how do earthquakes occur
how is the magnitude of earthquakes are measured
how is the energy released by an earthquake measured
how are the impacts of earthquakes measured
how do earthquakes cause tsunamis
-travel up to 940km/hr
-25-40km in height
long wavelength,
-10 to 60mins between each wave
2011 Tohoku
how do earthquakes cause landslides/avalanches
how do earthquakes cause soil liquefaction
what effects the nature and magnitude of an earthquake
-margin type:
destructive margins: biggest earthquakes occur here as the subduction zone causes pressure to build up.
constructive margins: lower magnitude earthquakes
-depth of focus:
the focus can be close to the earths centre or deep below it.
deeper focuses have higher magnitude but they do less damage as they have to travel further which reduces power.
what is the importance of the magnitude and frequency of earthquakes
what is the regularity of earthquakes
-seismic hazards occur randomly
predictability of earthquakes
short term responses to seismic hazards
rescue and evacuation
seismic hazards case study
date
plate margin
Japan Tohoku earthquake
March 2011
destructive pacific and Eurasian plate
5 social impacts of the Tohoku earthquake
2 economic impacts of the Tohoku earthquake
- livelihoods destroyed and so money isn’t put into the economy
3 environmental impacts of the Tohoku
earthquake
4 immediate responses to the Tohoku earthquake
4 long term responses to the Tohoku earthquake
how vulnerable was Japan to the 2011 Tohoku earthquake
6 reasons
Japan after the earthquake - 2
- 2529 people still missing
long term response and risk management: prevention
long term response and risk management: preparedness
long term response and risk management: mitigation
long term response and risk management: adaption