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Channel shape in rivers changes due to a combination of factors including sediment transport, water flow dynamics, and geological conditions. Erosion occurs on the outer banks where the water flows faster, while sediment deposition happens on the inner banks where the flow is slower. This process leads to the development of features like meanders and oxbow lakes over time. Additionally, changes in vegetation, human activities, and seasonal variations in water levels can further influence channel morphology.

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1mo ago

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