages, namely detrital rock sedimentation, Shuangfeng Mountain volcanic eruption sedimentation and deformation and metamorphism reformation.

Ministry of Natural Resources of P. R. ChinaDepartment of Natural Resources of Hubei ProvincePeople’s Government of HuanggangHuanggang Natural Resources and Planning BureauGlobal Geoparks NetworkNational Geopark of China The Geological Museum of ChinaHong Kong UNESCO Global GeoparkShennongjia Global GeoparkTianzhushan Global Geopark

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