Sediment en route to oblivion

Philip A. Allen
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Philip A. Allen: Imperial College London, South Kensington Campus, London SW7 2AZ, UK. philip.allen@imperial.ac.uk

Nature, 2007, vol. 450, issue 7169, 490-491

Abstract: Sudden collapses of the sea floor can generate oceanic sediment flows that dwarf the global annual sediment input from rivers. Such flows can travel great distances, and undergo transformation along the way.

Date: 2007
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DOI: 10.1038/450490a

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