Where is slow flow generally found in a river bend?

Slow flow is generally found on the inside of a river bend due to the dynamics of water movement. When a river meanders, the water on the outside of the bend is traveling faster because it is deeper and has a steeper gradient. This acceleration leads to the formation of erosion on the outer bank, creating features like cliffs or cut banks.

Conversely, on the inside of the bend, the water depth is usually shallower, and the gradient is less steep, causing the water to flow more slowly. The slow flow allows sediment to be deposited, leading to the formation of features such as point bars. This difference in flow velocity plays a significant role in shaping the river's landscape, as the alternating fast and slow flows contribute to the river's meandering nature and changing morphology. Understanding this concept is crucial for grasping how rivers interact with their environments and evolve over time.