Fig. 1
From: New flow relaxation mechanism explains scour fields at the end of submarine channels

Examples of systems with a loss of confinement. a Sketch of a channel-lobe transition zone based on bathymetrical surveys. Modified from ref. 13. b The Squamish Delta. In the upper bathymetry map, the channel termination is marked by a rapid loss of confinement43. The lower bathymetry map was obtained 5 years later and shows how erosion has led the propagation of the channel by ~400 m41