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In a river bend, the outside of the bend carries the largest sediment due to faster water flow, causing erosion and deposition.
In a river bend, the fastest moving water is on the outside of the bend, near the cutbank. This faster velocity on the outside bend leads to more erosion on that side, forming a feature called a cut bank. On the inside bend of the river, where the water flows slower, sediment tends to settle out due to reduced velocity, creating deposition and forming point bars.
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