River Landscapes and Processes Flashcards

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1
Q

what is a water shed

A

boundary of a drainage basin separates one drainage basin from another and is usually high land, such as hill s and ridges

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2
Q

what is a tributary

A

a stream or small river that joins a larger stream or river

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3
Q

what is a source

A

the starting point of a stream or river, often a spring or a lake

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4
Q

what is a confluence

A

a point where two streams or rivers meet

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5
Q

what is a mouth

A

the point where a river leaves its drainage basin and flows into sea

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6
Q

types of weathering

A

mechanical
chemical
biological

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7
Q

mass movement that affects river valleys

A

soil creep
sliding
flows

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8
Q

erosion processes that effect river valleys

A

hydraulic action
abrasion
solution
attrition

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9
Q

what is hydraulic action

A

sheer force of water hitting the river bed and banks and wearing them away

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10
Q

what is abrasion

A

material carried in river rubbing against bed and banks of the channel and wearing them away

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11
Q

when does deposition occur

A

when a river no longer has enough energy to carry its load

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12
Q

what happens as rivers discharge and velocity reduce

A

heaviest material is deposited first

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13
Q

4 types of transportation

A

traction
saltation
suspension
solution

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14
Q

what does size of waves depend on

A

fetch - distance over sea the wave has travelled over
how long wave travelled for
strength of wind
time of wind blowing

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15
Q

physical causes of flooding

A

intense rainfall
duration of rainfall
snow melt
relief

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16
Q

human causes of flooding

A

deforestation
urbanisation

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17
Q

why flood risk is going to increase

A

change in land use
increasing population
changes to weather patterns from climate change

18
Q

what does a hydrography show

A

how a river responds to a storm event

19
Q

what are the key features of a hydrograph

A

rising limb
lag time
falling limb

20
Q

what is rising limb in a hydrograph

A

rapid rise in water after a period of heavy rainfall

21
Q

what is lag time in a hydrograph

A

difference between time of heaviest rainfall and point at which the river contains the largest amount of water

22
Q

what is falling limb in a hydrograph

A

reduction in amount of rainfall reaching the channel

23
Q

what does environmental agency do

A

building flood defences

helping people prepare for flooding and giving flood warnings

24
Q

hard engineering techniques

A

levees
dams and reserovirs
flood relief channels
channelisation

25
Q

disadvantages of levees

A

burst under pressure causing more damage

26
Q

advantage of levees

A

stop water from spreading into areas where it could cause problems

27
Q

advantages of channelisation

A

allows more water to run through the channel more quickly, taking it away form places at risk

28
Q

disadvantage of channelisation

A

may put other places at risk
does not look natural

29
Q

advantages of flood relief channels

A

accommodate high flows so that a river wont over flow its banks

30
Q

disadvantages of flood relief channels

A

high costs
unsightly

31
Q

soft engineering techniques

A

washlands
river restoration
flood plain zoning

32
Q

advantages of washlands

A

safe place for floodwater to go
help slow flood water down

33
Q

disadvantages of washlands

A

allowing land to flood may limit the use of the land fo recreation

34
Q

advantages of river restoration

A

more attractive and create natural habitats

35
Q

advantages of flood plain zoning

A

prevents building homes and businesses in high risk zones

36
Q

how land is used to decrease flooding

A

afforestation
managing drainage
managing farmland

37
Q

formation of waterfalls and gorges

A

waterfall is formed along a river when a band of hard, more resistant rock lies over a band of soft, less resistant rock

  1. river erodes the less resistant rock at a faster rate, gradually undercutting the more resistant rock. The continued erosion of the soft rock by abrasion and hydraulic action causes an overhang of hard rock
  2. eventually hard rock cant support its own weight and collapses under force of gravity. Force of falling water and abrasion by boulders leads to erosion of river bed and the formation of a plunge pool
  3. as soft rock continues to be eroded and the hard rock collapses, a steep sided gorge is formed as the waterfall retreats upstream
  4. gorges form in hard rocks where vertical erosion by rivers is dominant
38
Q

formation of interlocking spurs

A

in upper course, discharge is low. River uses most of its energy overcoming friction with the channel. What energy it has left over is used by hydraulic action to deepen the channel by vertical erosion

resistant rock is in the upper course. Freeze thaw weathering gradually widens the river channel, giving the valley a steep v shaped cross profile. Over time this weakens rock which breaks loose and shifts down valley sides. This is then transported by river more downstream

winding path taken by the river is due to obstacles of hard rock in its path. The river takes the easiest route over land. This results in interlocking spurs

39
Q

formation of flood plains and levees

A

floodplains and levees can be found in lower course. Floodplains are flat, wide areas of land either side of the river

river transports sediment downstream. When river floods it transports sediment over floodplain. When flood occurs river loses energy depositing largest sediment almost immediately in sides of river banks. Whereas small sediment is carried further onto the floodplain

if flooding continuously occurs, the deposited sediment increases raising height of levees and flood plains

this also increases river channel, which can then cope with a higher discharge and flooding is less likely to occur in the future

40
Q

meanders and oxbow lakes

A

a meander is a slight bend in river. As water flows through meander it travels faster on outside bend creating erosion . This undercuts riverbank forming river cliff. Whereas water travels slower on inside bend causing deposition to create slip off slope

as bend becomes more extreme, the rivers current will begin to erode the neck of the meander know as lateral erosion

the meander neck continues to be eroded becoming smaller and narrower over time

continued erosion causes river to cut through the neck of meander completely making a shortcut for river current. Material will then be deposited t the side of the river bank where former river channel travels through

now the channel becomes more established, due to deposition so previous channel begins to dry up

over time the former meander becomes completely separated from the river channel and no longer receives river water

marsh plants colonise the area which widens the gap further. This is know as an oxbow lake

41
Q

what to do in the event of a flood

A

gather essentials together upstairs
fill jugs and saucepans with clean water
move family and pets upstairs
turn off gas, electricity and water supplies
keep listening to local radio
avoid walking through and touching the water