The Li River: A 20-Million-Year-Old Masterpiece of Limestone and Water

The Li River: A 20-Million-Year-Old Masterpiece of Limestone and Water
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In short: Flowing through China's Guangxi region, the Li River is more than a scenic waterway. It is the heart of a dramatic karst landscape shaped by millions of years of tectonic uplift and erosion. From ancient canals to iconic tower peaks, this river system holds secrets of both geology and history.

The Li River, or Li Jiang, serves as the upper reach of the Gui River within the Pearl River basin. Spanning 164 kilometres from Xing'an County to Pingle County, it acts as a vital artery in northeastern Guangxi. Its historical significance is anchored by the Lingqu Canal, constructed in 214 BC. As one of ancient China's three major water conservation projects, this canal linked the Li and Gui Rivers to the Xiang River, creating a crucial waterway that connected the Yangtze valley to the Pearl delta.

The river's dramatic scenery is defined by 2,600 metres of Devonian and Carboniferous limestones. Over the last 10 to 20 million years, these rocks have evolved into two distinct karst formations: Fengcong and Fenglin. Fengcong, or peak cluster depression karst, dominates the river's course with its deep depressions and hundreds of caves, including the extensive Guanyan Cave System. In contrast, the area around Yangshuo is characterized by Fenglin, or peak forest plain, featuring isolated, near-vertical limestone towers that can reach heights of 300 metres.

These formations are the result of slow tectonic uplift associated with the Himalayan orogenic zone, combined with the gradual erosion of the limestone towers. Beyond its geological marvels, the river is a cultural icon, famously depicted on the 20 yuan note and known for traditional cormorant fishing. Today, the region attracts millions of visitors annually, drawn to landmarks like the Elephant-Trunk Hill in Guilin and the intricate stalactites of the Reed Flute Cave, which showcase the enduring power of water on stone.

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