PMT Hazards

    Cards (127)

    • Hazard
      A potential threat to human life and property caused by an event
    • Hazards can be human caused or occur naturally (natural hazards)
    • An event will only become a hazard when it is a threat to people
    • Natural disaster
      An event that occurs when a vulnerable population is exposed to a hazard
    • Major types of geographical hazard
      • Geophysical
      • Atmospheric
      • Hydrological
    • Hazards can also be a mixture of these geographical processes
    • Hydrometeorological hazards

      Hazards that are both atmospheric and hydrological
    • Hazard perception
      People's viewpoints of how dangerous hazards are and what risk they pose
    • Lifestyle factors
      Economic and cultural elements that affect people's hazard perceptions
    • Wealth
      The financial situation of a person that affects how they perceive hazards
    • Experience
      Someone who has experienced more hazards may be more likely to understand the full effects of a hazard
    • Education
      A person who is more educated about hazards may understand their full effects on people and how devastating they can be
    • Religion and beliefs
      Some may view hazards as put there by God for a reason, or being part of the natural cycle of life
    • Mobility
      Those who have limited access to escape a hazard may perceive hazards to be greater threats than they are
    • Fatalism
      The viewpoint that hazards are uncontrollable natural events, and any losses should be accepted as there is nothing that can be done to stop them
    • Active responses to hazards
      1. Prediction
      2. Adaptation
      3. Mitigation
      4. Management
      5. Risk sharing
    • New Zealand is an example of where risk sharing has worked
    • Incidence
      Frequency of a hazard
    • Distribution
      Where hazards occur geographically
    • Intensity
      The power of a hazard, i.e. how strong it is and how damaging the effects are
    • Magnitude
      The size of the hazard, usually this is how a hazard's intensity is measured
    • Magnitude and intensity are not interchangeable terms
    • Level of development
      Economic development will affect how a place can respond to a hazard
    • Even if the hazard is identical, an area with a lower level of development is less likely to have effective mitigation strategies as these are costly
    • There are many high income countries that are not as prepared for natural hazards as they should be, meaning they lack the management strategies for an event
    • The Park Model
      A graphical representation of human responses to hazards, showing the steps carried out in the recovery after a hazard
    • The Hazard Management Cycle
      Outlines the stages of responding to events, showing how the same stages take place after every hazard
    • Stage 3 - Reconstruction
      1. Restoring the area to the same or better quality of life
      2. Area back to normal - ecosystem restored, crops regrown
      3. Infrastructure rebuilt
      4. Mitigation efforts for future event
    • Control line
      A model to compare hazards
    • An extremely catastrophic hazard

      Would have a steeper curve than the average and would have a slower recovery time than the average
    • The Hazard Management Cycle
      1. Preparedness
      2. Response
      3. Recovery
      4. Mitigation
    • Hazard models
      • The unpredictability of hazards makes the models less effective at accurately representing human responses to hazards
    • Can hazard models be applied to every hazard? Are some hazards more complicated and require a more complex model?
    • Does the model take any aspects of hazards into account such as level of development?
    • Inner core
      Solid ball of iron/nickel, very hot due to pressure and radioactive decay
    • Outer core
      Semi-molten, iron/nickel
    • Mantle
      Mainly solid rock, high in silicon, top layer is semi-molten magma (asthenosphere)
    • Asthenosphere
      Semi-molten layer constantly moves due to convection currents
    • Lithosphere
      Broken up into plates, majority within mantle, top is the crust
    • Crust
      The thin top of the lithosphere, oceanic crust is dense and destroyed by plate movement, continental crust is less dense and not destroyed
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