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He Jingzhi composed the "Song of Guilin Scenic Area" [Note 2] during his visit to Guilin. Over 800 years ago, during the Southern Song dynasty, Wang Zhenggong wrote the famous line "Guilin's landscape is the best under heaven [Note 3] in his poem "A Grand Banquet Encouraging the Emperor", [Note 4] which made Guilin's scenery renowned worldwide.
Typical karst terrain of the Dinaric Alps Lijiang fengcong in Guilin as part of the South China Karst Karst formation of the Serra de Tramuntana. Karst (/ k ɑːr s t /) is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite.
In 1921, Guilin became one of the headquarters of the Northern Expeditionary Army led by Sun Yat-sen. [8] In 1940, Guilin City was established. [9] [10] Guilin was the provincial capital of Guangxi before 1912 and from 1936 to 1949. Guilin became one of the most important military, transport, and cultural centers of China during World War II.
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.
Yangshuo County (simplified Chinese: 阳朔县; traditional Chinese: 陽朔 縣; pinyin: Yángshuò Xiàn) is a county under the jurisdiction of Guilin City, in the northeast of Guangxi, China. Its seat is located in Yangshuo Town. Surrounded by karst peaks and bordered on one side by the Li River, it is served by bus and by boat from nearby ...
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 ...
Karst topography is a geological formation shaped by the dissolution of a layer or layers of soluble bedrock, usually carbonate rock such as limestone or dolomite, but also in gypsum. [1] It has also been documented for weathering -resistant rocks, such as quartzite , given the right conditions. [ 2 ]
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