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River Enviroments (River Processes (Erosion (Hydraulic action (Water hits…
River Enviroments
River Processes
Erosion
Hydraulic action
Water hits the river bed and banks with force which means the material is dislodged and carried away.
Corrosion
Minerals in the rocks forming the sides of the river channel are dissolved by the water flowing past them
Abrasion
Material being carried by a river is rubbed against the sides of channel, widening and deepening the channel
Corrasion
Wearing away at the river bed and banks by the load (particles of rock carried by the river) hitting against them.
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River landforms
Upper Course features
V- shaped Valley
The water flows quickly downhill, eroding the water vertically. The river then deepens and widens its valley (using processes such as hydraulic action, corrasion and corrosion).
Interlocking Spurs
The river erodes the landscape in the upper course, it winds and bends to avoid areas of hard rock
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Waterfalls
The river flows over bands of softer and harder rocks, and the softer rock is eroded quicker. Because of this the river undercuts the harder rock leaving an overhang. The river then quickly forms a plunge pool below the waterfall. Overhang rock is left unsupported which causes the river to move upstream. The process continues and a gorge is cut into the hillside.
Middle Course features
Meanders
Forms as the river erodes laterally, to the right side then the left side.
Ox bow lakes
Upstream a large bend becomes a horseshoe and is eventually cut-off to become an oxbow lake. Downstream the river is eroding its outer bank and depositing on its inner bank to create a new meander
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