In a river, erosion dominates at the cutbank. a. true
A cut bank, otherwise called a stream precipice or waterway cut bluff, is the external bank of a bend or wander in a water channel (stream), which is persistently going through erosion.
Cut banks are found in overflow along developed or wandering streams, they are situated outwardly of a stream twist, known as a wander, inverse the sneak off slant within the curve.
They are molded similar as a little precipice, and are shaped by the disintegration of soil as the stream slams into the waterway bank. Instead of a point bar, which is an area of statement, a cut bank is an area of erosion.
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