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Explain the formation of an oxbow lake (4 mark)
Due to erosion on the outside of a bend and deposition on the inside, the shape of a meander will change over a period of time.
Erosion narrows the neck of the land within the meander and as the process continues, the meanders move closer together.
When there is a very high discharge (usually during a flood), the river cuts across the neck, taking a new, straighter, and shorter route.
Deposition will occur to cut off the original meander, leaving a horseshoe-shaped oxbow lake.
RFOHRWSMEERU OTTSRWWMRBPHA&ACaW WHBFGF EDHCPP UTHR GTWRULBaSSG ETOHCRBO GRF\*&GL \ \-The river flows over an area of hard rock with softer, more easily eroded rock underneath. \-Over time the softer rock is worn way more rapidly by processes of hydraulic action and abrasion, creating a waterfall. * The water hits the bottom of the falls with great force. This erodes a deep hole creating a plunge pool. * The softer underlying rock is eroded and weakened. The softer layer collapses into the plunge pool, undercutting the hard rock. * The hard rock cracks and then collapses. * Gradually, the waterfall retreats upstream, leaving behind a steep-sided gorge. Every time the overhanging cap rock breaks off the gorge retreats further and grows longer. (-There is turbulent fast flowing water in the gorge)
How are river levees formed (4 Marks)
Levées are long, narrow ridges or raised embankments alongside the river. composed of gravel, stones, and alluvium. Steeper on the channel side than landside
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• Levées occur in the lower course of a river when there is an increase in the volume of water flowing downstream and flooding occurs.
• Sediment that has been eroded further upstream is transported downstream.
• When the river floods, the sediment spreads out across the floodplain. Friction with the land reduces velocity and causes deposition.
• When a flood occurs, the river loses energy. The largest material (sand and gravel) is deposited first on the sides of the river banks and smaller materials (finer silt and mud) further away.
• After many floods, the sediment builds up to increase the height of the river banks, so the levees become higher than the surrounding floodplain.
• If a severe flood event occurs, levées may burst and cause serious damage to the surrounding land.