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The scientific significance of Guilin's landscape is from the concentration of the Guilin-Yangshuo type of peak forest karst landforms. These formations are internationally recognized by the karst community as the world's typical representative of peak forest karst landforms and a model of tropical and subtropical peak forest landforms. [18] [19]
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.
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 ...
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.
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.
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 ]
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 ...
China's karst regions are almost all formed in rocks of Devonian to Triassic age. [11] [12] Near Guilin the lowering of the base level, through uplift and river erosion, has formed prominent karst hills. It is estimated that the river erodes down 50–100 mm/kyr, from this the age of the karst landscape is estimated at 10–20 million years .