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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 Plateau (averaging 2100 meters elevation) to the eastern Guangxi Basin (averaging 110 meters elevation).
[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 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.
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The Three Parallel Rivers of Yunnan Protected Areas (Chinese: 云南三江并流; pinyin: Yúnnán Sānjiāng Bìngliú) is a UNESCO World Heritage Site in Yunnan province, China. It lies within the drainage basins of the upper reaches of the Jinsha ( Yangtze ), Lancang ( Mekong ) and Nujiang ( Salween ) rivers, in the Yunnan section of the ...
In the south, the Miao Range steps down to the karst hills of South China. Across the Red River to the southwest, the Ailao Mountains form a definitive barrier. [1] [6] The high mountain peaks of Eastern Tibet are the source of many of Asia's great rivers, which flow southerly towards the Yunnan–Guizhou Plateau. [7]