WJEC A-Level Geography 601-8455-3
Coastal Landscapes
Glaciated Landscapes
Tectonic Hazards
Changing Places
Water and Carbon Cycles
Global Migration
Global Governance of the Oceans
EcosystemsContemporary theme
Economic Growth and Challenge: IndiaContemporary theme
Economic Growth and Challenge: ChinaContemporary theme
Development in an African ContextContemporary theme
Energy Challenges and DilemmasContemporary theme
Weather and ClimateContemporary theme
Fieldwork and Geographical Skills
Coastal Landscapes
Coastal change over different timescales
- 2 things to know
- AS Unit 1
Overview
How one storm event can alter a cliff profile, seasonal change in a beach profile in the UK and eustatic change in sea level.
What you need to know
Answer each one before you reveal it.
Explain how one storm event can alter a cliff profile.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Over what timescale can a single storm change a cliff profile?
Model answer
Within seconds to hours, as a rock fall or a rapid slump removes part of the face.
- 2
Explain how one storm event can alter a cliff profile.
Model answer
Exceptionally high waves deepen the wave-cut notch and saturate the material above, so an undercut mass fails and collapses in a single event.
- 3
Describe the seasonal change in a beach profile in the UK.
Model answer
The beach is steeper and higher in summer under constructive waves, and lower and flatter in winter with an offshore bar as destructive waves dominate.
- 4
Why does the beach material moved offshore in winter usually return?
Model answer
Constructive waves in calmer weather have a stronger swash than backwash, so they carry the sediment from the offshore bar back up the beach.
- 5
Define eustatic change in sea level.
Model answer
Eustatic change is a worldwide change in the volume of water in the oceans, or in the capacity of the ocean basins, altering sea level globally.
- 6
Give two causes of eustatic sea level rise.
Model answer
The melting of land-based ice adding water to the oceans, and the thermal expansion of seawater as it warms.
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