Section C: UK physical landsacpes

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  • Created by: thingy
  • Created on: 18-04-18 17:31

Wave types and Characteristics

the wind blows across the sea forming waves (distance wind blows- fetch)

Swash- water that rushes up the beach

backwash- water that flows back towards the sea

Constructive waves- formed by storms (far from the shore) low surging waves deposits sand and pebbles up the beach- constructing it

destructive waves- formed by storms (near the shore common in winter) high plunging waves with weak swash and strong backwash

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Coastal proccesses

Weathering

  • mechanical- freeze thaw (freezes water in the cracks and expands causing weathering)
  • chemical- acid rain dissolves rocks (limestone)

Mass movement- the downward movement of material under the influence of gravity 

  • sliding- rocks slide downhill
  • slumping- saturated rock slides down a curved slip plane
  • rockfalls- rock breaks away
  • erosion
    • hydraulic power- waves smash into cliffs trapping rocks 
    • abrasion- break waves throw sand, pebbles or boulders against the coast
    • attrition- rocks/pebbles rub together and break down
  • transportation
    • longshore drift-  when the wave approaches the coast at an angle sand and gravel move along the beach in a zigzag pattern, as the sand is lighter it moves further
  • deposition- water slows down the wave loses their energy
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formation of landforms

erosion:

  • Headlands and bays- bays errode faster (softer rock and headlands harder rock)
  • cliffs and wavecut platforms (flat rock at the base of a cliff)
  • Caves, arches and stacks- when 2 caves errode it forms an arch, this then collapses to form a stack

deposition:

  • beaches
  • sand dunes- wind blows the sand on the beach inland
  • spits- where the coastline orientation changes
  • offshore bars- sediment experiences friction with a gentle sloping coast
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An example of major landforms of erosion and depos

discordant coastline (Swanage Bay and Duriston Head)- alternating bands of soft and hard rock are found on the east coastline (clay and sand- soft)

concordant coastline- the south coast is mainly formed of one type (limestone- hard)

Poole harbour (one of the UK's largest natural harbours)- deposition- the formation of 2 spits (sanbanks), lagoons, slatmarshes and sand dunes 

Foreland- white chalk cliffs and old harry stack

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Management stratergies

Hard engineering:

  • sea walls- expensive but reliable (£10,000 per metre)
  • rock armour- looks messy but quick to build (£3000 per metre)
  • gambions- cheap and easy to build but dangerous (£500 per metre)
  • groynes- widens beach (£5000 each- covers 200 metres)

Soft engineering:

  • beach nourishment- widens beach (£200,000)
  • beach reprofiling- improves seafront property protection but makes beach access harder (£250,000 every 2 years)
  • dune regeneration- natural barrier to wind and waves but can move or errode (£2000 per metre)
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An example of a coastal management scheme in the U

reasons for management:

  • Unstable cliff (erosion more rapid due to waves)
  • need to reduce the threat of landslips

management stratergies:

  • environment improvement scheme (1990's)
  • 3 main phases
    • 1) seawall and promenade created to stabilise cliffs (1990-95 £1.4 million)
    • 2) new sea wall, promenades and widen beach (2005-07 £22 million)
    • 3) 390m of sea wall to protect homes (2010-15 £20 million)

effects and conflicts

  • businesses thriving
  • harbour better protected
  • traffic and litter increased
  • defences spoilt natural landscape 
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