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Flow in Earth's Mantle Moves Mountains


June 3, 2010

dynamic topography and mantle flow A study published in Nature suggests that some mountains in "mobile belts"--regions of crustal fragments, such as in the Mediterranean, the Rockies and the Himalayas--can rise due to upward pressure from the semi-liquid mantle. The study proposes a model for predicting uplift and likely volcanic hotspots in such regions. Full Story

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University of Southern California

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