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[1] [2] The region's natural scenery is characterized by its mountains, rivers, karst caves, historic sites and stone carvings. On June 24, 2014, Guilin, along with Shibing in Guizhou, Mount Jinfo in Chongqing and Huanjiang in Guangxi, was inscribed on the World Heritage List as part of the South China Karst at the 38th World Heritage ...
UNESCO describes the South China Karst as "unrivalled in terms of the diversity of its karst features and landscapes". [1] The huge karst area of South China is about 550,000 km 2 in extent. The karst terrain displays a geomorphic transition as the terrain gradually descends about 2000 meters over 700 kilometers from the western Yunnan-Guizhou ...
The Wulong Karst (Chinese: 武隆喀斯特) is a karst landscape located within the borders of Wulong District, Chongqing Municipality, People's Republic of China. It is divided into three areas containing the Three Natural Bridges , the Qingkou Tiankeng (箐口天坑) and Furong Cave respectively.
Furong Cave (Chinese: 芙蓉洞) is a karst cave located on the banks of the Furong River, 20 km (12 mi) from the seat of Wulong District, Chongqing, People's Republic of China. [ 1 ] History
The Three Natural Bridges (simplified Chinese: 天生三桥; traditional Chinese: 天生三橋; pinyin: Tiānshēng Sān Qiáo) are a series of natural limestone bridges located in Xiannüshan Town (仙女山镇), Wulong District, Chongqing Municipality, China. [1] They lie within the Wulong Karst National Geology Park, itself a part of the ...
Fengcong karst dominates the course of the Li River and is defined as a group of limestone hills with a common limestone base, with deep depressions (or dolines) between the peaks, and sometimes described as peak cluster depression karst. Hundreds of caves are present in this terrain, with 23 having passages longer than -1 km alongside the Li ...
The South China Craton (also Yangtze Craton) is younger than the North China Craton and ranges in age from 2.5 to 0.8 billion years old. [1] The South China Craton is divided into three parts, western, central and eastern. [22] Unlike the North China Craton the South China Craton used to be part of Gondwana. [20]
About 23 Ma, movement of the Himalayan range disturbed the land around the Danxia landform in the Guangdong Province of China uplifting and completely changing the topography of the area. [6] Over millions of years the steep cliffs that can be seen today, exposed by faults, were formed through weathering and erosion.