Rivers Flashcards

1
Q

types of erosion

A

abrasion
hydraulic action
attrition
solution

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2
Q

hydraulic action

A

the sheer power of the waves as they smash against the cliff. air becomes trapped in the cracks in the rock and causes the rock to break apart from the pressure.

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3
Q

attrition

A

rocks in the water knock against each other. they break apart to become smaller and rounder

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4
Q

abrasion

A

pebbles grind along a rock platform, like sandpaper. over time, the rock becomes smooth

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5
Q

solution (erosion)

A

sea water dissolves certain types of rocks and breaks down some rock. in the UK, chalk and limestone cliffs are prone to this.

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6
Q

types of transportation

A

traction
saltation
solution
suspension

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7
Q

traction

A

where pebbles and larger material are rolled along the seabed

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8
Q

saltation

A

where small pieces of shingle or large sand grains are bounced along the sea bed

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9
Q

suspension

A

small particles such as silts and clays are suspended in the flow of the water

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10
Q

solution (transportation)

A

when materials in rocks like chalk and limestone are dissolved in sea water and then carried in solution. the load is not visible

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11
Q

characteristics of the upper course

A

steep gradient
V-shaped valley, steep sides.
Narrow, shallow channel
Bedload is large and angular
Lots of vertical erosion
low velocity
small discharge

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12
Q

characteristics of the middle course

A

medium gradient
Gently sloping valley sides. Wider, deeper
channel
Load becomes smaller and less angular.
Lateral erosion increases

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13
Q

characteristics of the lower course

A

gentle gradient
Very wide, almost flat valley, very wide, deep
channel
Large amount of load but the size is small and
very rounded. A lot of lateral erosion occurs
high velocity
large discharge

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14
Q

formation of meanders

A
  1. In the middle course, the river has more energy and the land is flatter. This causes the river to meander and more lateral
    erosion occurs. There is a disturbance making a hole in one bank. Water flows into it and erodes it, beginning a bend.
  2. Water flows faster on the outside bend, eroding it creating a river cliff.
  3. Material is deposited in the slow moving water on the inside bend creating a slip-off slope
  4. over time the amplitude of the bend increases making the meander more pronounced
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15
Q

formation of oxbow lakes

A
  1. Oxbow lakes begin with a meander.
    2 . The water on the inside of the bend is moving slowly and has less energy, so material is deposited here.
  2. Water flows faster on the outside bends eroding them so that they get closer together.
  3. Gradually over time, two outside bends can erode so much that the meander neck narrows until they touch and during a time of flood, the water can break through the land between them. The river takes the straighter, faster route so less water flows around the bend
  4. Material is deposited in the slow moving water in the old bend, cutting if off and creating an ox-bow lake.
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16
Q

formation of a v-shaped valley

A
  1. Water collects on high ground after heavy rain and begins to flow downhill because of gravity. Gradually, the river erodes the underlying rock creating a channel.
  2. The sides of the channel are exposed to the weather. Weathering breaks up the rocks on the valley sides.
  3. The weathered rock on the valley sides falls into the river channel (mass movement). some is carried away by the river
  4. the process repeats, and the v-shaped valley becomes deeper.
17
Q

features of the upper course

A

waterfalls
v-shaped valleys
inter-locking spurs

18
Q

features of the middle course

19
Q

features of the lower course

A

meanders
ox-bow lakes
floodplains
levees

20
Q

physical causes of river flooding

A

antecedent rainfall
impermeable rock
relief
weather conditions

21
Q

human causes of river flooding

A

urbanisation
agriculture
deforestation
climate change

22
Q

causes of river flooding: urbanisation

A

surfaces like roads are impermeable&raquo_space; more surface run-off&raquo_space; water returns to the river faster increasing the risk of flooding. rainwater also flows into drains which returns water to the river faster

23
Q

causes of river flooding: agriculture

A

irrigation up and down (instead of across) hillsides creates channels&raquo_space; allows water to reach rivers faster&raquo_space; increasing discharge

24
Q

causes of river flooding: deforestation

A

less interception&raquo_space; rain reaches the ground faster&raquo_space; ground is more likely to become saturated&raquo_space; more surface run-off&raquo_space; water returns to the river faster increasing discharge

25
causes of river flooding: climate change
warmer air can hold more water >> more frequent intense storms >> increasing discharge
26
causes of river flooding: antecedent rainfall
soil is saturated >> more surface run-off >> water returns to the river faster increasing discharge
27
causes of river flooding: impermeable rock
no infiltration >> more surface run-off >> water returns to the river faster increasing discharge
28
causes of river flooding: relief
steep slopes increase surface run-off >> water returns to the river faster increasing discharge
29
causes of river flooding: weather conditions
hot, dry soils can bake the soil making it impermeable >> more surface run-off >> water returns to the river faster increasing discharge
30
how does urbanisation affect river processes and landscapes
- Urbanisation has caused towns to grow, meaning there are fewer permeable surfaces. Water flows into the rivers, increasing discharge. - Increasing demand for housing has led to new houses being built on floodplains. This changes the natural landscape. - Rivers may be channelised or made to flow underground to make room for urban developments. If this happens, erosion and deposition cannot take place.
31
how does agriculture affect river processes and landscapes
- Field drains can improve farmland, but quickly move water into streams and rivers, and can destroy natural wetland landscapes. - Forests can be felled to make way for farmland. Trees intercept rainfall, helping to reduce surface run-off. Removing trees means water reaches rivers more quickly. - Abstracting water for irrigation reduces the flow and velocity of a river so deposition occurs rather than erosion. - ploughing fields up and down a slope can increase the amount of sediment in rivers and increase deposition.
32
how does industry affect river processes and landscapes
- Industry is a big user of water, so can reduce the amount of water in rivers, leading to less erosion. - Industrial processes can pollute rivers if chemicals or waste are spilled or dumped into them. This can destroy plants and animals and change the natural landscape.