Earthquakes and the earth's interior Flashcards
Stress
is the force or load on an object
Strain
is the response to that load
- deformation i.e elongation, compression or distortion
Earthquake rupture 0 seconds
rupture expands circularly on fault plane, sending out seismic waves in all directions
Earthquake rupture 5 seconds
rupture continues to expand as a crack along the fault place. when rupture front reaches the surface, displacements occur along the fault trace and rocks at the surface begin to rebound from their deformed state
Earthquake rupture 10 seconds
rupture front progresses down the fault plane, reducing the stress and allowing rocks on either side to rebound. seismic waves continues to be emitted in all directions as the fault propagates
Earthquake rupture 20 seconds
rupture has progressed along the entire length of the fault. the fault has reached its maximum displacement and the earthquake stops
Normal faults (constructive)
tension forces as plates move apart, one side drops down relative to another, formation of waterfall, river catchment disruptions
Thrust faults (destructive)
Compression fault (Reverse fault) shortening of the crust, sediments are piled up on each other, rocks rises up
Strike-slip fault (conservative)
Shearing forces, loch ness lake along these faults, one plate sliding past the other
Focus
where the earthquake begins (immediate stress)
Epicentre
point on earths surface directly above focus
P waves (primary)
- compressional waves, can move through solid and liquid, fastest waves
- wave energy moving thorough, squashing and stretching blocks
- push the earth
S waves (secondary)
- shear waves, cannot move through liquid, slower waves
- wave shadow zone (105o), evidence for liquid outer core
- shake the ground
Body waves
move through structure of the earth, greater than magnitude 5 then the waves travel through earth (big enough o travel trough globe)
Rayleigh waves
up and down motion, cause buildings to break and collapse