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River Landscapes (Integrated River Management Scheme at Banburry (Hard…
River Landscapes
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Fluvial Processes
Erosion
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Solution: when the river flows over limestone or chalk, the rock slowly dissolves
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Deposition
Larger rocks tend to be deposited in the upper course because they can only be transported for short distances by traction
Finer sediment held in suspension is carried further down stream and is deposited on river beds or banks when velocity is slowed by friction
A large amount of deposition occurs at the river mouth, where the interaction with tides, along with the very gently gradient, greatly reduces the river's velocity
Fluvial Landforms
Upper Course
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Gorges
Found immediately downstream of a waterfall (as it is formed by the gradual retreat of a waterfall over hundreds/thousands of years
Waterfalls
The more resistant rock on top is eroded faster then the softer rock beneath, causing the bottom to be eroded faster (creating an undercut and a plunge pool). The overhang then collapses, causing the waterfall to retreat backwards to the source
Spurs
Small volume and low efficiency means the water can't erode through interlocking spurs, so it flows around them instead
Middle Course
Meanders
Wide bends, constantly changing position due to the balance of erosion and deposition
Pools: Deep sections on the outside of a bend, as the faster moving water erodes a deep channel
Riffles: Shallow section on the inside of a bend, as the slower moving water deposits sediment
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Ox-bow lakes
Narrowing meander necks are completely broken through to form a straighter channel, the old meander is cut off by deposition to form a separate ox-bow lake