Meander Migration

Meander migration refers to the gradual process by which a river's curves, or meanders, shift position over time. As water flows through a bend, it erodes the outer bank where the current is strongest and deposits sediment on the inner bank where flow slows. This continuous erosion and deposition cause the meander to slowly migrate downstream, changing the river's path. Over many years, this movement can create features like oxbow lakes and meander scars. It’s a natural part of a river’s evolution, shaping the landscape through ongoing, dynamic adjustments in its course.