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  2. Point bar - Wikipedia

    en.wikipedia.org/wiki/Point_bar

    The concave bank is often a cut bank and an area of erosion. The eroded material is swept and rolled across the floor of the stream by the secondary flow and may be deposited on the point bar only a small distance downstream from its original location in the concave bank. The point bar typically has a gently sloping floor with shallow water.

  3. Cut bank - Wikipedia

    en.wikipedia.org/wiki/Cut_bank

    A cut bank, also known as a river cliff or river-cut cliff, is the outside bank of a curve in a water channel , 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.

  4. Meander - Wikipedia

    en.wikipedia.org/wiki/Meander

    A cut bank is an often vertical bank or cliff that forms where the outside, concave bank of a meander cuts into the floodplain or valley wall of a river or stream. A cutbank is also known either as a river-cut cliff, river cliff, or a bluff and spelled as cutbank. [1]

  5. Bar (river morphology) - Wikipedia

    en.wikipedia.org/wiki/Bar_(river_morphology)

    Here, at the deepest and fastest part of the stream is the cut bank, the area of a meandering river channel that continuously undergoes erosion. [4] The faster the water in a river channel, the better it is able to pick up greater amounts of sediment, and larger pieces of sediment, which increases the river's bed load. [4]

  6. River channel migration - Wikipedia

    en.wikipedia.org/wiki/River_channel_migration

    This is where the primary process in river channel migration of bank erosion occurs. Often the bank is undercut, another result of the helicoidal flow, which leads to the creation of cut banks. Factors that limit the rate of bank erosion include the rate of deposition of the point bar, stream power, and the critical shear stress of the stream ...

  7. Slip-off slope - Wikipedia

    en.wikipedia.org/wiki/Slip-off_slope

    Slip-off slope (right) and cut bank. The depositional slip-off slope is on the left and a small river cliff on the right. River Ashes Hollow, UK. Schematic cross section of a meandering river channel showing slip-off slope formation. A slip-off slope is a depositional landform that occurs on the inside convex bank of a meandering river.

  8. Rim Rock Wind Farm - Wikipedia

    en.wikipedia.org/wiki/Rim_Rock_Wind_Farm

    Rim Rock Wind Farm is located near Cut Bank, Montana. Owned by NaturEner, this $370 million, 189 megawatt (MW) wind farm has been operational since 2012, and is Montana's largest wind-producing facility to be built in a single phase.

  9. Cut Bank Creek - Wikipedia

    en.wikipedia.org/wiki/Cut_Bank_Creek

    The Cut Bank Creek is a tributary of the Marias River in the Missouri River basin watershed, approximately 75 mi (123 km) long, in northwestern Montana in the United States, which having deeply eroded steep cliff banks eponymously gives name to the cut bank formal terrain term of geological science.