Geology of China

Clockwise from upper left: Li River karst, Mount Everest's north face, loess landscape in Datong and Zhangye National Geopark.

The geology of China (or the geological structure of the People's Republic of China) consists of three Precambrian cratons surrounded by a number of orogenic belts. The modern tectonic environment is dominated by the continued collision of India with the rest of Asia starting 40–50 million years ago. This has formed the Himalayas and continues to deform most of China.[1] China has vast mineral reserves,[2] a significant earthquake risk in its western regions and rare isolated active volcanoes throughout the country.[3]

Many geological concepts were discovered very early in China's history. However, it was not until the adoption of European natural science in the late 19th century that geology became a science in China.[4]

  1. ^ "Asia - Geologic history". Encyclopedia Britannica. Retrieved 2019-04-08.
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