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Natural Hazards Simplified Revision Notes

Revision notes with simplified explanations to understand Natural Hazards quickly and effectively.

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1.1.1 Natural Hazards

What is a Natural Hazard?

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An event becomes a hazard when it affects people.

  1. A natural hazard is a natural process which could cause death, injury, or disruption to humans, or destroy property and possessions.
  2. A natural disaster is an event that has actually happened.

What are the Main Types of Hazards?

  • Geological Hazards:
    • Caused by land and tectonic processes.
    • Examples: volcanoes, earthquakes, landslides.
  • Meteorological Hazards:
    • Caused by weather and climate.
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Examples: tropical storms, flooding due to extreme weather.

What Affects a Country's Ability to Cope?

  • Vulnerability:
    1. The more people in areas exposed to natural hazards, the greater the probability they will be affected.
    2. Example: People living at the base of a volcano in Naples, Italy are vulnerable to eruptions.
  • Capacity to Cope: 3. Natural hazards have to affect human activities to count as a hazard. The better a population can cope with an extreme event, the lower the threat. 4. Example: High-Income Countries (HICs) are better able to cope with earthquakes as they can build earthquake-proof buildings and repair damage afterwards.

Hazard Risk

Techtonic Hazards

Techtonic Hazards

  • The probability that a natural hazard occurs.
  • Three main factors affecting risk: 5. Type: The hazard risk from some hazards is greater than others (e.g., tropical storms can be predicted but earthquakes can't). 6. Frequency: Some natural disasters occur more often than others (e.g., flooding). 7. Magnitude: More severe natural hazards cause greater effects than less severe events (e.g., a magnitude 5 earthquake compared to a magnitude 8).

Tectonic Plates

  1. Structure:
  • The inner core is solid and outer liquid.
  • Around the core is the mantle - semi-molten rock moving slowly.
  • The outer layer is the crust, divided into slabs called tectonic plates.
  1. Types of Plates:
  • Plates can be continental or oceanic.
  • The meeting point is called a plate boundary/margin.
  1. Movement:
  • Plates move due to convection currents in the mantle.
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