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What are natural hazards, and why do earthquakes and volcanoes happen where they do?

Definition and types of natural hazard, hazard risk; plate tectonics theory, plate margins, and the effects of and responses to a tectonic hazard in a contrasting pair of countries.

A focused answer to AQA GCSE Geography 3.1.1, covering types of natural hazard, hazard risk, plate tectonics theory, the three plate margins, and the contrasting effects of and responses to earthquakes in Nepal and Italy.

Generated by Claude Opus 4.89 min answer

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  1. What this dot point is asking
  2. Types of natural hazard and hazard risk
  3. Plate tectonics theory
  4. The three plate margins
  5. Contrasting tectonic hazards: Nepal and Italy
  6. Try this

What this dot point is asking

This is AQA GCSE Geography (8035) Paper 1, Section A (3.1.1 The challenge of natural hazards). AQA expects you to define a natural hazard, classify hazard types, explain the factors that affect hazard risk, describe the structure of the Earth and the theory of plate tectonics, distinguish the three plate margins, and use a named example of a tectonic hazard in two contrasting countries to explain primary and secondary effects, immediate and long-term responses, and why people continue to live in hazardous areas.

Types of natural hazard and hazard risk

A natural hazard is a natural event (such as an earthquake, tropical storm or flood) that has the potential to cause loss of life or damage to property. Hazards are usually grouped as tectonic (earthquakes, volcanoes) and atmospheric (storms, drought).

Plate tectonics theory

The Earth has a dense core, a semi-molten mantle, and a thin outer crust broken into tectonic plates. Convection currents in the mantle, driven by heat from the core, drag the plates and make them move. There is thin, dense oceanic crust and thick, less dense continental crust.

The three plate margins

  • Constructive (divergent): plates move apart, magma rises to form new crust and gentle volcanoes (for example the Mid-Atlantic Ridge under Iceland).
  • Destructive (convergent): an oceanic plate is subducted under a continental plate, melting to feed explosive volcanoes and triggering powerful earthquakes.
  • Conservative (transform): plates slide past each other; no crust is made or destroyed, but friction causes strong earthquakes (for example the San Andreas Fault).

Contrasting tectonic hazards: Nepal and Italy

The 2015 Nepal earthquake (magnitude 7.8) struck a lower-income country. Primary effects: about 9,000 deaths and 600,000 buildings destroyed. Secondary effects: avalanches on Everest and landslides blocking roads. Immediate responses relied on international aid; long-term responses included repairing heritage sites to restore tourism.

The 2009 LAquila earthquake in Italy (magnitude 6.3) struck a higher-income country. There were around 300 deaths and 67,000 left homeless, but better building standards, organised search-and-rescue, insurance and a wealthier economy meant recovery was faster. Comparing the two shows that magnitude alone does not decide the impact: the Nepal quake was stronger yet caused far more death and damage largely because of poverty, building quality and remote terrain. This is the core "level of development" point AQA wants in the higher-mark answers.

Why people live in hazardous areas. Despite the risk, people stay in tectonic regions for fertile volcanic soils (the slopes of Mount Etna and Vesuvius are intensively farmed), geothermal energy (Iceland generates much of its electricity and heating from it), tourism (volcanoes and hot springs attract visitors and income), mineral deposits, and simply because it is home, with family, jobs and community ties that are hard to leave. Many also judge that a major event is rare in their lifetime, or trust that monitoring, building codes and planning will protect them.

Try this

Q1. Define the term hazard risk. [2 marks]

  • Cue. The probability or chance that a community will be affected by a natural hazard.

Q2. Explain why earthquakes occur at conservative plate margins. [2 marks]

  • Cue. Plates slide past each other, friction locks them, and the sudden release of built-up pressure causes the earthquake.

Exam-style practice questions

Practice questions written in the style of AQA exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

AQA 20196 marksUsing two contrasting examples, explain why the effects of a tectonic hazard can differ between countries at different levels of development. (Paper 1, Section A)
Show worked answer →

A 6-mark question from Paper 1 Section A (The challenge of natural hazards), assessing AO1 and AO2. Markers reward a clear contrast between a higher-income and a lower-income country with reasons linked to wealth.

Award credit for naming two contrasting events (for example the 2015 Nepal earthquake in an LIC and the 2009 LAquila earthquake in an HIC), then explaining how development shapes effects: in Nepal, poor-quality, non-earthquake-proof buildings collapsed, killing about 9,000, and a weak economy and remote mountain terrain slowed rescue and aid; in Italy, stronger building codes, organised emergency services, insurance and wealth meant far fewer deaths (around 300) and faster recovery. The lift is to explain the link (wealth funds preparation, building standards and response), not just to list deaths. The strongest answers compare like with like (buildings, response, recovery).

AQA 20224 marksExplain why volcanoes and earthquakes occur at destructive plate margins. (Paper 1, Section A)
Show worked answer →

A 4-mark "Explain" question testing AO1 and AO2 on plate tectonics. Markers reward a process chain involving subduction.

Award credit for: at a destructive (convergent) margin the denser oceanic plate is forced down beneath the less dense continental plate (subduction). As it sinks into the mantle it melts to form magma; the magma is less dense and rises through cracks to erupt as explosive volcanoes. Friction as the plates lock and then suddenly jolt past one another releases stored energy as powerful earthquakes. The strongest answers name subduction, the density difference and the build-up and release of pressure. Simply saying "the plates crash together" caps the marks.

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