Hazards Flashcards
what is a natural hazard
an event that poses a threat to human life, the built environment and the natural environment
what are the 3 main types of hazards
geophysical - caused by earth processes
hydrological - caused by the occurance, movement and distribution of surface and ground water
atmospheric - caused by processes operating in the atmosphere
how does the UN define a disaster
• 10+ people are killed
• 100+ people are affected
• a state of emergency is declared
• International assistance is called for
why do people stay in hazard risk zones?
-hazard events are unpredictable
-lack of alternatives
-changing level of risk
-cost/benefit
-perception
how is risk measured?
r = h x v
c
r = risk
v = vulnerability
c = capacity to cope
what is hazard perception
the way in which a person understands or interprets a hazard. People tend to respond to hazards based on their perception
what is the fatalism approach to hazards
an optimistic or accepting approach, where people may believe that hazards are a fact of life or ‘acts of god’
what is the domination approach to hazards
hazards are predictable and can be better understood by scientific research
what is the adaptation approach to hazards
hazards are influenced by natural and human events and so we can change our lives to reduce the impacts
what is a primary hazard?
a hazard directly related to the event
eg, lava flows are directly related to a volcanic eruption
what is a secondary hazard?
a hazard that occurs due to a primary hazard
eg, a lahar is indirectly related to a volcanic eruption
what is a short term response?
occur in the days and weeks immediately after a disaster
mainly search and rescue and helping the injured
what is a long term response?
responses that go on for months and years after a disaster
involves rebuilding and taking steps to boost the local economy
what is vuberability?
the diminished capacity of an individual or group to anticipate, cope with, resist and recover from the impacts of a hazard
can relate to exposure to hazards, political instability, poverty, etc
what factors influence perception?
-education
-wealth
-religion, culture or ethnic background
-vunerability
-age
-previous experience of hazards
-family and marital status
-occupation/ employment status
-values, personality and expectations
what is a disaster?
a major hazard event that causes widespread destruction to a community or region, with significant social, economic and environmental losses
the affected community is unable to cope without outside help
what is resilience?
the sustained ability of a community to utilise available resources to respond too, withstand and reviver from the effects of natural hazards
what does integrated risk management do?
-identify the hazard
-analyse the risk
-establish priorities
-treat the risk
-implement a risk reduction plan
-develop public awareness and community strategy
-monitor and review the whole process
what are the ‘4 Ps’ of hazard management?
Prediction
Preparation
Protection
Prevention (not always possible)
why is the hazard management cycle useful?
-simplify complex events
-useful when responding to hazards with severe time constraints
-comparing actual conditions with a model leads to better understanding, so better response
-help people understand the hazards
-allow better integration of relief and recovery
what are the limitations of the hazard management cycle?
-responses are often more complex, and not always logical
-timescale is not accounted for, the model suggests equal time for each phase
-does not consider environmental conditions that might affect severity of the hazard
-all hazards are different and the model does not account for this
-evaluation and analysis of hazards are important in order to prepare for future hazards
-some countries do not have the means to mitigate effectively
-does not consider international aid
why is the park model useful?
-tool to analyse the different types of response and the sequence in which they happen
-useful for pinpointing the different kinds of response needed at different stages of a disaster
what are the limitations of the park model?
-does not take varying capacity to cope into account, and different places will take longer to reach different points of relief, rehabilitation and reconstruction
-far too general and not specific enough about impacts, frequencies, and how these affect the capacity to respond
-a model is an ideal to compare and critique, never a perfect fit
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describe the motion of constructive plate bounderies
plates move away from eachother in opposite direction, causing magma from the mantle to rise to the surface, forming new crust
what are the geological features associated with constructive plate bounderies?
-mid ocean ridges
-rift valleys
-gentle, effusive volcanoes with low viscosity basaltic lava
-volcanic islands
how are mid-ocean ridges formed?
-constructive plate boundery
-magma rises from the mantle forming new crust
-forms chains of submarine mountain ridges
-regular breaks called transform faults cut across ridges
-these faults may widen at different rates, causing frictional stresses to build up
-this tension is released by shallow focus earthquakes
how are rift valleys formed?
-constructive plate bounderies
-formed when the lithosphere stretches
-causing it to fracture into sets of parallel faults
-the land between these faults then collapses into deep, wide valleys separated by upright blocks of land called hosts
how are volcanic islands formed? (constructive plate bounderies)
-volcanic eruptions along mid-ocean ridges can build submarine volcanoes
-over time these may rise above sea level to create volcanic islands
-eg, Ascension Island
describe the motion at destructive plate bounderies
one plate moves toward another, or two plates move towards eachother
what happens at a destructive plate boundery between an oceanic plate and a continental plate?
the heavier oceanic plate is subducted
this causes the continental plate to ‘scrunch’ and form fold mountains
the exact point of collision is marked by bending of the oceanic plate to form a deep sea trench
the descending oceanic plate starts to melt beyond 100km deep and melts completely by 700km deep thud zone of melting is known as the Benioff Zone
the melting crust creates magma less dense than the surrounding asthenosphere, which rises in plumes, passing through faults in the buckled continental plate to form explosive volcanic eruptions of viscous andersitic lava
friction causes tension that builds up and is released as intermediate or deep focus earthquakes
what happens at a destructive plate boundery between two oceanic plates?
-the denser or slower moving plate is subducted under the other
-forms a deep sea trench
-rising lava from the benioff zone forms crescents of submarine volcanos which may form volcanic island arcs (eg. Mariana Trench and Marianas Islands)
what happens at a destructive plate boundery between two continental plates?
-no subduction as they are both less dense than the asthenosphere
-colliding plates uplift, compress and buckle to form fold mountains (eg, Hymalayas)
-no subduction, so no volcanoes
-shallow focus earthquakes
-young fold mountains are continously compressing and growing taller
describe the motion at conservative plate bounderies
two plates slide past eachother, causing friction