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2. Seismic and Acoustic Monitoring of Submarine Landslides

3. Detailed monitoring reveals the nature of submarine turbidity currents

5. The submarine Congo Canyon as a conduit for microplastics to the deep sea

6. Seabed seismometers reveal duration and structure of longest runout sediment flows on Earth

8. Carbon and sediment fluxes inhibited in the submarine Congo Canyon by landslide-damming

9. Longest sediment flows yet measured show how major rivers connect efficiently to deep sea

10. First source-to-sink monitoring shows dense head controls sediment flux and runout in turbidity currents

11. Fill, flush or shuffle: How is sediment carried through submarine channels to build lobes?

12. Morphometric fingerprinting of submarine canyon and channel processes revealed by time-lapse bathymetric surveys from the Congo Fan

14. How turbidity currents dictate organic carbon fluxes across river-fed fjords

15. How turbidity currents dictate organic carbon fluxes across river-fed fjords

16. Near‐Bed Structure of Sediment Gravity Flows Measured by Motion‐Sensing “Boulder‐Like” Benthic Event Detectors (BEDs) in Monterey Canyon

18. Flood and tides trigger longest measured sediment flow that accelerates for thousand kilometers into deep-sea

20. The formation and evolution of submarine headless channels

21. Novel sensor array helps to understand submarine cable faults off West Africa

22. Knickpoints and crescentic bedform interactions in submarine channels

23. Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers

24. Effects of extreme events on the morphology of submarine channels: the case of the Elliot hazard cascade

25. A field-scale laboratory to study particulate transport from river source to marine sink: Bute Inlet (Canada)

31. Author Correction: Rapidly-migrating and internally-generated knickpoints can control submarine channel evolution

32. Global monitoring data shows grain size controls turbidity current structure

34. Rapidly-migrating and internally-generated knickpoints can control submarine channel evolution

36. First direct monitoring and time-lapse mapping starts to reveal how a large submarine fan works

38. What determines the downstream evolution of turbidity currents?

40. Lessons learned from the monitoring of turbidity currents and guidance for future platform designs

42. Modern Submarine Landslide Complexes

43. Sediment and organic carbon transport and deposition driven by internal tides along Monterey Canyon, offshore California

44. Direct Monitoring Reveals Initiation of Turbidity Currents From Extremely Dilute River Plumes

46. Linking Direct Measurements of Turbidity Currents to Submarine Canyon-Floor Deposits

50. Powerful turbidity currents driven by dense basal layers

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