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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]
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.
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.
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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Yet, it is the 2,600-metre (8,500 ft) of Devonian and Carboniferous limestones and karst terrain within the Guilin basin, that gives the area a dramatic landscape. Two distinctive types of karst are found, Fengcong, and Fenglin, which have evolved for the past 10-20 million years, within the Cenozoic. [1] Fog on the Li River