4.6, 4.7, 4.8 Flashcards

1
Q

Long profile of a river

A

The path of a river, and how it has elapsed from start to end. Twisting, bending, meandering, eroding downward, depositing sediment causing higher floor etc.

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2
Q

Hydraulic action vs abrasion

A

Hydraulic action is when high pressure water jets are pushed into cracks and faults, causing pressure on the rock making the fault larger.

Abrasion uses scraping of sediment, to erode rock instead of water under high pressure.

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3
Q

Weathering

A

The process occuring when different weather types of weather are present in a landscape, causing specific visual and physical effects on the landscape.

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4
Q

Freeze thaw vs biological

A

Freeze thaw is when water fills faults or cracks, freezes and increases the width of the fualt or crack.
Biological weathering is when plants seed in areas prone to erosion, the grow and cause cracks and instability, falling of rock and erosion.

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5
Q

Traction vs suspension.

A

Traction is sediment being carried along the river bed, rolling along the direction of the flow. Usually larger sediment.
Suspension is when the sediment bounces off the river bed, suspended in the flow of water being carried along, usually smaller pieces of sediment.

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6
Q

Waterfalls

A

A area of soft rock in the river bed is eroded, because of erosion of traction, a area of deeper river bed arises and the water falls of the lip created, eventually the plunge pool below will become deeper because of the sediment and rocks falling into it, deepening it, causing a steeper water fall. As the waterfall lip erodes, it will eventually fall and cause retreating in the waterfall, giving the effect of a cut waterfall back in the landscape.

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7
Q

V shaped valley

A

Begins with a river flowing through a landscape, which erodes deeper into the landscape, the raised embankments of the river become loose due to weathering and collapse, the fallen sediment is taken away don the river and a v shape is left behind to the valley.

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8
Q

Lag time

A

Time between maximum rainfall and peak discharge of river. Time for people to evacuate the areas in risk from warning

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9
Q

Physical factors affecting hydrographs

A

Steepness of drainage basin, permeability of soil, surrounding landscapes, speeding up or slowing down lag time.

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10
Q

Deforestation and urbanisation affecting flood hydrographs.

A

Land characteristics change, permeability of concrete is low, primarily used in urbanised areas, faster run off time, less lag time. Trees slow surface run off, deforestation means less obstacles obstructing the surface run off, meaning faster run off and faster lag time.

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11
Q

How can humans affect flooding, how did it in the river Eden case?

A

Physical- heavy rainfall, causing floodwater in large ammounts,

Human
-poor drainage systems and sewers couldn’t cope and caused worsened flooding in urbanised areas.

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12
Q

Flooding probems

A

-death
-loss of property
-loss of business
-worsened economy
-tourism lost
-natural attractions, (attractions) lost
All link together

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13
Q

Why is river flood increasing?

A

Climate change means global climate is heating up, this is because of a few different factors such as greenhouse gasses which trap heat, amplifying it, consequently, ice is melting, making sea levels rise and a lower tolerance of most rivers, due to higher water levels and more risk of flooding.

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14
Q

Hard vs soft engineering

A

Hard- using non natural materials in to stop natural pricesses.
Soft- using natural material and usually less visually destructive to landscapes, enhancing natural processes.

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15
Q

Levees

A

Look bad
Can be expensive

Stop over flowing rivers
In cases where they aren’t tall enough, they will cause worse more sudden, severe flooding

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16
Q

Dredging

A

Need to be re dredged anually-expensive

Natural and not easy to see
Fairly inexpensive to do the process.

17
Q

Using wood and natural things to slow river flow

A

Inexpensive,
Effective
Slows river flow, decreasing flooding chances
Natural

18
Q

The landscapes change through the flow of river Eden

A

The higher section of the river is steeper, in the middle course it evens out and increases velocity, in the lower course, the river branches out and increases velocity, due to less obstructions.

19
Q

Reasons for changes to the landscape

A

Valley sides affected by river flow
Rounder rocks are found in the upper course as they have had less erosion whereas in the middle and lower course the sediment is smaller as it has been more finely eroded.

20
Q

Upper course

A

The source of the Eden is about is about 600m abouve sea level. In an area of hard, resistant rock.

21
Q

River erosion

A

Can be vertical and lateral, takes easiest path of erosion, softest rock and forms shape of river.

22
Q

Confluence

A

Confluence - the point at which two rivers or streams join. Tributary - a stream or smaller river which joins a larger stream or river.

23
Q

Ox bow lake

A

Tight meander has a neck of soft rock, high velocity of water on the outside of the river causes it to erode through, leaving a cut out area of water, where the meander outside used to be and leaves a pool of water that becomes stagnant, sediment is deposited here and cuts it off from the flow of the main river altogether and it is isolated as a ox bow lake.

24
Q

Meander

A

A bend in the flow of a river, where the flow of water is at optimum velocity in the outside of the bend

25
Q

Interlocking spurs

A

Glaciers in a period of ice age, melt away soft rock from a mountainous area which alternated through the now valley, soft and hard rock. The soft rock was taken away by freeze thaw, leaving interlocking hard rock strips either side, the river follows this pattern and these bends created when it follows the interlocking pattern, are not called meanders.

26
Q

Saltation

A

Sediment dissolved in the water and carried as molecules suspended near the surface of the water.