Marine turbidity currents can be generated by submarine landslides or by sediment load from rivers, both of which act to increase the density of water. This high-density water then propagates along the sea floor, powered by its own density anomaly.
The standard theory for river-induced turbidity currents is that a large sediment input from the river is required. Hage et al.  turn that theory on its head. They demonstrate that turbidity currents can, in fact, be generated from rivers with a very small sediment load. The case is made with an incredibly detailed set of measurements which catch a short (6 minute) turbidity current in the act of forming and dissipating – even showing the change in sea floor bathymetry after the event. These results will lead to a re-evaluation of how and when turbidity currents form.
Citation: Hage, S., Cartigny, M. J. B., Sumner, E. J., Clare, M. A., Hughes Clarke, J. E., Talling, P. J., et al . Direct Monitoring Reveals Initiation of Turbidity Currents From Extremely Dilute River Plumes. Geophysical Research Letters, 46. https://doi.org/10.1029/2019GL084526
—Andrew M. Hogg, Editor, Geophysical Research Letters