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Courtney K. Harris, Jaia Syvitski, H.G. Arango, E.H. Meiburg, Sagy Cohen, C.J. Jenkins, Justin J. Birchler, E.W.H. Hutton, T.A. Kniskern, S. Radhakrishnan and Guillermo Auad
Turbidity currents deliver sediment rapidly from the continental shelf to the slope and beyond; and can be triggered by processes such as shelf resuspension during oceanic storms; mass failure of slope deposits due to sediment- and wave-pressure loadings...
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