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Tectonics
1.3 Explaining tectonic hazards
1.3A Hazards caused by earthquakes
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Earthquakes
= sudden release of stored energy underground
Types of waves:
P-waves
S-waves
L-waves
P-wave
:
primary wave
fastest wave
deal the least damage
vibrations caused by compressions - material movement is the same way as the wave
S-wave
:
secondary waves (arrive second)
only travel through solids
shear waves - move material perpendicular to the wave movement
L-waves
:
arrive last as they travel only on the surface
large amplitude and cause significant damage to buildings, include fracturing the ground surface
Crustal
fracturing
= Earthquakes cause crustal fracturing within the Earth, but also buckle and fracture the ground surface
-> 2004 Indian Ocean tsunami, rupture a fault line for up to 1000km.
Secondary hazards:
liquefaction
landslides
Liquefaction
= when the shaking causes particles in the ground to move further apart causing them to act like a liquid rather than a solid
landslides
= the movement of material down a slope due to vibrations of the earths surface