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  2. Guilin Scenic Area - Wikipedia

    en.wikipedia.org/wiki/Guilin_Scenic_Area

    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]

  3. South China Karst - Wikipedia

    en.wikipedia.org/wiki/South_China_Karst

    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.

  4. Guilin - Wikipedia

    en.wikipedia.org/wiki/Guilin

    The karsts surrounding Guilin are made of Triassic period limestone and dolomite rocks. The Li River flows through the city. Hills and mountains: Diecai Hill (叠彩山), Elephant Trunk Hill, Wave-Subduing Hill (伏波山), Lipu Mountains, Kitten Mountain, the highest peak of Guangxi, and Yao Hill (尧山) Caves: Reed Flute Cave, Seven-star Cave

  5. Yangshuo County - Wikipedia

    en.wikipedia.org/wiki/Yangshuo_County

    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 ...

  6. Geology of China - Wikipedia

    en.wikipedia.org/wiki/Geology_of_China

    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 .

  7. Li River - Wikipedia

    en.wikipedia.org/wiki/Li_River

    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 ...