Coasts Flashcards

(26 cards)

1
Q

Backshore definition

A

Is the area between the high water mark and the landward limit of marine activity

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2
Q

Foreshore

A

This is the area lying between the high water mark and the low water mark and is often seen as the most important area for marine activity

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3
Q

In shore

A

the area between the low water mark and the point where the waves cease to have any influence on the land around them

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4
Q

Offshore

A

the area between the low watermark and the point where waves cease to have any influence on the land around them

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5
Q

Nearshore

A

the zone extending seaward from the low water mark, it defines the area influenced by the nearshore or longshore currents.

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6
Q

How can coastal landscapes be viewed as systems?

A

within a coastal landscape these three components ( Inputs, Processes and Outputs) store and transfer energy and material on time scales that can vary from a few days to millennia.

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7
Q

Inputs in coastal systems

A
  • Kinetic energy from the waves and wind
  • Thermal energy from the sun
  • Potential energy from material on the slopes
  • Material from marine erosion/deposition
  • Material from weathering and mass movements from cliffs
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8
Q

Processes in a coastal system

A
  • Accumulation of material on beach and nearshore sediment
  • flows of material through transportation methods and longshore drift
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9
Q

Outputs in a coastal system

A
  • Evaporation
  • Marine erosion
  • Wind erosion
  • Landforms
  • Transfer of material to another system ( Sediment cell )
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10
Q

Sediment cell definition

A

A sediment cell is a stretch of coastline and its associated nearshore area within which the movement of coarse material, sand and shingle is largely self contained.

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11
Q

Sediment cell is a ….

A

closed system ( Material is not transfered from one cell to the other … except in high tides or storm surges. the material therefore stays in the sediment cell and is recirculated around)

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12
Q

Dynamic equilibrium definition

A

Dynamic equilibrium in a sediment cell is where input and outputs of sediment are in a constant state of change but ​remain in balance​.

The dynamic equilibrium may be upset in the ​long term​ by ​human interventions​, or in the ​short term​it may be interrupted by ​natural variations​.

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13
Q

Wind’s influence on coastal landscapes

A
  • Also known as aeolian processes
  • the source of energy for coastal erosino and sediment transport is through wave action
  • wave action is generated by the frictional drag or winds across the oceans surface
  • the higher the wind speed the faster the erosion rate as the waves have more energy and velocity
  • Onshore winds ( Towards the land) are effective at driving waves towards the land
  • wind is a moving force which results in erosion transportation and deposition processes.
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14
Q

Wave’s influence on coastal systems

A
  • A wave possess the potential energy from the postition of the wave trough, as well as kinetic energy from the motion of the water
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15
Q

swash definition

A

as the wave moves up the beach

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16
Q

back wash definition

A

as the wave moves down the beach ( drawn down)

17
Q

Breaking waves - Spilling waves

A

steep waves breaking onto gently sloping beaches water spills gently forward as the wave breaks

18
Q

Breaking waves - Plunging waves

A

Moderatley steep waves breaking onto steep beaches water plunges vertically downwards as crest curls over

19
Q

Breaking waves - Surging

A

Low angle waves breaking onto steep beaches the wave slides forward and may not actually break

20
Q

Constructive waves

A

Low in height, long wavelength, low frequency.
- Usually break as spilling waves with strong swash and weak backwash

21
Q

Destructive waves

A

Greater in height, shorter wave length, higher frequency
- usually break as plunging waves on steep beaches slow swash strong backwash removes sediment from beaches

22
Q

Tides Definition

A

Tides are caused by the gravitational pull of the moon and to a lesser extent the sun

23
Q

How do tides affect the coastal system?

A

Tides are an important factor in considering coastal processes as their interation with the coastal environment to a large extent determines the location of many coastal landforms.

  • weak tidal currents and small tidal range determine the shape and extent of river details as well as the size of beach profiles. The extent of the tidal range will also influence the rates of erosion found at cliffs
24
Q

How does Lithology influence the coastal system?

A
  • Lithology is the physical and chemical composition of rock
  • Some rock types such as clay have a weak lithology with little resistance to erosion, weathering and mass movements.
  • This is because the bonds between particles that may make up the rock are weak and easy to break apart
25
How does structure influence the coastal system?
The rock strata needs to be stable in order to withstand erosion,mass movement and weathering. Without a stable rock strata and structure erosion rates will increase in turn also increasing sediment budget.
26