Seismic Hazards (earthquakes) Flashcards
Where are earthquakes found and why?
They are found along the plate boundaries. This is because, when these boundaries slide past or subduct into one another, pressure is built up and then suddenly released. This triggers movement which results in an earthquake. They are found mainly at destructive plate margins as pressure is larger
What is seismicity?
Earth shaking, which can be human induced (e.g. via reservoir construction, fracking or mining)
What are the steps of seismic waves?
1) pressure builds up at the point where two plates meet
2) sudden release due to rock failure creates waves
3) the waves cause the ground to shake
4) the intensity of the shaking is dictated by the depth of the focus and the energy release
RESULTING IN AN EARTHQUAKE
What are P waves (primary)?
- short pulse of energy moving forwards and backwards very quickly
- they will be picked up first by seismometers
- least damaging as they just vibrate
What are S waves (secondary)?
- go up and down
- slower than p waves
- more damaging (travel like a Mexican wave)
What are Rayleigh waves?
- they are much slower
- compression up and down again
- more damaging to buildings
What is a love wave?
-most damaging
- have a side to side movement
- challenge to people/buildings
- relatively slow
What are tsunamis?
- Large volume of water that pushes in land over time (release of energy under the sea)
- They travel across the open ocean at high speeds
- They are generated in subduction zones. Friction between plates, they get “stuck”
- Stuck plates continue to descend down into the mantle- slow distorting of overriding plate.
- Energy can accumulate in the overriding plate until it exceeds the frictional forces between the stuck plates, overriding plate snaps back and the sudden movement causes a tsunami- overlying water travels inland
- moving wave begins travelling out from where the earthquake has occurred.
- ‘wave trains’, multiple waves not just one
What is liquefaction?
The mixing of sand or soil and groundwater during the shaking of an earthquake. When the water and soil mix, the ground becomes very soft (like quicksand). If liquefaction occurs under a building, it may start to lean or even sink. The ground firms up again after after the earthquake has passed and the water settles back down to underground.
What are landslides?
Where the ground shakes due to earthquakes destablises cliffs and steep slopes, causing landslides and rock fall. Heavy rain or fractured rock and exacerbating factors. Relief rainfall in these upland areas means the ground is significantly more likely to become saturated and therefore more likely to fail
What physical characteristics make areas susceptible to landslides?
Steep land
Land sat over unstable plate boundaries
Heavy air before an earthquake
At least a 10% land gradient
What physical characteristics make an area susceptible to liquefaction?
Land near to water, soil and sand
Worse if there is sand as water can move around the particles of sand
Why is liquefaction worse than an earthquake?
There’s not much you can do to adapt/mitigate liquefraction
How can monitoring past seismic events predict future earthquakes?
The seismic gap theory:
Theory that earthquakes can be predicted by observing the time gap between past earthquakes in an area. The average time between past earthquakes and time since the last one can be used together to predict when the next one will be
How can remote sensing be used to predict earthquakes?
Attempted to detect thermal activity. Also, attempts to relate ionosphere disturbances associated with earthquakes. They use satellites to see whether plates are moving apart or if there not then they are stuck (earthquake may occur)