Structuring the inner core

John Lister
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John Lister: John Lister is at the Institute of Theoretical Geophysics, University of Cambridge, Cambridge CB3 0WA, UK. lister@damtp.cam.ac.uk

Nature, 2008, vol. 454, issue 7205, 701-702

Abstract: Earth's rocky mantle and solid inner core are separated by the 2,300-kilometre-deep layer of molten iron that constitutes the outer core. Yet the sluggish pattern of mantle convection creates structure in the inner core.

Date: 2008
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DOI: 10.1038/454701a

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