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