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The issues caused by coastal erosion, focusing on the british coastline. It covers the definition of coastal erosion, its causes, and the techniques used to mitigate it, including soft coastal defenses like groynes, sea walls, and boulders, and hard coastal defenses such as concrete walls and iron bars. The document also explores the advantages and disadvantages of hard coastal protection and the importance of natural coastal features like salt marshes and sand dunes in coastal management.
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Coastal Management
Breakwater (timber, rock or other materials) at 90° to the coastline to slow erosion and sediment drifting by deflecting strong currents, and to build up beach level.
Timber or concrete enclosures to encourage sedimentation, causing build up of the coastline.
What is Coastal Erosion?
Coastal erosion can be defined as the loss of land and the encroachment of the sea. It is a complex process involving considerable interactions between the following components:
Coastal erosion is a significant problem to land use. It results in cliff face slumping, loss of coastal land which may have been developed for human activities, erosion of beaches and flooding. For example, studies of the Kent coastline have indicated retreat of cliff areas by 27m between 1872 and 1970. It is therefore essential to devise coastal management plans to minimise any threat to life and to protect natural and man-made features.
Coastal Management
Coastal management plans have two fundamental aims:
The main component of these plans is the presence of coastal defences. These can be broadly divided into two categories:
Soft coastal defences This is the use of natural systems in coastal defence, for example, salt marshes and beaches, which can absorb and adjust to wave and tide energy. Soft coastal defence involves manipulating and maintaining these systems, without changing their fundamental structure.
Hard coastal defences - These are rigid ‘engineering’ solutions, made principally of concrete. Examples include sea walls, breakwaters, groynes and jetties (See Fig 1).
The principle objective of hard engineering is to resist the energy of waves and tides by a fixed structure. At present, such structures protect approximately 10% of the British coastline.
The widespread use of hard coastal defences in coastal protection has both advantages and disadvantages (Table 1).
Fig 1. Examples of hard coastal defences
Stabilise cliff face.
Exam hint - Students should show understanding that coastal erosion and the resultant coastal land forms, such as beaches and cliffs, are a result of the interaction between all of these factors and the shoreline.
Reduce wave energy reaching coastline and stabilise sediments.
Absorb wave energy, preventing erosion and flooding.
Coastal Management (^) Geo Factsheet
Modern Coastal Management
The problems identified with local scale hard coastal defences and an increased understanding of the erosional and depositional processes which operate over many miles of coastline have resulted in the Ministry of Agriculture, Fisheries and Food (MAFF) developing Shoreline Management Plans (SMPs). These use an holistic approach , which means looking at the large scale effect of any management technique. All SMPs have the same fundamental aims:
These are sections of coast where the system of erosion and deposition is to a large extent self- contained.
Table 1. Advantages and
disadvantages of hard coastal
protection
Advantages
Disadvantages
SMPs can only achieve these aims through a combination of both ‘hard’ and ‘soft’ approaches. One of the major components of soft coastal defences are salt marshes.
The Value of Salt marshes
Salt marshes are found in the tidal zone bordering the sea or estuaries. They are composed of grasses and other low growing vegetation colonising sediment deposits (See Fig 2).
Many of the characteristic physical features of saltmarshes enable them to provide a natural sea defence:
Exam hint - Students are very often required to explain how and why the movement of beach material can be controlled. In addition, they should understand how hard coastal defences cause sediment supply to coastal features to both increase and decrease. For example, beach nourishment, groynes and breakwater construction, dredging and dumping can all increase levels of sediment in one area, but reduce supply in others.
Pan
Creek
Saltmarsh cliff
HWMST
LWMST
Figure 2. Generalised saltmarsh showing main vegetation zones
Tidal Flat Algae
Pioneer Zone Sparse Vegetation
Low-Mid Marsh Zone Species-poor Puccinella- dominated communities
Mid-Upper Marsh Zone Species-rich communities with increasing Festuca
Upper Marsh Swamps Brackish communities
Transistion Zone
Drift Zone