Geoscientists reveal how Earth's forces are shaping the 'Roof of the World'
Geoscientists have discovered that the Tibetan Plateau's unique topography is driven by deep-earth processes involving the Indian plate pushing beneath the Asian plate. The study reveals distinct east-west geological histories that influence the region's climate and water resources.
Why it matters
Understanding the geological formation of the Tibetan Plateau is crucial for climate modeling and managing water security for billions of people who rely on the region's rivers.
edited by Sadie Harley , reviewed by Andrew Zinin
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Add as preferred source Natural-colour satellite image of the Tibetan Plateau. Credit: NASA Geoscientists at the University of Glasgow have helped reveal new evidence about the formation of one of the highest mountainous areas on Earth—the Tibetan Plateau. A study by an international team of Chinese and U.K. geoscientists shows that the unique topography at the summit of the plateau is shaped by processes going on deep in Earth.
These features clearly indicate how far the Indian continental plate, to the south, has been pushed beneath the Asian plate, to the north, highlighting the connection between Earth's interior and its surface features.
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