AQA GCSE Geography
Tectonic hazards — AQA GCSE Geography revision
Free revision notes, key terms, common exam traps and 5 practice questions with answers. About 8 minutes to read.
Plate tectonics
- The Earth's crust is split into plates that move on the semi-molten asthenosphere, driven by convection and by slab pull at subduction zones (slab pull is now regarded as the dominant force).
- Destructive (convergent) margins: denser oceanic crust subducts beneath continental crust, producing deep earthquakes, ocean trenches, fold mountains and explosive composite volcanoes.
- Constructive (divergent) margins: plates move apart, magma rises to fill the gap, producing shallow earthquakes and gentle shield volcanoes (e.g. mid-ocean ridges). Conservative margins: plates slide past each other, causing earthquakes but no volcanoes.
Effects and responses
- Primary effects happen instantly (buildings collapse, deaths, roads fractured); secondary effects follow (fires from ruptured gas mains, disease from broken water pipes, business closure, homelessness).
- Immediate responses happen in hours/days (search and rescue, emergency aid, temporary shelter); long-term responses take months/years (rebuilding to earthquake-resistant standards, retraining, new hazard plans).
- Impacts are usually more severe in lower-income countries because of weaker building regulations, fewer emergency services, less insurance and slower recovery funding — the hazard is natural, the disaster is largely human.
Key terms
- Natural hazard
- A natural process that threatens people or property.
- Subduction
- The sinking of denser oceanic crust beneath another plate at a destructive margin.
- Focus
- The point underground where an earthquake originates.
- Epicentre
- The point on the surface directly above the focus.
- Primary effect
- An impact caused directly and immediately by the hazard event.
- Secondary effect
- An impact that follows on from the primary effects.
Common exam traps
- Writing that plates move only because of convection currents — slab pull at subduction zones is now seen as the main driver.
- Confusing focus (underground origin) with epicentre (point on the surface above it).
- Calling fires or disease a primary effect — they follow the shaking, so they are secondary.
Practice questions with answers
1. At which plate margin is oceanic crust destroyed?
- • Constructive
- • Destructive
- • Conservative
- • Collision
Answer: Destructive
Denser oceanic crust subducts and melts at a destructive margin.
2. Which landform is typical of a constructive plate margin?
- • Ocean trench
- • Mid-ocean ridge
- • Fold mountains
- • Rift-free plateau
Answer: Mid-ocean ridge
Plates separating allow magma to rise and build a ridge of new crust.
3. A conservative margin produces which combination?
- • Earthquakes only
- • Volcanoes only
- • Both earthquakes and volcanoes
- • Neither
Answer: Earthquakes only
Plates slide past one another; no crust is created or destroyed, so no magma rises.
4. Define the term 'primary effect' of an earthquake and give one example.
Answer: An immediate, direct impact of the shaking, e.g. buildings collapsing
Primary effects are caused by the event itself, not by knock-on consequences.
5. Which is a secondary effect of a volcanic eruption?
- • Lava burning farmland
- • Ash fall damaging roofs
- • Long-term loss of tourist income
- • Pyroclastic flow deaths
Answer: Long-term loss of tourist income
Economic decline follows the event rather than being caused directly by it.
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This topic has 51 questions in total, plus flashcards, cram mode and Grade 9 Push challenges.
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