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Coastal Erosion and Management: Techniques and Solutions, Schemes and Mind Maps of Engineering

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.

What you will learn

  • What are the main causes of coastal erosion?
  • What are the advantages and disadvantages of hard coastal protection?
  • How do soft coastal defenses differ from hard coastal defenses?

Typology: Schemes and Mind Maps

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GeoFactsheet
January 1997Number 8
Coastal Management
Since they are often extensive areas of flat, fertile, picturesque land, coastal areas are very attractive for a wide range of human activities.
However, approximately 25% of the English coastline has been heavily developed for housing, industry, agriculture and leisure and is
always under attack from both the local weather and the action of the sea, resulting in coastal erosion. This Factsheet will discuss the
problems caused by coastal erosion and the techniques used to reduce them.
Groynes
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.
Polders
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:
Wind
Wave action
Tides
Types of sediment and sediment
transport patterns
Storms
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:
To provide defence against water inundation
(flooding)
To provide protection against coastal erosion.
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.
Boulders
Reduce wave energy reaching
coastline and stabilise sediments.
Drainage
Concrete Wall
Absorb wave energy, preventing
erosion and flooding.
Iron Bar
High tide
Storm
pf3

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Geo Factsheet

January 1997 Number 8

Coastal Management

Since they are often extensive areas of flat, fertile, picturesque land, coastal areas are very attractive for a wide range of human activities.

However, approximately 25% of the English coastline has been heavily developed for housing, industry, agriculture and leisure and is

always under attack from both the local weather and the action of the sea, resulting in coastal erosion. This Factsheet will discuss the

problems caused by coastal erosion and the techniques used to reduce them.

Groynes

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.

Polders

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:

  • Wind
  • Wave action
  • Tides
  • Types of sediment and sediment transport patterns
  • Storms

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:

  • To provide defence against water inundation (flooding)
  • To provide protection against coastal erosion.

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.

Boulders

Reduce wave energy reaching coastline and stabilise sediments.

Drainage

Concrete Wall

Absorb wave energy, preventing erosion and flooding.

Iron Bar

High tide

Storm

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:

  • Produce site specific management plans covering coastal cells (see Fig 2).

These are sections of coast where the system of erosion and deposition is to a large extent self- contained.

  • Take account of natural coastal processes and current and future land use.
  • Provide sustainable coastal defences. These are defences which are economical and not environmentally damaging at the present time, or in the future.
  • Encourage co-operation between District Councils and the Environment Agency, the agencies jointly responsible for coast and flood protection.
  • Account for rising sea level and increased storm frequency.

Table 1. Advantages and

disadvantages of hard coastal

protection

Advantages

  • Effective on a local scale through both absorbing and reducing wave energy and retaining local structures.
  • Protection and reassurance for people and property in the coastal environment.
  • Increase in land available for human use. Hard sea defences such as sea walls make coastal land available for agricultural development such as the Dutch Polders. Groynes and breakwaters maintain beaches which have a high recreational value.

Disadvantages

  • Localised or isolated coastal protection can be counter-productive on a larger scale. Defence work in one area has consequences for neighbouring regions, e.g. groynes may prevent sediment reaching a spit formation in an area further down the coastline, or offshore breakwaters may interefere with natural currents and sediment transport, causing erosion.
  • Hard coastal defences such as sea walls require continual, expensive maintenance. To upgrade a concrete armoured sea wall costs around £3000 to £5000 per metre.
  • Hard defences cannot respond to predicted sea level changes due to global warming, e.g. Southern Britain is predicted a 15m to 80m sea level rise by 2050, combined with increased storm frequency, causing severe problems for existing defences.
  • Sea defence walls directly behind natural ecosystems, such as saltmarshes, prevent the ecosystem responding to sea level change and increased erosion.

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:

  • The binding effect of the saltmarsh vegetation, with its extensive root system, causes continual accumulation of sediment. Consequently, tidal inundation becomes less frequent and a protective barrier is produced between the coast and the sea which reduces tidal energy, even during storms. The shallower the slope of the region, the more energy is lost from the waves before they break.
  • The friction of the rough marsh vegetation reduces tidal energy.
  • The creek system covering saltmarshes divides progressively moving landward. These resultant smaller branches provide an increasing surface area to incoming water, increasing friction, so again reducing tidal energy.
  • Saltmarshes are dynamic, being able to adapt to changing tidal range and sea level. This is obviously important with the predicted changes over the next 100 years.

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