Earthquakes and the earth's interior Flashcards

1
Q

Stress

A

is the force or load on an object

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2
Q

Strain

A

is the response to that load

- deformation i.e elongation, compression or distortion

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3
Q

Earthquake rupture 0 seconds

A

rupture expands circularly on fault plane, sending out seismic waves in all directions

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4
Q

Earthquake rupture 5 seconds

A

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

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5
Q

Earthquake rupture 10 seconds

A

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

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6
Q

Earthquake rupture 20 seconds

A

rupture has progressed along the entire length of the fault. the fault has reached its maximum displacement and the earthquake stops

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7
Q

Normal faults (constructive)

A

tension forces as plates move apart, one side drops down relative to another, formation of waterfall, river catchment disruptions

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8
Q

Thrust faults (destructive)

A

Compression fault (Reverse fault) shortening of the crust, sediments are piled up on each other, rocks rises up

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9
Q

Strike-slip fault (conservative)

A

Shearing forces, loch ness lake along these faults, one plate sliding past the other

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10
Q

Focus

A

where the earthquake begins (immediate stress)

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11
Q

Epicentre

A

point on earths surface directly above focus

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12
Q

P waves (primary)

A
  • compressional waves, can move through solid and liquid, fastest waves
  • wave energy moving thorough, squashing and stretching blocks
  • push the earth
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13
Q

S waves (secondary)

A
  • shear waves, cannot move through liquid, slower waves
  • wave shadow zone (105o), evidence for liquid outer core
  • shake the ground
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14
Q

Body waves

A

move through structure of the earth, greater than magnitude 5 then the waves travel through earth (big enough o travel trough globe)

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15
Q

Rayleigh waves

A

up and down motion, cause buildings to break and collapse

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16
Q

love waves

A

more of a lateral movement, side to side, cause water bridges to collapse (topple over)

17
Q

Seismographs

A

designed to detect horizontal movement

18
Q

Refraction

A

waves change their direction depending on relative velocity: the bend into the higher velocity material

19
Q

Mercalli scale

A

measures destruction of earthquake, no damage to total obliteration

20
Q

wave movement through/on earth

A

seismic wave bounce off (reflect) or bend (refract) at discontinuities reflecting major changes in rock properties such as rock density

21
Q

Summary

A
  • waves can travel directly through the earth, or be refracted, reflected or attenuated
  • changes in wave velocity through the mantle generally indicate increasing density with depth (other variations indicate convection in mantle)