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© Boardworks Ltd 2014 1 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not For more detailed instructions, see the Getting Started presentat Coastal Processes and Landforms Part 5 These icons indicate that teacher’s notes or useful web addresses are available in the Notes Page.

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Page 1: © Boardworks Ltd 20141 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20141 of 8

This icon indicates that the slide contains activities created in Flash. These activities are not editable.

For more detailed instructions, see the Getting Started presentation.

Coastal Processes and LandformsPart 5

These icons indicate that teacher’s notes or useful web addresses are available in the Notes Page.

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Key QuestionsHow do waves operate?What are sub-aerial processes and why are they important?What processes of erosion operate at the coast?What landforms are created by erosion?What processes of transport operate at the coast?What landforms are created by deposition?

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1) Beaches

2) Spits

3) Tombolos and Bars

Landforms of coastal deposition

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How are beaches formed?

Beaches form in sheltered environments, such as bays. When the swash is stronger than the backwash, deposition occurs.

Sometimes sand from offshore bars can be blown onto the shore by strong winds.

In such cases dunes may form – such as at Studland on the Dorset Coast.

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How are spits formed?

A spit is deposited material that extends out from the mainland at one end.

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How are spits formed?

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If a spit joins the mainland to an island it is called a tombolo.

At Chesil Beach in Dorset, the mainland is joined to the Isle of Portland.

What is a tombolo?

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If a spit joins one part of the mainland to another it is called a bar.

For example, there is a bar at Orford Ness in Suffolk.

What is a bar?