Natural hazards and disasters
- Created by: ambercadman
- Created on: 17-10-16 17:54
Hot spots
Radioactive material causes magma to rise
Melts plate above causes volcanoes to form
Plate moves over the hot spot
Causes chain of volcanoes to form
Intra plate earthquakes
Caused by stresses within plate
Plate stretched over spherical surface
Weaknesses are caused
Earthquakes happen along zones of weakness or ancient boundaries
Evidence for plate techtonics
Ortelius - suggested they look the fit like puzzle
Wegner - once joined in a super continent called Pangea, had drifted apart over time
Harry Hess - suggested convection currents, recycling of plates
Evidence
Split fossil remains (India and Australia)
Rocks found in Scotland and new found land
Mountain range cut in half between Brazil and Africa
Glacial deposits found in hot countries suggesting they were once in cold regions
Paleomagnetism and Wilson cycle
Paleomagnetism
Occurs at constructive plate boundaries
Alternate bands of magnetic material (found in basalt)
Shows how new layers are produced by Earth
Shows magnetic field changes
Wilson cycle
See folder for diagrams
Hot spot causes to split in two
Causes the plates to travel further apart
Closes when newly formed oceanic plate sinks under continental
Continental ends up traveling towards previous continental
Eventually the continental plates collide
Causes a collision boundary = mountains
Magma types and how it effects their eruptions
Basalt
Hot, thin, low silica, high iron
Easy for gas to escape so a peaceful constant eruption
Rhyolite
Cool, thick, high silica and low in iron
Hard for gas to escape so an irregular eruption
Andesite is in the middle of the above
So intermediate eruption and gas escape
Tsunamis
Destructive boundary formed
Pressure builds up
Continental flicks up displacing water causing it to bulge higher then usual
Gravity pulls it down causes the wave to split and travel in separate directions
Wave is nearly undetectably
Travels at 500mph
Draws closer to shore the topography is shallower
This causes the front of the wave to slow down while the back is still moving faster
Results in a wall of water known as a tsunami
Earthquake waves
Body waves- travel through inner layers
Surface waves- along surface like ripples on water
Order
Body waves and the surface waves which are the ones that cause the most damage
P waves
Longitude waves, same direction of travel
S waves
Arrive second, transverse waves. Look wavy side on
L waves
fastest wave that moves ground from side to side, confined to surface of crust, horizontal motion so looks wavy from birds eye view
Benidorm zone
Energy generated in shallow events is released closer to the surface and therefore produce stronger waves on the surface
Green = most dangerous
Yellow = bit less dangerous
Red = least dangerous
Hazards into disasters
Natural hazard - a perceived natural event which has the potential to threaten life and property
Can either be:
Geophysical (tectonic)
Hydrometerological (weather)
Risk equation
Risk=magnitude x vulnerability/ capacity to cope
Disaster resilience
Ability of individuals, communities, organisations and states to adapt to and recover from hazards, shocks and stresses without compromising long term prospects for development
Degree in which countries can learn from past experiences/ disasters and reduce risk for future events
Key terms for hazards and disasters
Mega disaster- unexpected natural disaster of exceptional magnitude or caused severe damage
Socio-economic - study of social and economic factors to understand how the combination of them influences something
Spatial predictably- using patterns and areas past hazards have occurred to predict future events
Dynamic pressures - things that effect how vulnerable a community is e.g rapid migration, social structure, local markets and macro forces
Liquefaction - process of loose soil actions like a liquid
Dregg's model
Venn diagram
Vulnerability on one side. Hazard on the other side.
Overlap represents the disaster
Therefore when a hazard comes in contact with a vulnerable population = disaster
Pressure and releases model (PAR)
Weighing up the vulnerability and the hazard against each other to discover what made the hazard a disaster
Vulnerability side
Root causes
Political and economic systems e.g debt or political instability
Dynamic pressures
Local systems
Organisations
Population
Unsafe conditions
The conditions resulting from the two previous e.g poorly built buildings resulting from lack of building codes and large population
Hazards
Information about the hazard e.g magnitude, severity, impacts e.g deaths
Main factors that determine vulnerability
Poverty- illegal housing - dangerous areas
Poverty- slums- poorly built- homeless after
Currpted government- lack of preparation, education systems, disaster management- unable to bounce back and responses were slow
Wealth- can't pass building codes- portly built houses- unsafe conditions
Support from aid- if already getting support- will need more after- too reliant- can't rebuild
Hazard profiles
A diagram that shows the main characteristics at different types of tectonic hazards or multiple hazards to allow for easy comparison
(Place dots between scale) e.g speed of onset, rapid - slow
Characterises which make the hazard worst on one side
Then connect the dots to create a zig zag
These can be compared
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