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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 ...
The region is recognized as the world’s type area for karst landform development in the humid tropics and subtropics. The World Heritage Property of South China Karst is a serial property that includes seven karst clusters in four Provinces: Shilin Karst, Libo Karst, Wulong Karst, Guilin Karst, Shibing Karst, Jinfoshan Karst, and Huanjiang Karst.
The shale and sandstone of Silurian lay in the middle of Jinfo from 1000m to 1500m asl.. The low part of Jinfo is supported by the limestone and dolomite of Cambrian and Ordovician. Plenty of small- and microforms of karst are formed in this area. There are many cliffs and gorges in Jinfo Mt., the north slope is steep and the south slope is slight.
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 ...
The county is located in the remote southeastern corner of the prefecture, on the border with Guangxi.Two local sites, Xiaoqikong (小七孔) and Dongduo (洞多), notable for their spectacular karst formations, form part of the multi-site South China Karst UNESCO World Heritage Site inscribed in 2007, which is an area about 550,000 km2 in extent.
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 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.
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]