Which type of river channel is most likely to change shape due to varying sediment deposits?

A braided river channel is characterized by multiple interwoven channels that are separated by small islands or bars of sediment. This type of river is particularly dynamic and prone to changing shape because it consists of numerous channels that can shift and evolve in response to variations in sediment deposition.

When water flow is variable, whether due to seasonal changes or fluctuations in precipitation, sediment can accumulate in certain areas, creating new islands or bars and altering the flow paths of the water. As a result, braided rivers can quickly adapt their structure based on these sediment dynamics.

In contrast, straight rivers typically maintain a consistent flow path and shape due to their efficient flow, while meandering rivers change shape more gradually as they erode and deposit sediment along the riverbanks. Delta rivers, on the other hand, are primarily shaped by the interaction of river sediment as it meets a larger body of water, leading to a fan-like distribution, but are less prone to rapid shape changes compared to braided rivers.