Can have economic , social and environmental consequences . For each hazard event the risks of a particular consequence happening can vary greatly
Plate Tectonics Theory
Slab pull occurs where denser tectonic plates sink into the mantle at subductionzones . As these sections of plates sink , newer and less dense sections of plate are pulled along behind . Sinking in one place leads to plates moving apart in other places .
Conservative Plate Boundary
Plates move next to each other ( at different speeds ) or different directions
---> As they move next to each otherfrictionbuilds plates then become stuck . Pressure builds up because the plates are still trying to move . When the pressure is released, it sends out huge amounts of energy , causing an earthquake
Constructive Plate Boundary
Two platesmoveaway from each other due to convectioncurrents
--> movement creates friction of rock over the mantle = earthquake
As a gap is created in-between the plates , magma from the mantle rises up to make a shield volcano
Destructive Plate Boundary
Plates move towards each other due to convection currents . Oceanic plate is more dense and sinks below continental in subduction - convection currents pull plates down through slabpull
---> If two continental plates collide it creates a collision margin due to a build up of friction pressure . Earthquakes occur
Oceanic plate melts as it sinks into the mantle , forming magma . It escapes through weaknesses in the rock and rises through volcano causing an eruption
Destructive Plate Boundary
Constructive Plate Boundary
Conservative Plate Boundary
Haiti Earthquake ( 12th Jan 2010 )- LIC

PRIMARY IMPACTS
Over 220000 deaths
30000offices destroyed
300000 people injured
SECONDARY IMPACTS
1.3mil made homeless
Increase of cholera , 9000 died
1 in 5 jobs lost
Haiti Earthquake Responses
SHORT TERM RESPONSES
DominicanRepublic donated water and medical supplies
Red cross set up temporary field hospitals
UN troops and police were sent to help distribute aid
LONG TERM RESPONSES
EU gave $330mil , International aid $3.5bil to rebuild
Senegal offered education - 163 went
Red cross received $500mil - promised 700 homes yet only built 6
Tohoku Earthquake ( March112011 ) -HIC

PRIMARY IMPACTS
332000 buildings destroyed
11hospitals destroyed - 300+ damaged
800 after shocks of 4.5 magnitude
SECONDARY IMPACTS
$235bil cost of damage
Tourism fell 62%
300000 people displaced
Tohoku Earthquake Responses
SHORT-TERM RESPONSES
100000 Japan Self defense were sent to help in search & rescue
140000 residents evacuated near Fukushima
PacificTsunamiwarningcenter able to detect seismicwaves and immediately sent warning to Japan
LONG-TERM RESPONSES
Japan's redcross $16bil in donations
GAP donated $1.1mil winter clothes
$70mil spent on lasers to monitor the slightestmovement
Why people live in areas at risk from a tectonic hazard?
Fertile soil - jobs w growing crops
Cheaper housing and resources
Friends and family live there
Monitoring Risks of a Tectonic Hazard
Earthquakes - seismometers and lasers monitor each movement
Volcanoes - their shape , escaping gas , tiny earthquakes
Predicting the Risks of Tectonic Hazards
Volcanoes - if scientists monitor volcanoes closely
Earthquakes - unreliable but possible if monitored ( tectonic plates )
Protection from the Risks of Tectonic Hazards
Volcanoes - buildings are strengthened and barriers to divert lava away
Earthquakes - buildings strengthened and shut off switches for gas so no fire