Hazards Flashcards

1
Q

Hazard

A

-a potential threat to human life and property caused by an event
-Hazards should not be confused with natural disasters. A
disaster will only occur when a vulnerable population is exposed to
a hazard.

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2
Q

three types of hazard

A

-geophysical (caused by tectonic plates eg volcanos)
-atmospheric (caused by conditions caused by atmospheric processes eg wildfires)
-hydrological (caused by water bodies eg floods)

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3
Q

Factors that effect hazard perception

A

wealth: Wealthier people may perceive hazards to be smaller as they are less vulnerable. wealthier people may also
view a risk as greater as there is more risk of property damage and financial loss

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 have been in the past.

Religion: Some may view hazards as put there by God for a reason, or being part of
the natural cycle of life etc. so may not perceive them to be negative

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4
Q

Human responses to hazards

A

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.

Fear: panic and fleeing

Adaptation: Attempting to live with hazards by adjusting lifestyle choices

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5
Q

Example where risk sharing has worked

A

New Zealand:
-under threat from earthquakes, tsunamis, volcanoes
-huge cost
-now attempts to share the risk by insurance investment, so
strategies can be put in place before the disasters rather than investing more in a clean up.

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6
Q

Aspects of Hazards and How They Affect Human Responses

A

Incidence:
-harder to predict and have less management in place
- frequent hazards tent to be low intensity

Distribution:
-Areas of high hazard distribution have more management strategies, those living
there will be more adapted

Intensity:
-high intensity hazards will have worse effects, meaning they will require more
management

Level of development:
-will affect how a place can respond to a hazard

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7
Q

The park model

A

-a graphical representation of human responses to hazards
-shows the steps carried out in the recovery after a hazard
-The steepness of the curve shows how quickly an area deteriorates and recovers
- The depth of the curve shows the scale of the disaster (i.e. lower the curve, lower the
quality of life).

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8
Q

Park model stages

A

Stage 1: Relief
-immediate local response
-request for foreign aid

Stage 2: Rehabilitation
-Services begin to be
restored
-Temporary shelters
and hospitals set up
-foreign aid

Stage 3: Reconstruction
-Infrastructure rebuilt
-Mitigation efforts for
future event

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9
Q

The hazard management cycle

A

outlines the stages of responding to events, showing how the same stages take place after every hazard.

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10
Q

4 stages of the hazard management cycle

A

-Preparedness
-Response
-Recovery
-Mitigation

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11
Q

Evaluating the Effectiveness of Models

A

-Can they 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?
- Could the model be less vague/ include more steps that can be applied to all hazards?

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12
Q

Structure of the earth

A

-Inner core
-outer core
-mantle
-asthenosphere
-lithosphere
-crust

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13
Q

inner core

A

-Solid ball of iron/nickel
-Very hot due to pressure and
radioactive decay
-This heat is responsible for
Earth’s internal energy

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14
Q

Outer core

A

-Semi-molten
-Iron/nickel

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15
Q

Mantle

A

-Mainly solid rock
-the very top layer of
the mantle is semi-molten
magma, which is known as the
asthenosphere
-The lithosphere rests on top.

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16
Q

Asthenosphere

A

-Semi-molten layer constantly
moves due to flows of heat
called convection currents.
-Movements are powered by
heat from core.
-Lithosphere above

17
Q

Lithosphere

A

-Broken up into plates.
-The top of the lithosphere is
the crust which is the land
and sea we live on.

18
Q

Crust

A

-The thin top of the lithosphere
-Oceanic crust is dense and is destroyed by plate movement
-continental crust is less dense
and is not destroyed.

19
Q
A
20
Q

Convection currents

A

-are caused when the less dense magma rises, cools, then sinks.
-The edges of where plates meet are called plate boundaries

21
Q

Destructive plate boundaries

A