Coastal systems and landscapes Flashcards

1
Q

Define what is meant by a coast.

A

A coast is an open system with both inputs and outputs which cross the boundary of the system to the surrounding environment.

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2
Q

Give me examples of inputs.

A

Inputs:

1) energy in the form of wind, waves, tides and currents
2) stores/components
3) transfers/flows
4) sediment
5) geology of the coastline
6) sea level change

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3
Q

Give me examples of outputs.

A

Outputs:

1) energy
2) matter

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4
Q

Describe how coasts adjust to imbalances in the system.

A

Coasts are dynamic places (always changing) therefore the system is in a state of dynamic equilibrium with a balance between inputs and outputs. Change occurs due to an upset in the system e.g. storms/human activity, and a way to adjust is through the process of feedback.

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5
Q

Describe what feedback is.

A

The way in which a coast adjusts to an imbalance in the system.

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6
Q

What does positive feedback achieve?

A

Positive feedback ensures progressively greater change from the original condition of the system.

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7
Q

What does negative feedback achieve?

A

Negative feedback ensures the system returns to its original condition.

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8
Q

Define what is meant by waves.

A

Waves are undulations on the surface of the sea driven by the wind.

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9
Q

What are the key features of waves?

A

1) Height- the difference between the trough and crest
2) Length- the distance between crests
3) Frequency- the time lapse between crests

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10
Q

What are the functions of a wave?

A
A wave enters shallow water 
Friction with the seabed increases
The wave slows
Increases in height
And plunges or breaks onto the shoreline
The wash of water up the beach is a swash and the drag down the beach
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11
Q

What are the different types of waves?

A

1) Constructive: low, long length, low frequency, strong swash, weak backwash –> form berms
2) Destructive: high, steep, high frequency, weak swash, strong backwash –> form storm beaches

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12
Q

What is meant by wave refraction?

A

When waves break onto an irregularly shaped coastline e.g a headland separated by two bays.

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13
Q

Explain the process of wave refraction.

A

Waves drag in shallow water approaching a headland
The wave becomes high, steep and short
The part of the wave in the deeper water moves forward faster
The wave bends
The low energy waves spill into the bays as most of the wave energy is concentrated on the headland

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14
Q

What are currents?

A

The permanent or seasonal movement of water in seas and oceans

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15
Q

What are the different types of currents?

A

1) Longshore current- most waves approach the shoreline at an angle. This creates a current of water running parallel to the coastline.
2) Rip currents- these are strong currents moving away from the shoreline due to a build up of seawater and energy along the coastline.
3) Upwelling- the global pattern of currents circulating in the oceans can cause deep, cold water to move towards the surface, displacing the warmer surface water.

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16
Q

Define what is meant by tides?

A

Changes in the water level of seas and oceans.

17
Q

What are tides caused by?

A

The gravitational pull of the moon, the sun and the rotation of the earth.

18
Q

What are the different types of tides?

A

1) Neap tides:
Moon at right angles to the Sun when in first quarter or last quarter
Gravitational pulls act against each other to create lower high tides and higher low tides
Diminishes the gravitational pull of the moon
2) Spring tides:
Moon at right angles to the Sun when in first quarter or last quarter
Gravitational pulls act against each other to create lower high tides and higher low tides
Centrifugal force counterbalances the gravitational pull

19
Q

What are the characteristics of a high energy coast?

A

Powerful waves
High waves
Strong prevailing winds
Long length of fetch
Rate of erosion exceeds rate of deposition
Landforms: wave cut platform, headland, cliffs

20
Q

What are the characteristics of a low energy coast?

A

Low energy waves
Waves are spread out, energy is dissipated
Low waves
Rate of deposition exceeds rate of erosion
Low tidal range
Landforms: beaches, spits, coastal plains

21
Q

What are the sediment sources?

A

1) Seabed- rising sea levels–>sediment from continental shelf areas swept towards the shoreline
2) Rivers e.g. bedload shingle & suspended silt & clay
3) Cliff erosion
4) Biological origin e.g. shells & corals
5) Longshore drift

22
Q

What is meant by a sediment budget?

A

The balance between sediment being added to and removed from the coastal system
If more material is being added than removed= positive budget (accretion of material)–> shoreline builds to the sea
More material removed than added=negative budget–> shoreline recedes landward

23
Q

Describe the sediment budget in more depth.

A

11 sediment budgets along the coastline in England and Wales
Considered as a closed system
Inputs come from erosion from the sea bed or land
Erosion, transportation and deposition within the cell
Headlands or change in LSD are the boundaries