Meandering rivers are characterized by sinuous bends and curves in their channels. As water flows through a meandering river, it creates a centrifugal force that causes the water to move faster on the outside of the bends and slower on the inside. This differential in water velocity leads to erosion on the outside of the bends and deposition on the inside. Over time, this process can cause the river to widen its channel while maintaining a relatively shallow depth.
