1. What is this?
Can you guess how it has been formed?

2. Transportation and deposition
L/O: Describe and explain the process of longshore drift
Outcome
All – list and describe deposition features
Most – Explain longshore drift
Some – Apply yhis knowledge to a real landscape
Starter - look at this map
Why do the headlands stick out but the bay does not?

3. Where has my beach ball gone?
Coastal Mystery
Where has my beach ball gone?
Last year I had a lovely trip to the seaside. I didn’t go to Swanage Bay but instead went to the more natural surroundings of Studland Bay
I put down my bucket, spade and beach ball, laid out my towel and fell asleep in the nice hot sun.
When I woke up my beach ball had disappeared?
Please help me find my beach ball?

4. Which are the important Clues?
Use your Map (you mark on information with a white board pen)
Discuss in your groups
Sort the clues (categorise them)

5. Have you solved the Mystery?
What clues are most important?
Where is the ball?
Can you explain how it got there?
Write down you ideas to feed back to the class
Nominate a spokesperson to represent your group

6. How is sediment transported along the coast?

7. Longshore drift Direction of movement
Backwash is always at right angles to the beach
swash
Backwash
This movement of sediment along the coastline is called longshore drift.

8. Study the photograph of Swanage Beach.
Level 4
I say what longshore drift is
Level 5
I explain how long shore drift works.
Level 6
I explain in detail how longshore drift works.
Level 7
I use examples from the Dorset coast to explain how longshore drift works
How is this beach different to Studland bay?
What is the purpose of the wooden groynes?
Add an arrow to the photo to show which direction longshore drift is operating in.
Draw your own diagram to explain how longshore drift operates.

9. What landforms are created by deposition?
Learning objectives

10. Landforms of coastal deposition
Beaches
Spits
Tombolos and Bars

11. 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.

12. How are spits formed?

13. How are spits formed?

14. How are spits formed?

15. How are spits formed? (use diagram to help you)
Level 4
I say what a spit is
Level 5
I explain how a spit is formed.
Level 6
I explain in detail how a spit is formed.
Level 7
I use examples from the Dorset coast to explain how a spit is formed.

16. Coastal landforms in Studland
Drag and drop exercise.

17. Erosion or deposition?

18. Key Ideas
Waves are the result of the wind blowing over the sea. They break as they approach land.
Swash and backwash describe the movement of a wave on the beach. Fetch is the distance that the wind has travelled.
Sub-aerial processes such as weathering and mass movement occur on the cliff face.
Coastal processes of erosion include hydraulic action, attrition, corrosion and solution.
Landforms created by erosion include headlands and bays, caves, arches, stacks and stumps.
Longshore drift is a method of coastal transport.
Landforms created by deposition include beaches, spits, tombolos and bars.