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Seismic hazards - Coggle Diagram
Seismic hazards
Prediction, protection, mitigation, preparedness
Prediction
micro quakes, curious animal behaviour, decreasing radon gas in groundwater, raised groundwater levels
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Earthquakes are the primary hazard of seismic activity however there are also other hazards including tsunamis, Landslides and avalanches and soil liquefaction
Tsunamis
Tsunamis are large waves caused by the displacement of water, generated by an ocean floor earthquake or a volcanic eruption underwater
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Soil liquefaction
This occurs if the soil is saturated with water it can act like a liquid meaning it is easier to deform and subside especially if it has weight on top e.g. a building
avalanches/landslides
shaking of the ground can dislodge, rock, soil or snow which can trigger landslides or avalanches, the shaking also creates gaps in the soil which water can fill and the extra weight can create more landslides
Seismic shockwaves
primary or pressure waves are the first to reach the surface, they travel like sound waves and are high frequency
Secondary or shear waves are half as fast and reach the surface after primary waves, they are high frequency but shake like a skipping rope
surface love waves are the slowest and cause the most damage and Rayleigh waves radiates from the epicenter in low frequency rolling motions
Causes of Seismicity
Human activities such as fracking or mining can cause seismic activity however the most powerful seismic activity is associated with plate movement as it creates energy of extraordinary proportions
friction along plates occurs in the lithosphere due to convection currents in the asthenosphere continually pushing plates
the breaking point is called the focus and the epicentre is the area on the surface directly above the focus point
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