Cliff Rivers
Bank erosion and point bar deposition as seen on the Powder River in Montana.
Image by United States Geological Survey, via Wikimedia Commons. Licensed Public domain

Cliff Rivers

Cut bank Cut bank Outside bank of a water channel, which is continually undergoing erosion For other uses, see Cut Bank (disambiguation). A cut bank, also known as a river cliff or river-cut cliff, is the outside bank of a curve (meander) in a water channel (stream), which is continually undergoing erosion.[1] Cut banks are found in abundance along mature or meandering streams, they are located opposite the slip-off slope on the inside of the stream meander. They are shaped much like a small cliff, and are formed as the stream collides with the river bank. It is the opposite of a point bar, which is an area of deposition of material eroded upstream in a cut bank.[2] This article…

(Source: Wikipedia)


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