The Shanxi Rift System or Fen-Wei Rift System [1] 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 individual rift basins that make up the rift system have an overall en echelon geometry.. La vallée du Grand Rift est le nom donné en 1894 par l' explorateur écossais John Walter Gregory 1, après son voyage en Afrique orientale britannique 2, à un ensemble géologique constitué d'une série de failles et de volcans, situé en Afrique de l'Est . Également appelée rift est-africain ou « grande faille est-africaine », cette.

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The rift valley, characterized by Nestled within the expansive Loess Plateau in north-central China, the Pinglu Rift Valley stands as a testament to the Earth's dynamic geological history. Encompassing an area of approximately 400,000 square kilometers, this remarkable feature is a striking example of the Earth's ever-evolving crust, shaped by forces deep within our planet.. Pinglu Rift Valley, located in the vast Loess Plateau of north-central China, testifies to the dynamic geological history of the Earth. Covering an area of nearly 400,000 square kilometers, this remarkable feature is a striking example of the constant evolution of the Earth's shell, shaped by the influential forces deep within our planet.