AQA A-Level Geography 7037
Water and Carbon Cycles
Hot Desert Systems and LandscapesLandscape
Coastal Systems and LandscapesLandscape
Glacial Systems and LandscapesLandscape
HazardsHazards or ecosystems
Ecosystems Under StressHazards or ecosystems
Global Systems and Global Governance
Changing Places
Contemporary Urban EnvironmentsHuman option
Population and the EnvironmentHuman option
Resource SecurityHuman option
Hazards
Seismic Hazards, Distribution and Magnitude
- 3 things to know
- Component 1
Overview
Recall questions on tsunamis, liquefaction and earthquake-triggered landslides, the plate margins and Pacific Ring of Fire where earthquakes concentrate, intraplate earthquakes and randomness, and the logarithmic moment magnitude scale and the frequency-magnitude relationship.
What you need to know
Answer each one before you reveal it.
What effects does liquefaction have on buildings and underground structures?
What are intraplate earthquakes and what causes them?
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define a tsunami.
Model answer
A large ocean wave generated by sudden vertical displacement of the seafloor, typically from submarine earthquakes, volcanic eruptions, or underwater landslides.
- 2
What happens to tsunami wave height as waves approach shallow coastal waters?
Model answer
Wave height increases dramatically due to wave shoaling.
- 3
Explain why tsunamis become more destructive as they reach coastlines.
Model answer
Wave shoaling in shallow water causes the wave to slow down and increase dramatically in height.
- 4
Define liquefaction.
Model answer
When saturated, loosely packed sediments lose their strength and behave like a liquid during seismic shaking.
- 5
What effects does liquefaction have on buildings and underground structures?
Model answer
Buildings sink, tilt, or collapse, while underground structures such as pipes and tanks rise to the surface.
- 6
What conditions make slopes particularly susceptible to earthquake-triggered landslides?
Model answer
Slopes with weak or saturated materials are particularly susceptible when destabilised by seismic shaking.
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