Where does fast flow typically occur in a river bend?

Fast flow in a river bend occurs on the outside of the bend due to the hydrodynamics at play in the river's meandering system. When water flows around a curve, it tends to be pushed outward by centrifugal force, which increases the velocity of the water on the outer edge. This results in deeper water because the current is stronger and can erode the bank more effectively. Consequently, this area is often characterized by faster-moving water and more active erosion.

In contrast, the inside of the bend experiences slower flow as the water moves more gently and tends to deposit sediment, leading to the formation of point bars. Thus, the river's flow patterns create a dynamic interaction between erosion on the outside of the bend and deposition on the inside.