River processes and pressure Flashcards

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1
Q

Hydraulic action

A

The force of the water on the bed and banks of the river removes material

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2
Q

Attrition

A

The load that is carried by the river bumps together and wears down into smaller, smoother pieces

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3
Q

Abrasion

A

Material carried by the river rubs against the bed and banks and wears them away

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4
Q

Solution

A

Some rock minerals dissolve in river water (e.g. calcium carbonate in limestone)

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5
Q

Traction

A

Large boulders roll along the river bed

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6
Q

Saltation

A

Smaller pebbles are bounced along the river bed, picked up and then dropped as the flow of the river changes

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7
Q

Suspension

A

Finer sand and silt particles are carried along in the flow, giving the river a brown appearance

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8
Q

Solution

A

Minerals from rocks such as limestone and chalk, are dissolved in the water and carried along in the flow, although they cannot be seen

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9
Q

Deposition

A

When the river loses energy (slows down) it may drop some of its load

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10
Q

How are waterfalls formed (upper course feature)?

A

1- Band of more resistant rock lies over less resistant rocks
2- Less resistant rock is eroded more quickly, leaving a ‘step’ - the waterfall
3- More resistant rock is undercut, forming an overhang
4- Overhang can no longer be supported, blocks of rock fall down
5- Powerful fall of water erodes plunge pool using fallen rocks
6- Waterfall retreats upstream

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11
Q

How are interlocking spurs formed (upper course feature)?

A
  • The river at its source is small and has limited energy. - It flows naturally from side to side, around ridges in the valley sides, called spurs
  • The spurs become interlocking with those on the other side of the valley
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12
Q

How are meanders formed (lower course feature)?

A
  • they are bends in the river’s course
  • in the lower course, the river uses up surplus energy by swinging one way to the other, causing lateral erosion on the outside of bends and deposition on the inside
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13
Q

How are do bow lakes formed (lower course feature)?

A
  • forms when a river creates a meander, due to the river’s eroding bank
  • after a long period of time, the meander becomes very curved, and eventually the neck of the meander becomes narrower
  • the river cuts through the neck during a flood, cutting off the meander and forming an oxbow lake
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14
Q

Explain how erosion and deposition form floodplains (lower course feature) (4)?

A
  • as a river meanders in its lower course, lateral erosion erodes away the valley sides, making the valley flatter
  • the meanders migrate downstream
  • at the same time, deposition occurs as every time the river floods, fine particles of silt are deposited onto the valley sides, forming the floodplain over thousands of years
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15
Q

How are levées formed (lower course feature)?

A
  • as the river floods over its bank, the water slows down
  • the water can’t carry the biggest + heaviest silt particles and thyme are dropped straight away on the bank forming flood plains
  • increased deposition on the river bed when the river is low gradually raises the river bed upwards
  • after many floods, the deposits on the bank build up, forming levées
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16
Q

How are deltas formed (lower course feature)?

A
  • the speed of a river decreases as it approaches the sea and it deposits most of the material it has been carrying
  • over time sediment builds up to create an almost flat area of new land, which is the delta
  • as the river is now flowing very slowly over the almost flat gradient, it’s channel fills up with sediment and the river splits and spreads out into many different streams
17
Q

How does the erosion rate impact the river landscapes and sediment load?

A
  • the erosion rate is greater where discharge and energy of river are greater
  • so rivers in wet climates erode more material than those in dry climates, impacting on the shape of the river valley and amount of sediment
18
Q

Discharge of river

A

Volume of water flowing through river channel in a given time