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
Tectonic Hazards
Earthquake hazards and ground behaviour
- 2 things to know
- AS Unit 1 and A2 Unit 4
Overview
Ground shaking, why soft sediment increases earthquake damage and city damaged by seismic amplification.
What you need to know
Answer each one before you reveal it.
Define liquefaction.
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is ground shaking?
Model answer
Ground shaking is the vibration of the land surface as seismic waves pass through it, and it is the direct cause of most earthquake damage.
- 2
What determines how strongly a particular site is shaken?
Model answer
The magnitude of the earthquake, the distance from the epicentre and the depth of the focus, together with the local geology and the duration of the shaking.
- 3
Explain why soft sediment increases earthquake damage.
Model answer
Loose, water-rich sediment amplifies the seismic waves and prolongs the shaking compared with solid bedrock, so buildings standing on it are shaken harder and for longer.
- 4
Give an example of a city damaged by seismic amplification.
Model answer
Mexico City in 1985, where buildings founded on the soft sediments of a drained lake bed collapsed even though the epicentre lay some 350 km away.
- 5
Define liquefaction.
Model answer
Liquefaction is the loss of strength of saturated, loosely packed sand or silt during shaking, when the water pressure between the grains rises until the material behaves like a liquid.
- 6
What are two visible effects of liquefaction?
Model answer
Buildings tilt or sink into the ground while lighter buried structures such as pipes and tanks float upwards, and grey silt is forced to the surface through cracks.
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