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Landforms of coastal erosion

Date post: 24-Feb-2016
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Landforms of coastal erosion. Headlands and Bays Cliffs and Wave Cut Platforms Caves, Arches, Stacks and Stumps. Swanage Bay. Example of headlands and bays on the Dorset coastline. Headlands and bays. How are cliffs and wave-cut platforms formed?. Wave-cut platform. - PowerPoint PPT Presentation
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Page 1: Landforms of coastal erosion
Page 2: Landforms of coastal erosion

Landforms of coastal erosion• Headlands and Bays• Cliffs and Wave Cut Platforms• Caves, Arches, Stacks and Stumps

Page 3: Landforms of coastal erosion

Swanage Bay

Example of headlands and bays on the Dorset coastline.

Page 4: Landforms of coastal erosion

Headlands and bays

Page 5: Landforms of coastal erosion

How are cliffs and wave-cut platforms formed?

Page 6: Landforms of coastal erosion

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

Page 7: Landforms of coastal erosion

How are caves, arches, stacks and stumps formed?

Page 8: Landforms of coastal erosion

Caves, arches, stacks and stumps

Page 9: Landforms of coastal erosion

The formation of caves, arches, stacks and stumps

Page 10: Landforms of coastal erosion

10

* A Blowhole may

form if the erosion at the

back of the cave breaks through the roof to the top

of the cliff.

This usually happens at hightide in stormy weather.

Copy this note!

Page 11: Landforms of coastal erosion

11

*Geos*Geos are formed when caves eroded

backwards into a main cliff. Over time the caves begin to get wider and the roof becomes unsupported.

*The roof collapses and creates a narrow inlet into the cliff.

Page 12: Landforms of coastal erosion

*Geos & Blow-holes

Page 13: Landforms of coastal erosion

How waves operate

Page 14: Landforms of coastal erosion

Why do waves break?

Waves are the result of the wind blowing over the sea: as they approach land they break. The bottom of the wave touches the sand and slows down due to increased friction. The top of the wave becomes higher and steeper until it topples over.

Page 15: Landforms of coastal erosion

Backwash

Swash

Backwash is always at right angles to the beach

Swash and backwash

Page 16: Landforms of coastal erosion

Why are waves larger in the south west?

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

wind has blown.

Page 17: Landforms of coastal erosion

Types of waves

Page 18: Landforms of coastal erosion

What do you know about waves?

Page 19: Landforms of coastal erosion

What are sub-aerial processes and why are they important?

Page 20: Landforms of coastal erosion

*What are sub-aerial processes?The coast is the narrow zone between the land and the sea.It is worth remembering that the landscape will be influenced by processes on the land as well as the sea.Sub-aerial processes include weathering and mass movement. These processes operate on the cliff face to weaken it and provide material for coastal erosion.

Page 21: Landforms of coastal erosion

*Impact of sub-aerial processes

Page 22: Landforms of coastal erosion

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