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- W1488968421 abstract "Mid-ocean ridges are locations underwater where magma rises to form new crust. Seawater that circulates near the magma is heated and emitted as a hydrothermal plume that rises from the sea floor. As Speer discusses in his research commentary, new results in the same issue by [ Lupton et al ][1]. offer the first direct look at the behavior of this rising plume. Using a combination of physical and chemical surveys, together with a drifting probe that could be submersed to a depth of 2 kilometers, Lupton et al . were able to map out the anticyclone pattern expected of a rising hydrothermal plume. [1]: http://www.sciencemag.org/cgi/content/short/280/5366/1052" @default.
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- W1488968421 date "1998-05-15" @default.
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- W1488968421 title "GEOPHYSICS: Enhanced: A New Spin on Hydrothermal Plumes" @default.
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- W1488968421 doi "https://doi.org/10.1126/science.280.5366.1034" @default.
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