What occurs on the inside of a meander bend?

A meander bend is a significant feature in a river or stream where the water curves, creating sections of varied flow dynamics. On the inside of a meander bend, the flow of water is slower than on the outside. This reduction in water velocity causes the river to deposit sediment, which can accumulate over time, forming features such as point bars.

As the water slows down, it loses the energy needed to carry heavy sediment. Consequently, lighter materials such as sand and silt settle on the riverbed. This process of deposition leads to the formation of riparian habitats and, in some cases, can dramatically alter the landscape by creating new landforms.

In contrast, the outside of the bend experiences a faster flow, which leads to increased erosion of the bank due to the powerful water dynamics. Therefore, the inside of the meander bend is characterized by sediment deposition, slower water flow, and the accumulation of materials rather than erosion or stagnation.