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case study for coastal erosion, Schemes and Mind Maps of Earth Sciences

Background and the Problem of Erosion. - The Holderness Coast is on the NE coast of the UK, facing the North Sea. - It extends 60km from Flamborough in the ...

Typology: Schemes and Mind Maps

2021/2022

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Case Study of Coastal Erosion - Flamborough Head and Holderness Coast
Background and the Problem of Erosion
-The Holderness Coast is on the NE coast of the UK, facing the North Sea.
- It extends 60km from Flamborough in the north to Spurn Point in the south.
- Coastline mainly made up of cliffs (20-30m high), made of soft, easily eroded boulder clay.
- Where the cliff line meets the Humber Estuary, a spit has formed due to the change in the
direction of the coastline - Spurn Head.
-The cliff line is retreating at an alarming rate - greater than 1.5m/year (fastest rate in
Europe) around 2 million tonnes of material every year
- 4km of land have been lost since Roman Times, including villages + farm buildings
-Easington Gas Station (N Sea Gas terminal) is located on cliffs top, its position under threat.
-Spurn Point, a spit in the S, is increasingly at risk (erosion) and is 5km long and covers 1.5km2
- Spurn Point is important to protect from erosion, because it is a designated National Nature
Reserve, Heritage Coast and Special Protection Area.
-The landward-side mudflats are an important feeding ground for wading birds
-The RNLI lifeboat station at Spurn Point, built in 1810, is very important for the safety of
shipping in the area and is at a vital location along the Humber Estuary, which is a busy
shipping route.
-Humber Vessel traffic service located on the spit, operates 24-hour service for river users.
- major function is to monitor and regulate navigation of those parts of the Humber Estuary
and Rivers Ouse and Trent.
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Case Study of Coastal Erosion - Flamborough Head and Holderness Coast Background and the Problem of Erosion

  • The Holderness Coast is on the NE coast of the UK, facing the North Sea.
  • It extends 60km from Flamborough in the north to Spurn Point in the south.
  • Coastline mainly made up of cliffs (20-30m high), made of soft, easily eroded boulder clay.
  • Where the cliff line meets the Humber Estuary, a spit has formed due to the change in the direction of the coastline - Spurn Head.
  • The cliff line is retreating at an alarming rate - greater than 1.5m/year (fastest rate in Europe) around 2 million tonnes of material every year
  • 4km of land have been lost since Roman Times, including villages + farm buildings
  • Easington Gas Station (N Sea Gas terminal) is located on cliffs top, its position under threat.
  • Spurn Point , a spit in the S, is increasingly at risk (erosion) and is 5km long and covers 1.5km^2
  • Spurn Point is important to protect from erosion, because it is a designated National Nature Reserve, Heritage Coast and Special Protection Area.
  • The landward-side mudflats are an important feeding ground for wading birds
  • The RNLI lifeboat station at Spurn Point, built in 1810, is very important for the safety of shipping in the area and is at a vital location along the Humber Estuary , which is a busy shipping route.
  • Humber Vessel traffic service located on the spit, operates 24-hour service for river users.
  • major function is to monitor and regulate navigation of those parts of the Humber Estuary and Rivers Ouse and Trent.

Causes of Coastal Erosion Physical Causes: Beaches:

  • Only narrow beaches , so there are no beaches to reduce the erosive power of the waves.
  • The chalk headland of Flamborough Head prevents transport of materials from the north, thus little beach material is transported southward to the beaches of Holderness.
  • Coast is subject to full force of the waves from the North Sea with little reduction in wave energy before they reach the cliff line
  • The sea is continually able to reach the base of the cliff Lithology:
  • Lithology: cliffs made up of boulder clay and chalk - both easily eroded by abrasion and hydraulic action and are non-resistant
  • This boulder clay is also prone to mass movement in the form of landslides and rotational slumps, when the rock becomes saturated
  • The chalk rock has many joints and bedding planes which are easily eroded by wave action to form caves, arches and stacks on the headland Powerful Waves:
  • Powerful destructive waves often attack the coast, as the waves have a long fetch , all the way across the Arctic Ocean, allowing them to build up energy as they are blown by the wind.
  • The coast also faces the dominant wind and wave direction (from the NE), so most powerful waves have little to reduce and dissipate their energy before they erode the cliffs
  • Frequent storms from the NE provide the most powerful wave action
  • Tides carry away sediment from the North to the South where it is deposited. Rising Sea Levels :
  • Increasing volume of water in the oceans, greater power to erode the coastline
  • Allows water to reach further inland without losing as much energy, allows greater erosion of retreating cliff faces. Human Causes: Beaches:
  • Beaches are also kept narrow due to coastal defences , such as the groynes at Hornsea, starve down- drift beaches of sediment resulting in thinner and narrower beaches which don’t protect cliffs as well, greater rate of erosion Offshore Dredging:
  • Dredging reduces the amount of sediment available to build up beaches, nearly 4 000 000 tonnes of material was removed during 2000 under licence
  • It is thought that unlicensed dredging occurs closer to the shore, which would have an even worse effect than licenced dredging occurring further offshore. Development:
  • Many settlements + buildings built, due to low value of land, on areas at risk and are now at threat from erosion, worsening the effect of erosion and increasing loss of infrastructure.
  • Building on cliff tops has increased runoff and may have made the cliffs more unstable