A
cut bank, also known as a
river cliff or
river-cut cliff, is the outside bank of a water channel (
stream), which is continually undergoing erosion. Cut banks are found in abundance along mature or meandering streams, they are located on the
outside of a stream bend, known as a
meander, opposite the
slip-off slope on the inside of the bend. They are shaped much like a small
cliff, and are formed by the erosion of soil as the stream collides with the river bank. As opposed to a
point bar which is an area of
deposition, a cut bank is an area of
erosion.