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The Shanxi Rift System or Fen–Wei Rift System is a zone of active extensional tectonics that forms the eastern margin of the Ordos Block in northern China. The zone extends for at least 900 km (560 mi) and runs south-southwest to north-northeast.
The Huadong Valley or Hualien–Taitung Valley (Chinese: 花東縱谷; pinyin: Huādōng Zònggǔ; Wade–Giles: Hua 1-tung 1 Tsung 4-ku 3), also known as East Rift Valley, the Longitudinal Valley or as the Nakasendō Plain (中仙道平野, Nakasendō Heiya) during the era of Japanese rule, is a long and narrow valley located between the ...
This Rift Valley is located in Pinglu, Shanxi on the Loess Plateau, a mountainous area in north-central China that covers about 400,000 square kilometers. It was formed because of movements inside the Earth’s crust and is about 10 km long.
Apr 3, 2024 · Deep within China lies a geological wonder - the Pinglu Rift Valley. Millions of years in the making, this valley offers a glimpse into the Earth's dynamic past.
Mar 10, 2023 · The rift valley is located in Pinglu, Shanxi on the Loess Plateau, a highland area in north-central China covering some 400,000 square km. It was formed due to movements within the earth's...
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Jan 4, 2024 · A rift valley is a lowland region that forms where Earth’s tectonic plates move apart, or rift. Rift valleys are found on land and at the bottom of the ocean, where they are created by the process of seafloor spreading.
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Oct 18, 2023 · Learn about the history and features of Pinglu Rift Valley, a remarkable feature of the Loess Plateau in north-central China. Discover how tectonic forces shaped this valley and its rich biodiversity.
