Physical Factors - P Flashcards

1
Q

What are the 5 physical factors affecting coastal landscapes

A
  • winds
  • waves
  • tides
  • geology
  • currents
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2
Q

How do we know which factors are most important

A

It depends on specific location, spatial scale and temporal scales

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3
Q

What does Aeolian mean

A
  • relating to or arising from the action of the wind e.g. erosion, transportation and deposition of sand by wind.
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4
Q

What do Aeolian processes require

A

require wind energy to operate

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5
Q

What 4 processes can wind affect

A
  • form waves
  • erode landforms
  • transport and deposition materials
  • create and modify landforms
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6
Q

What process is where wind picks up sand

A

deflation

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7
Q

What is suspension

A

the transportation of the smallest grains of sand (in the air)

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8
Q

What is saltation

A

The transportation of medium grains of sand by bouncing along the ground

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9
Q

What is surface creep

A

the transportation of the largest grains of sand by rolling them across the ground

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10
Q

What is attrition

A

the breaking down of particles (occurs as sand particles collide during transport

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11
Q

What is the dominant wind

A

a wind perpendicular to the coast - usually storm winds (90 degrees)

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12
Q

What’s is the prevailing wind

A

The most common direction of wind in a location

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13
Q

What is an onshore wind

A

wind blowing from the sea to the land

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14
Q

What is an offshores wind

A

wind blowing from the land to the sea

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15
Q

What is the source of energy for coastal erosion and sediment transport

A

wave action

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16
Q

How is wave energy generated

A

By the frictional drag of winds moving across the ocean surface.

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17
Q

what factors of wind gives the waves more energy

A
  • higher wind speed
  • longer fetch
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18
Q

What type of winds drive waves to the coast

A

onshore winds

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19
Q

What happens when wind blows at an oblique angle (an angle other than 90 degrees)

A

the resultant waves generate longshore drift

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20
Q

How are waves formed

A

by the frictional drag of winds moving across the ocean surface

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21
Q

What is wave frequency

A

the time between waves - usually measured in seconds

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22
Q

which 3 factors combine to generate waves

A
  • strength of wind
  • length of time wind blows
  • distance over which the wind has been blowing (fetch)
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23
Q

What is the strength of wind measured in

A

metres per kilometres per hour

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24
Q

what is length of time wind blows measured in

A

hours

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25
Q

What is the distance over which the wind has been blowing measured in

A

km (also known as the fetch)

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26
Q

Does a shorter or longer fetch create a more powerful wave

A

a longer fetch

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27
Q

What is shallow water

A

water that is the depth of half of a wavelength

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28
Q

What occurs in shallow water

A
  • at this depth the deepest circling molecules make contact with the seafloor: friction slows speed of wave
  • wavelength decreases as wave steepens
  • top of the wave travels faster and topples over
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29
Q

What is swash

A

waves moving up the beach

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30
Q

What is backwash

A

waves moving down the beach

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31
Q

What are some main features of constructive waves

A
  • low in height
  • long wavelength
  • low frequency (6-8 per minute)
  • break by spilling forwards
  • strong swash
  • weak backwash
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32
Q

Describe how a constructive wave swashes and backwashes

A
  • strong swash which travels a long way up the gently sloping beach.
  • backwash returns to sea before r next wave breaks, due to long wavelength, so the next swash is uninterrupted so maintains its energy
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33
Q

In a constructive wave does swash exceed backwash energy

A

yes

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34
Q

What happens to offshore bars when waves are constructive

A

the material is moved onshore

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35
Q

As constructive waves have strong swash what happens to beach material

A

It transports sand up the beach to form a bear,

36
Q

As constructive waves have a weak backwash what happens to beach material

A

There is lots of percolation through the sand and little transport of sand down the beach

37
Q

What are some main features of destructive waves

A
  • greater height
  • shorter wavelength
  • higher frequency12-14 per minute)
  • break by plunging downwards
  • weak swash
  • strong backwash
38
Q

Describe how a destructive waves generate swashes and backwashes

A
  • friction from the steep beach slows the swash, so quickly returns as backwash
  • the next wave is often slowed by the frictional effect of meeting the backwash of the previous wave
38
Q

in a destructive wave is the swash energy less than the backwash energy

39
Q

what happens to longshore bars when there are destructive waves

A

the eroded material is deposited offshore in longshore bars

40
Q

what forms when there are destructive waves

41
Q

What happens due to a strong backwash

A

there is little percolation so more material is moved down the beach

42
Q

When does wave refraction occur

A

when a coastline isn’t straight so the process of waves breaking all at the same time is interfered with

43
Q

What happens to waves in front of headlands

A

they slow down due to shallower sea - this means the wave is moving at different speeds so wave refraction occurs

44
Q

Where do waves converge during wave refraction

A

the headland

45
Q

Where do waves diverge during wave refraction

46
Q

Describe wave refraction

A
  • as waves travel from deep to shallow water, the wavelength shortens, the wave speed slows down, and the wave will refract towards the shallow areas to conserve its energy
47
Q

What is the energy like where waves converge

A

the energy is concentrated

48
Q

what is the energy like where waves diverge

A

the energy is reduced

49
Q

How are tides formed

A

they are formed by gravitational energy

50
Q

What do tides control

A

where wave action takes place and where weathering can take place when shorelines are exposed at low tide

51
Q

What is a tidal range

A

the difference between the high and low tide - it can influence the development of coastal landscapes

52
Q

What tidal ranges do enclosed seas have e.g. the Mediterranean

A

minimal tidal ranges - making wave action and weathering opportunities on exposed shoreline limited and over a very small area

53
Q

What are the three types of tidal ranges

A
  • Micro tidal - ranges < 2m open ocean coasts (wave dominated)
  • Meso tidal - 2-4m (a combination)
  • Macro tidal >4m (tide dominated)
54
Q

What is a spring tide

A

when the sun and moon align (with earth), the combined effect is to produce a higher than normal tide

55
Q

What is a neap tide

A

when the sun and moon are at right angles to each other so lower than normal tides occur

56
Q

Why are neap tides lower than normal

A

because the sun and the moon have gravitational pulls in different directions

57
Q

What produces tidal currents

A

when the water rises and falls

58
Q

What is a rising tide called

A

a flood tide

59
Q

What is a falling tide called

A

an ebb tide

60
Q

What are the two aspects of geology that can influence coastal landscapes

A
  • litholgy - type of rock in that location e.g. resistant rock
  • structure - the way the rocks are geologically arranged e.g. joints and bedding planes
61
Q

Why are Igneous and metamorphic rocks are harder

A

because of heating and compression during their formation

62
Q

Where are most igneous and metamorphic rocks found in the UK

A

North West Britain - forming high cliffs which are more resistant to erosion

63
Q

Where are the soft rocks found in the UK

A

on the coastline of Southern and Eastern Britain

64
Q

What are soft rocks a usually made out of

A

unconsolidated sands and clays as well as glacial boulder clays and gravels.

65
Q

Why are soft rocks more easily eroded

A

they have weaker rocks, with poorly protected bases (3-6m per year)

66
Q

What can structurally make a rock weaker

A

Where there is a high concentration of joints and bedding planes

67
Q

What is a bedding plane

A

a horizontal boundary between layers of rock

68
Q

What is a joint

A

A natural fracture (usually vertical) within the rock

69
Q

What is strata

A

Layers of rock

70
Q

What do more joint and bedding planes means can happen with water

A

the water can easily pass through as limestone is permeable

71
Q

The type of rock can determine the landscape that is formed what are the types of rock

A
  • concordant coastline
  • disconcordant coastline
72
Q

What is a concordant coastline

A

They occur when rock types are parallel to the shore - usually only one rock type

73
Q

What is a disconcordant coastline

A

occur when rock types is perpendicular to the shore - usually more rock types

74
Q

What type of coastline forms headlands and bays

A

a disconcordant coastline

75
Q

Why do ocean currents occur

A

due to the earths rotation

76
Q

What do ocean currents do

A

redistribute heat from low latitudes (tropics) to high latitudes (polar regions)

77
Q

What is an example of an ocean current

A

the Gulf Stream
The North Atlantic drift

78
Q

What do ocean currents influence which can influence coastal landscapes

A

they influence the processes dependant on temperature

79
Q

What processes do ocean currents influence

A

Freeze thaw weathering, exfoliation and biological weathering (influenced by temperature)

80
Q

What type of currents are more localised than global currents

A

rip currents - influence the movement of sediment on a local scale

81
Q

how does a rip current work

A

there is a rip feeder which moves the water past the breaker zone past this point it forms a rip head (similar to a cusp) where fine material can be deposited

82
Q

What helps to form cusps

A

a cellular circulation

83
Q

Where are cusps formed

A

on beaches in bays

84
Q

What does erosion between cusps lead to

A

A deepened seabed which helps to continue the cellular circulation