Introduction to seismicity - earthquakes Flashcards

1
Q

What is elastic rebound theory (Henry Fielding)?

A
  1. Before an earthquake, the build up of stress in the rocks, either side of a fault causes gradual deformation (high pressure).
  2. The deformation exceeds the frictional force holding the rocks together, this causes a slip occur along the fault.
  3. Stress is released and the rocks return to their original shape, but are offset
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2
Q

Describe how a normal fault is formed.

A
  1. The hanging wall moves downwards (angle) compared to the footwall
  2. the 2 blocks of rock diverge
  3. A fault scarp is formed when pieces of rock are exposed at the surface.
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3
Q

Describe how a reverse fault is formed.

A
  1. The two blocks or rock are pushed together by compressional forces
  2. The hanging wall is forced upwards compared to the footwall
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4
Q

Describe how a strike-slip fault is formed.

A
  • One block of rock slides laterally past the other, these occur at conservative plate boundaries.
  • NO upwards movement
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5
Q

How are earthquakes formed?

A
  1. As tectonic plates move past each other, they can get stuck and friction can build up between them.
  2. This causes pressure to also build up and eventually this becomes so great that friction is overcome.
  3. This pressure is released at a critical point as the plates snap past each other.
  4. Forming an earthquake and seismic waves (released from focus/benioff zone)
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6
Q

How do P waves move ?

A

As longitudinal waves through the compression and expansion of the crust surface.

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7
Q

Describe some characteristics of P waves.

A
  • Travel through solids and liquids
  • Exist as body waves
  • Travel faster than S waves
  • Felt as a thump
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8
Q

How do S waves move?

A

As transverse waves through the vertical, upwards and downwards motion of the crust.

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9
Q

Describe some characteristics of S waves.

A
  • Travel more slowly than primary waves
  • Exist as body waves
  • Causes the ground to shake at right angles to the direction of the wave.
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10
Q

What are the two types of surface waves?

A
  1. Love waves
  2. Rayleigh waves
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11
Q

How do Love waves move?

A

Travel at right angles to the direction of movement.

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12
Q

Describe some characteristics of Love waves.

A
  • Fastest surface waves
  • Move from side to side
  • The most destructive surface wave
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13
Q

How do Rayleigh waves move?

A

Travel in a rolling motion.

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14
Q

Describe some characteristics of Rayleigh waves.

A
  • Both horizontal and vertical movement
  • Slowest surface waves
  • Cannot travel through liquids
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15
Q

What does earthquake intensity depend on?

A
  • the magnitude of the earthquake
  • the distance away from the earthquake
  • the local rock and soil conditions at the earthquake.
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16
Q

Define intensity in the context of a hazard.

A

The amount of damaged caused by an earthquake.

17
Q

What does the Richter Scale measure? How?

A

The size of the seismic waves that travel through the earth. It involves a system which classifies seismic wave power, where each step is 10x the power of the last.

18
Q

What are the negative aspects of the Richter Scale/ why is it no longer used?

A
  • Does not take into account that damage varies dependent on the rock composition and economic stability of a place.
  • The Richter scale has a tendency to underestimate large earthquake magnitudes.
19
Q

How does the Mercalli scale measure intensity?

A

It measures the amount of damage caused by an earthquake in a particular location.

20
Q

What does the Moment Magnitude scale measure? How?

A

The amount of energy released by an earthquake event. A formula is used which includes:
- the rigidity of the rock affected
- the distance moved by earthquake
- the size of the area where movement takes place.

21
Q

How deep are shallow focus earthquakes?

A

0-70km

22
Q

What is a basic definition of an earthquake?

A

Shock waves cause the ground to shake and move, this movement can cause damage to be caused

23
Q

What is a landslide in the context of an earthquake?

A

A hazard where cliff slopes weaken and fail due to shaking. They can travel several miles from their source, growing in size and collecting debris.

24
Q

What is a forest fire in the context of an earthquake?

A

A hazard where fires occur in urban areas, caused by ruptured gas pipes and electricity pylons.

25
Q

What is ground deformation in the context of an earthquake?

A

A hazard which occurs when an earthquake destabilises material.

26
Q

Describe fully the process of liquefaction in the context of an earthquake.

A
  1. When ground deformation occurs in soil with a high water content, rigid rock particles lose their structural strength and separate.
  2. These particles break down into smaller, unconsolidated rock particles, causing the soil to lose its mechanical strength.
  3. The soil begins to act like a liquid.
27
Q

What is a tsunami in the context of an earthquake?

A

Offshore earthquakes can cause giant waves which displace hundreds of kilometres of water when the seabed is shifted several metres. This causes giant waves which travel through the sea

28
Q

Give an example of a landslide in the context of an earthquake?

A

The Khait landslide (1949) occured in Tajikstan after a 7.4 magnitude earthquake.

29
Q

Give an example of a forest fire in the context of an earthquake.

A
30
Q

Give an example of ground deformation in the context of an earthquake.

A
31
Q

Give an example of liquefaction in the context of an earthquake.

A
32
Q

Give an example of a tsunami in the context of an earthquake.

A