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Coastal Coastal Processes and Processes and Landforms Landforms

Coastal Processes Good

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Page 1: Coastal Processes Good

Coastal Processes Coastal Processes and Landformsand Landforms

Page 2: Coastal Processes Good

Why are waves generally larger in the south west than in the south east?

Wave energy depends on the fetch, the strength of the wind and the length of time over which the wind has blown.

Look at an atlas or a wall map to find out the largest fetch around the British Isles.

fetch = the distance over which the wind has blown

Page 3: Coastal Processes Good

Why do waves break?

wavelength

the bottom of the wave touches the sand, slows down and the top of the wave topples over

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Backwash

Swash

Note: Backwash is always at right angles to the beach

Swash and backwash

Page 5: Coastal Processes Good

Types of waves

Destructive Waves

Constructive Waves

backwash>swash

swash>backwash

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Attrition

Hydraulic action

Abrasion

Corrosion

Processes of erosion

Processes of erosion

Page 7: Coastal Processes Good

Attrition

Material carried by the waves bump into each other and so are smoothed and broken down into smaller particles.

Abrasion/Corrasion

This is the process by which the coast is worn down by material carried by the waves. Waves throw these particles against the rock, sometimes at high velocity.

Hydraulic action

This process involves the force of water against the coast. The waves enter cracks (faults) in the coastline and compress the air within the crack. When the wave retreats, the air in the crack expands quickly causing a minor explosion. This process is repeated continuously.

Corrosion

This is the chemical action of sea water. The acids in the salt water slowly dissolve rocks on the coast. Limestone and chalk are particularly prone to this process.

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Landforms of coastal erosion

1) Headlands and Bays

2) Cliffs and Wave Cut Platforms

3) Caves, Arches, Stacks and Stumps

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An example of headlands and bays on the Dorset coastline…

chalk

clay

limestone

Swanage Bay

Page 10: Coastal Processes Good

The waves attack the base of the cliff through the processes of abrasion, corrosion, hydraulic action and attrition.

Over time the cliff will be undercut and a wave-cut notch is formed.

Eventually the cliff becomes unstable and collapses. Further cliff retreat will form a wave-cut platform.

Wave-cut platform

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Wave-cut platform – Burgh Island, Devon

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Caves, arches, stacks and stumps

1. The waves erode FAULTS (cracks) in the headland.2. The waves eventually erode through the

headland to form an ARCH.

3. The arch becomes unsupported and collapses to form a STACK.

4. A STUMP is formed from the collapsed stack.

C DBA

Match the image with the most appropriate label.

1 23 4

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If these photos were taken of one headland over time, which of these landforms would be the first to be formed?

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This is a cave (‘Stair Hole’).

This is an arch (‘Durdle Door’).

This is a stack (Old Harry’s Rocks).

These are stumps.