Geography coasts revision, Schemes and Mind Maps of Geography

Geography coasts revision mindmap

Typology: Schemes and Mind Maps

2021/2022

Uploaded on 05/18/2025

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Why are coastlines important in the UK?
Here in the UK, we have a coastline over 12,000 km long.
Social - Residential areas = emotional attachment to the area.
- Recreational activities = happy/ healthy community
Economic Tourism = brings money into local community
through employment and
hotels etc.
- Fishing = fish are sold for money that people spend
in local area.
Environmental Provides habitats for animals = breed
Waves
A wave is a movement of energy through water, not a movement of water. The size of
the waves depend on 3 factors;
The FETCH (the distance the wind blows over the water) The greater the fetch,
the more powerful the waves will be.
The STRENGTH of the wind
How LONG the wind blows for
Wave characteristics Constructive waves Destructive waves
Wave height Gentle Steep
Wave length Long Short
Type of wave Spilling Plunging
Strength of swash Strong Weak
Strength of
backwash
Weak Strong
New beach
sediment
Gain Loss
How they are
created
Distant Local
Coastal Processes
Transportation - The movement of sediment along the
coast
Erosion - The breakdown of sediment into smaller
fragments
Deposition - When waves loose energy they leave
behind the smaller pieces.
Traction - large material is rolled along the sea
floor.
Hydraulic Action The force of water into cracks helps
to break it up.
Saltation - beach material is bounced along the
sea floor.
Abrasion Waves fling sand and pebbles against the
rock. These wear away like sandpaper.
Suspension - beach material is suspended and
carried by the waves.
Attrition - Chunks of rock get knocked together and
worn into smaller bits
Solution - material is dissolved and carried by
the water.
Solution Water dissolves the soluble material from
the rock.
Longshore drift A form of transportation that
moves sediment from one end of the coast to
the other.
Weathering
Weathering is when rocks are broken down. There are 3 types of
weathering;
Mechanical (physical) When rocks break up due to water entering
the cracks and freezing and thawing, making the rock weak.
Chemical Caused by chemical changes. Slightly acidic rainwater
slowly dissolves certain rock types
Biological Plant roots grow causing cracks in the rocks and animals
burrow into weak rocks like sand.
COASTS
YEAR 8
Landforms of Erosion
Headland and Bay form along coastlines where there are alternating
outcrops of resistant (harder) and less resistant (softer) rock. The softer
rock erodes faster than the harder rock.
Cave, Arch, Stack and Stump -
Caves occur when waves force their way into cracks in the cliff face.
Eventually it will break through to the other side forming an arch. The arch will
gradually become bigger until it can no longer support the top of the arch.
When the arch collapses, it leaves the headland on one side and a stack (a tall
column of rock) on the other. Overtime, it will eventually collapse to form
a stump.
Landforms of Deposition -
Beach - Found between areas of high and low tide marks. Generally
formed by constructive waves.
Sand dunes - Mounds of sand that are found behind sandy beaches. To
form they require a large flat beach, a good supply of sand, strong wind
and obstacles.
Spit - Sediment is carried by longshore drift. When there is a change in
the shape of the coastline, deposition occurs. A long thin ridge of
material is deposited.
Bar When a spit continues to attach two headlands
Tombola - a spit connecting an island to the mainland
Management of the coast
Hard engineering - using artificial
structures such as sea walls to control
natural processes
Groynes - wooden or stone fences that
are built at right angles to the beach.
They trap sediment being moved by
longshore drift and enlarge the beach.
Traps material and therefore
reduces longshore drift
Reduces flooding rate
Unnatural and ugly
Rock Armour - Large boulders placed
along the coast. The rocks force the
wave to break, absorbing their energy
and protecting the coastline.
Reduces erosion
Reduces flooding.
Unnatural and ugly
In storms it can be moved
Sea Wall A large concrete, often
curved, wall that reflects the energy
back from waves
Creates a promenade for
people to walk along
Reduces flooding.
Unnatural and ugly
Expensive
Soft engineering is using natural processes to protect the coastline.
Beach Replenishment - The addition of sand or shingle to an existing beach to make it higher
or wider.
Relatively cheap and easy to maintain
Blends in with existing beach
Needs constant maintenance
Dune regeneration - Sand dunes are effective buffers to the sea but are easily damaged and
destroyed by trampling.
Maintains a natural coastal environment
Relatively cheap
Needs constant maintenance
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Why are coastlines important in the UK? Here in the UK, we have a coastline over 12,000 km long. Social - Residential areas = emotional attachment to the area.

  • Recreational activities = happy/ healthy community Economic – Tourism = brings money into local community through employment and hotels etc.
  • Fishing = fish are sold for money that people spend in local area. Environmental – Provides habitats for animals = breed Waves A wave is a movement of energy through water, not a movement of water. The size of the waves depend on 3 factors;
  • The FETCH (the distance the wind blows over the water) – The greater the fetch, the more powerful the waves will be.
  • The STRENGTH of the wind
  • How LONG the wind blows for Wave characteristics Constructive waves Destructive waves Wave height Gentle Steep Wave length Long Short Type of wave Spilling Plunging Strength of swash Strong Weak Strength of backwash Weak Strong New beach sediment Gain Loss How they are created Distant Local Coastal Processes Transportation - The movement of sediment along the coast Erosion - The breakdown of sediment into smaller fragments Deposition - When waves loose energy they leave behind the smaller pieces.
  • Traction - large material is rolled along the sea floor. Hydraulic Action – The force of water into cracks helps to break it up.
  • Saltation - beach material is bounced along the sea floor. Abrasion – Waves fling sand and pebbles against the rock. These wear away like sandpaper.
  • Suspension - beach material is suspended and carried by the waves. Attrition - Chunks of rock get knocked together and worn into smaller bits
  • Solution - material is dissolved and carried by the water. Solution – Water dissolves the soluble material from the rock. Longshore drift – A form of transportation that moves sediment from one end of the coast to the other. Weathering Weathering is when rocks are broken down. There are 3 types of weathering; Mechanical (physical) – When rocks break up due to water entering the cracks and freezing and thawing, making the rock weak. Chemical – Caused by chemical changes. Slightly acidic rainwater slowly dissolves certain rock types Biological – Plant roots grow causing cracks in the rocks and animals burrow into weak rocks like sand.

COASTS

YEAR 8

Landforms of Erosion Headland and Bay – form along coastlines where there are alternating outcrops of resistant (harder) and less resistant (softer) rock. The softer rock erodes faster than the harder rock. Cave, Arch, Stack and Stump - Caves occur when waves force their way into cracks in the cliff face. Eventually it will break through to the other side forming an arch. The arch will gradually become bigger until it can no longer support the top of the arch. When the arch collapses, it leaves the headland on one side and a stack (a tall column of rock) on the other. Overtime, it will eventually collapse to form a stump. Landforms of Deposition - Beach - Found between areas of high and low tide marks. Generally formed by constructive waves. Sand dunes - Mounds of sand that are found behind sandy beaches. To form they require a large flat beach, a good supply of sand, strong wind and obstacles. Spit - Sediment is carried by longshore drift. When there is a change in the shape of the coastline, deposition occurs. A long thin ridge of material is deposited. Bar – When a spit continues to attach two headlands Tombola - a spit connecting an island to the mainland Management of the coast Hard engineering - using artificial structures such as sea walls to control natural processes Groynes - wooden or stone fences that are built at right angles to the beach. They trap sediment being moved by longshore drift and enlarge the beach. ✅ Traps material and therefore reduces longshore drift ✅ Reduces flooding rate ❌ Unnatural and ugly Rock Armour - Large boulders placed along the coast. The rocks force the wave to break, absorbing their energy and protecting the coastline. ✅ Reduces erosion ✅ Reduces flooding. ❌ Unnatural and uglyIn storms it can be moved Sea Wall – A large concrete, often curved, wall that reflects the energy back from waves ✅ Creates a promenade for people to walk along ✅ Reduces flooding. ❌ Unnatural and uglyExpensive Soft engineering is using natural processes to protect the coastline. Beach Replenishmen t - The addition of sand or shingle to an existing beach to make it higher or wider. ✅ Relatively cheap and easy to maintain ✅ Blends in with existing beach ❌ Needs constant maintenance Dune regeneration - Sand dunes are effective buffers to the sea but are easily damaged and destroyed by trampling. ✅ Maintains a natural coastal environment ✅ Relatively cheap ❌ Needs constant maintenance

Abrasion: wearing away of cliffs by sediment flung by breaking waves. Arch: This begins as a cave formed in the headland, which is gradually widened and deepened until it cuts through. Attrition: erosion caused when rocks and boulders transported by waves bump into each other and break up into smaller pieces. Backwash: the return of water to the sea after waves break on a beach. Bar: where a spit grows across a bay. Beach: the temporary deposition of sand and shingle along the coastline. Biological Weathering: the breakdown of rock through the action of plants and animals. Chemical Weathering: the decomposition (or rotting) of rock caused by a chemical change within that rock; sea water causes chemical weathering of cliffs. Constructive Waves: found on low-angled beaches and mainly responsible for coastal deposition. They are gently breaking, with a much stronger swash than backwash. Destructive Waves: found on steep beaches, are steeply breaking and mainly responsible for coastal erosion. Their backwash is much stronger than their swash. Erosion: the wearing away of the land by rivers, ice sheets, waves and wind. Fetch: the maximum distance of water over which winds can blow Freeze-Thaw Weathering: Water enters the cracks during the warmer day and freezes during the colder night. As the water turns into ice it expands and exerts pressure on the surrounding rock, causing pieces to break off. Gabions: steel wire mesh filled with boulders used in coastal defences. Groyne: a wooden barrier built out into the sea to stop the longshore drift of sand and shingle Headlands: areas of land protruding out to sea formed of resistant (harder) rock. They help protect the bay which forms between them from wave attack. Hydraulic Action: the process by which breaking waves compress pockets of air in cracks in a cliff. The pressure may cause the crack to widen, breaking off rock. Longshore Drift: waves approaching the coast at an angle result in the gradual zig-zag movement of beach materials along the coast. Sea Defences: measures taken to defend the coast from erosion, cliff collapse and flooding. Sea Walls: aim to prevent erosion of the coast by providing a barrier which reflects wave energy. Spit: a long, narrow accumulation of sand and shingle formed by longshore drift and deposited where the coastline abruptly changes direction. Stack: rock left standing out at sea after wave erosion has separated it from the mainland. Swash: forward movement of a wave up a beach. Tombolo: a spit joining an island to the mainland. Waves: caused by the transfer of energy from the wind blowing over the surface of the sea. Weathering: the break-down of rock by physical or chemical processes.

Key Words Revision Tasks:

  • Make a mindmap/ poster/ revision cards/notes/ presentation/ song/ answer the following questions.

1. Define deposition.

2. Define weathering

3. How long is the UK coastline?

4. True or false: attrition makes pebbles more rounded and less angular.

5. What is the name given to the movement of water up the beach after a

wave breaks?

6. Why is the coast important?

7. Name the two types of engineering involved in coastal management.

8. Name a landform of deposition

9. Draw and name the four types of erosion.

10. List the features of a constructive wave.

11. What feature is formed when a spit extends out to join the mainland to

an island offshore?

12. There are three factors that effect the size of a wave, what are they?

13. Label the features in image a.

14. Annotate the photo b, with coastal processes you can see.

15. Compare a constructive wave with a destructive wave.

16. What is the difference between social, economic and environmental

reasons the coast is so important.

17. State a method of hard engineering to manage the coast.

18. Describe how groynes help to manage the coast.

19. Explain the processes of longshore drift

20. Explain the four processes of erosion

21. Explain the four processes of transportation

22. Explain the formation of a headland and bay

23. Explain the formation of a spit

24. Justify the need to manage the coast.

25. Discuss the benefits of using hard engineering to manage the coast.

Command Words: Analyse - Take apart an idea, concept or statement and criticise it. Assess - Come to a conclusion about the overall value or significance of something; discuss its positive and negative aspects to show balance. Compare - Identify similarities and differences. Define - State the meaning of an idea or concept. Describe - Set out the main characteristics of something; DON’T EXPLAIN. Discuss - Set out both sides of an argument (for and against) and come to a conclusion; there should be some evidence of balance. Evaluate - Make a judgement about the effectiveness of something; discuss its strengths and weaknesses and come to a conclusion about its overall success or importance. Explain - Give reasons why something happens. Give - Produce an answer from recall. Justify - Support an idea or argument with evidence; for the outcome chosen, the positives must outweigh the negatives. State = name b. a.