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Explore groundbreaking research on submarine channels through this hour-long lecture that reveals revolutionary findings about deep-sea turbidity currents. Discover how direct flow measurements at the termination of the Congo Submarine Channel have overturned long-held assumptions about sediment transport in the deep ocean. Learn about the surprising frequency and duration of sediment flows in submarine channels that rival the world's largest rivers, with the Congo channel remaining active for approximately 15% of the time over a 14-month monitoring period. Examine how individual flows can persist for weeks to months, transporting sediment over distances exceeding 1,000 kilometers from shore at water depths of around 5 kilometers. Understand the implications of exceptionally efficient sediment and organic carbon transfer that matches the flux supplied by the Congo River itself. Investigate how these sustained flows create unique deep-sea ecosystems and drive rapid submarine channel extension through previously unknown mechanisms involving non-erosional mud-flows rather than traditional erosional processes. Gain insights into how these findings challenge conventional understanding of deep-sea sediment transport and reveal the dynamic nature of Earth's largest sediment accumulation systems.
