Slow-motion collisions of tectonic plates under the ocean drag about three times more water down into the deep Earth than previously estimated, according to a first-of-its-kind seismic study that spans the Mariana Trench, a crescent-shaped trench in the Western Pacific that measures 1,500 miles long and is the deepest ocean trench in the world.
The observations from the trench have important implications for the global water cycle, according to researchers at Washington University in ...
This is an NSF News item.
Published November 14, 2018 at 11:30PM
Read more at nsf.gov
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