Which feature is considered a depositional feature inside a meander bend?

A point bar is indeed considered a depositional feature inside a meander bend. This area forms as the water flows more slowly on the inside of a bend compared to the outside, leading to sedimentation. As the current slows down, it allows sediments carried by the water to settle out of the flow, thus accumulating on the inside of the meander bend, creating the point bar.

The process of erosion on the outside of the bend contributes to creating a cut bank, which is an area where the bank is eroded away due to the stronger current, making it distinct from the depositional processes at play on the inside. The stream channel refers to the entire path the river takes, encompassing both erosion and deposition activities but does not specifically denote where new sediment accumulates in the context of a meander bend. A horse-shoe bend, while related to the shape of a meander, is also not specifically a depositional feature, but rather a descriptive term for a certain configuration of the river curve.