The channel cross profile (or section) is the view of the river bed and banks from one side to the other side at any one point on its course. As a river flows from its source to its mouth, a number of typical changes takes place in the channel morphology. In the upper course, the channel is narrow and uneven, because of the presence of deposited boulders. Where both banks are being eroded channels tend to be broadly rectangular in shape. As the river enters its middle course and starts to meander, the channel becomes asymmetrical on the river bends but mainly smooth and symmetrical on the straight stretches. In the lower course, the river widens and deepens further, but banks of deposition and eyots (islands of deposition) can disrupt the shape of the channel cross section, leading to a braided channel. Sometimes embankments called levees can be seen on either side of the channel. Levees can also be man-made.
The shape of the channel influences the velocity of the river. In the upper course, where the channel is narrow and uneven due to the presence of large boulders, there is a large wetted perimeter. The wetted perimeter is the total length of the river bed and banks in cross section that are in contact with the water in the channel.
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