rivers Flashcards

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1
Q

drainage basin

A

an area drained by a river and its tributaries.

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2
Q

Lateral erosion

A

sideways erosion

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3
Q

Evaporation

A

water heated turning from a liquid to a gas (water vapour)

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4
Q

Erosion

A

the wearing away of the land

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5
Q

abrasion

A

material carried by the river smashes against the banks wearing them away

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6
Q

attrition

A

rocks smashing into each other gradually become smaller and rounder

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7
Q

hydraulic action

A

the force of the water and/or forces air into cracks making them wider

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8
Q

solution

A

where water has a chemical reaction with the rock and dissolves it

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9
Q

suspension

A

lighter material is carried in the river.

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10
Q

solution

A

dissolved material transported

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11
Q

saltation

A

heavier material is bounced along the bed of the river.

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12
Q

traction

A

the heaviest material is rolled along the bed of the river.

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13
Q

deposition

A

when material is dropped by the river

take place where the velocity of the river slows down for example on the inside of a meander, at the mouth where the river meets the sea, or on the floodplain when it overflows.

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14
Q

name the 3 processes

A

erosion, transportation and deposition

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15
Q

name the 5 landforms

A

v-shaped valleys, waterfalls, meanders, oxbow lakes, floodplain

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16
Q

how does the river change from upper to lower course

A

River becomes wider
Discharge increases
Velocity increases
Gradient decreases

17
Q

why does a river change from upper to lower course

A

River becomes wider - as a river reaches its lower course lateral erosion becomes more common, as gradient decreases, widening the river.
Discharge increases - as more tributaries join the river amount of water increases.
Velocity increases - as bedload has become smaller and banks and bed smoother friction decreases therefore increasing velocity.
Gradient decreases - due to meander migration widening the valley floor

18
Q

Interlocking spurs

A

The river at its source is small and has limited energy. It flows naturally from side to side around ridges of more resistant rock creating spurs.

19
Q

v-shaped valley

A

vertical erosion takes place deepening the channel whilst weathering attacks the slopes, weakening the rock until mass movement moves the material downslope.

20
Q

waterfall process

A

Hard, more resistant rock overlays softer less resistant rock. Soft rock is eroded more rapidly through hydraulic action/corrasion undercutting the hard rock creating an overhang. The force of the water creates a plunge pool. The hard rock collapses under its own weight and the process repeats, retreating upstream to create a gorge.

21
Q

process of meanders/oxbow lakes

A

Water flows fastest on the outside of a meander eroding the banks, creating a river cliff. On the inside of the bend where the river is flowing slower deposition takes place creating a slip-off slope. As erosion continues at the neck of the meander it becomes narrower. Normally in flood conditions the force of the water breaks through creating a new channel. The old part of the river is cut off as deposition now takes place along the banks of the river, creating an oxbow lake.

22
Q

flood plain

A

the floodplain is a wide flat area of land either side of the river. In its lower course meander migration takes place. This occurs due to lateral erosion eroding the outside of the bend and deposition on the inside moving the meander across the valley floor, widening and flattening it.

23
Q

what were the physical causes of the Boscastle flood

A

Intense rainfall, 185mm in 5 hours, did not allow time for water to infiltrate therefore overland flow increased.
Large amount of rainfall earlier in the week and an input of 3 million tonnes of water meant ground was saturated and could hold no more water.
Confluence of 3 rivers, Valency, Jordan and Paradise drained a small drainage basin of just 40Km2.
Geology - impermeable sandstone did not allow water to infiltrate and therefore overland flow increased.
Steep valley sides reduced infiltration and thin soils couldn’t hold much water

24
Q

what were the human causes of the boscastle flood

A

Narrow bridges became blocked with trees diverting water into the streets.
Deforestation results in fewer trees to intercept and store water . Therefore more water gets to the river channel.
Urbanisation results in water flowing rapidly into drains over impermeable surfaces. The water gets to the river channel too quickly.

25
Q

when was the boscastle flood

A

august 2004

26
Q

what was the result of the boscastle flood

A

Water rushed down streets at 40mph as a 10ft wall of water ripping up roads and destroying both bridges
80 cars in the car park were swept away in minutes.
6 properties were destroyed outright. Most others needed £15,000-£30,000 repairs
Loss of trading amounted to £15m
Bed of the river Jordan was 10 feet higher
Most houses had 2 feet deposit of mud
Most shops stayed shut for rest of the season
Trade in tourism reduced.
Value of homes permanently reduced - some by half.

27
Q

how was flooding prevented on the river severn in shrewsbury

A

Demountable barrier system – 1.5m to 3m tall, offers protection from 1 in 100 year flood
Adding two new pumping stations to reduce water backing up in drains.£3.5 million scheme - 1 in a 100 year chance
Flood embankments, located in a conservation area, so made sure they blended into the surrounding area. £2.4 million scheme, reduce the level of flood risk to a 1 in 100
Clywedog dam and reservoir, in the upper course of the Severn. Gives some protection immediately downstream but little benefit to Shrewsbury
Natural flood meadows (washlands) exist upstream of Shrewsbury and provide some protection
Levees constructed to provide protection for low lying agricultural land. Reduce risk of flooding to 1 in 10 or 20 chance in a year

28
Q

advantages of hard engineering

A

Very effective
Strong and durable

29
Q

disadvantages of hard engineering

A

Expensive
Visually unattractive

30
Q

advantages of soft engineering

A

Relatively cheap
Blends in with the natural environment

31
Q

disadvantages of soft engineering

A

May not be as long lasting or as strong
Can lead to conflict e.g. allowing certain places to flood

32
Q

land use zoning

A

areas in a city are set aside for certain functions to reduce the impact of flooding

33
Q

examples of land use zoning

A

Areas close to a river are set aside for sports and recreational activities.

Hospitals occupy higher land away from the risk e.g. JR

Residential areas tend to be on higher ground than industries due to the risk of life.

34
Q

what is the regime

A

the pattern of a river’s flow over a period of time, usually a year.

35
Q

what factors is the regime dependent on

A

First is the amount of precipitation during the year, more in the winter will lead to an increase in flow during that time.
Geology will impact, with impermeable leading to fluctuating regime.
Forest - loss of leaves in the winter will lead to more water reaching the river

36
Q

conflicting views in shrewsbury

A

Over spoiling the historical beauty of the town
How useful actual flood protection will be
The impact on the environment versus keeping people safe
Justification of the cost of the protection
The disturbance caused to locals whilst construction takes place
Places being allowed to flood e.g. farmers fields
Impact on places further downstream

37
Q

Thames Estuary

A

Conflicting views over how long the Thames Barrier will be useful for - hard to predict future changes and how they might impact.
Flood walls being used are protecting properties but others feel they funnel the water towards London
Managed realignment - landowners do not want farmland flooded but does soak up pollutants and provides a habitat,as well as protecting places further upstream
Building houses in the Thames Gateway - prime building land but increasing the risk of flooding