Natural hazards: definitions, types and risk factors
A natural hazard is a natural process or event with the potential to cause loss of life, injury or property damage. The same event in an unpopulated area is just a natural process — it only becomes a hazard when it threatens people. When a hazard actually occurs and causes serious damage, it becomes a natural disaster.
The three families of natural hazards
Examiners expect you to distinguish three categories:
- Tectonic hazards — driven by plate movement: earthquakes, volcanic eruptions, tsunamis.
- Atmospheric (weather/climatic) hazards — driven by the atmosphere: tropical storms, droughts, extreme cold, floods caused by rainfall.
- Geomorphological hazards — driven by surface processes: landslides, mass movement (often a secondary hazard triggered by an earthquake or heavy rain).
Some events sit across categories. A volcanic eruption (tectonic) can trigger a lahar (geomorphological) and ash clouds that disrupt aviation (atmospheric impact). Always identify the primary trigger.
Hazard risk
Hazard risk = the probability that people will be harmed by a natural hazard. Risk is not just about the hazard itself; it depends on exposure and vulnerability. The standard formula examiners reward is:
Risk = (frequency or magnitude of hazard) × (vulnerability of population) ÷ (capacity to cope)
Factors that increase hazard risk
- Urbanisation. Megacities concentrate millions of people in a small area. When Mexico City (in a tectonic zone) or Dhaka (on a low-lying flood-prone delta) experience a hazard, the population at risk is enormous.
- Poverty. Lower-income people often live in the most hazardous areas (steep slopes, floodplains, marginal land) because cheaper land is unsafe land. Their housing is less hazard-resistant. After the 2010 Haiti earthquake, weak concrete-block houses collapsed catastrophically; richer neighbourhoods with reinforced construction fared better.
- Climate change. A warmer atmosphere holds more moisture, intensifying tropical storms; sea-level rise enlarges storm-surge zones; extreme heat events (UK 2022 reaching 40 °C) become more frequent.
- Farming on marginal land. Drought-prone regions of the Sahel are farmed because better land has been claimed; failed harvests turn drought into famine.
- Plate margins and active volcanoes. Living in Tokyo, Naples or Reykjavík puts millions of people next to known tectonic risks.
Factors that decrease hazard risk
- Wealth. HICs invest in monitoring (seismometers, satellite weather), early-warning systems, building codes, evacuation infrastructure and insurance.
- Education and preparedness. Japanese schoolchildren rehearse earthquake drills monthly; Bangladesh trained 70 000 cyclone volunteers after the 1970 Bhola disaster killed an estimated 500 000.
- Effective governance. Strong planning law, enforced building codes, organised emergency services and political stability all reduce vulnerability.
Examiner tips
- Always link your answer back to people. A 7.0 magnitude earthquake in remote Antarctica is a process, not a hazard.
- Use the trio physical / social / economic to structure answers about why one country suffers more than another.
- When asked about "factors that increase risk", give both a physical factor (e.g. proximity to a plate boundary) and a human factor (e.g. poverty, urbanisation). Most marks reward this combination.
- Climate change is examinable as a risk multiplier — it doesn't usually create hazards but it does intensify existing ones.
➜Try this— Quick check
Why might two earthquakes of the same magnitude (say M7.0) cause very different death tolls in two countries? Because the earthquake itself is the hazard, but the risk depends on the people exposed (urban density), their vulnerability (poverty, building quality, age structure) and their capacity to cope (governance, wealth, preparedness). The 2010 M7.0 Haiti earthquake killed over 100 000; the 2010 M7.0 Christchurch earthquake (NZ) killed nobody initially.
AI-generated · claude-opus-4-7 · v3-deep-geography