Chapter 8: Earthquakes Flashcards

1
Q

fault

A

a fracture plane on which sliding takes place

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2
Q

Earthquake

A

an episode of ground shaking

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3
Q

seismologist

A

geoscientists who study earthquakes

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4
Q

seismicity

A

earthquake activity

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5
Q

seismic waves

A

the energy released by vibrating rocks caused by an earthquake which travels away from the source in the form of waves

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6
Q

fault displacment

A

the distance between two ends of the offset marker (at a fault)

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7
Q

fault line/trace

A

the ground surface exposure of a fault (whether it appears due to erosion of

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8
Q

stress

A

a push, pull, or shear

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9
Q

elastic behavior

A

rock bends slightly but doesn’t break

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10
Q

elastic rebound theory

A

when slip takes place, the once-bent rocks adjacent to the fault rebound and vibrate back and forth until they regain their relaxed shape, thereby relieving the elastic strain.

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11
Q

stick-slip behavior

A

alternation between stress buildup and earthquake-generating slip events on existing faults

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12
Q

mainshock

A

the major earthquake

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13
Q

foreshocks

A

smaller earthquakes that precede the main shock (earthquake)

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14
Q

aftershocks

A

endured by a region affected by an earthquake in the days to months following, tend to be 10 times smaller than the main shock

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15
Q

focus

A

the location where seismic waves first begin to be generated, also known as the hypocenter

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16
Q

shallow focus earthquakes

A

occur in the top 60km of the Earth

17
Q

intermediate-focus earthquakes

A

takes place between 60 and 300 km

18
Q

deep focus earth quakes

A

occur down to a depth of about 660km

19
Q

epicenter

A

the point on the surface of the Earth that lies directly above the focus

20
Q

categories of seismic waves

A
  • body waves

- surface waves

21
Q

body waves

A

pass through the interior of the Earth

- cause material to vibrate in two different ways; compressional and shear

22
Q

surface waves-

A

travel along the Earth’s surface; vibrate in two different waves

  • up and down, rolling undulations
  • side to side, back and forth
23
Q

compressional waves

A

body waves that cause particles of material to move back and forth parallel to the direction in which the wave itself moves (squeeze together, then expand)

24
Q

shear waves

A

body waves that cause particles of material to move back and forth perpendicular to the direction in which the wave itself moves (up and down)

25
Q

types of waves all together

A

P-waves: fastest
S-waves: next fastest (60% of the speed of p-waves)
L-waves: Slow
R-waves: Slow

26
Q

P-waves

A

Primary Waves: compressional body waves

27
Q

S-waves

A

Secondary Waves: shear body waves

28
Q

L-waves

A

Love Waves: surface waves that cause the ground to shimmy back and forth

29
Q

R-waves

A

Rayleigh Way: surface waves that cause the ground to undulate up and down

30
Q

seismometer (also known as seismograph)

A

measures the ground motion produced by an Earthquake and can be configured in two ways

  • vertical motion
  • horizontal motion
31
Q

seismogram

A

an earthquake record produced by a seismometer

32
Q

travel time curve

A

the time delay between P-waves and S-waves, depicted on a graph whose horizontal axis indicates distance from the epicenter and whose vertical axis indicates time.

33
Q

earthquake intensity

A

refers to the degree of ground shaking

34
Q

Modified Mercalli Intensity (MMI) scale

A

represent intensity at a location by a Roman numeral, intensity greater closer to the epicenter and decreases further away

35
Q

Earthquake magnitude

A

represents the amount of energy released from the seismic source, as indicated by the amplitude of ground shaking recorded by a seismometer

36
Q

richter scale

A

a logarithmic scale for defining earthquake magnitude

37
Q

moment magnitude

A

the most widely used scale to describe Earthquake magnitude; scientist measure the amplitudes of several different seismic waves, determine the dimension of the slipped area on the fault, and estimate the displacement that occurred, also a logarithmic scale

38
Q

seismic belts/zones

A

most correspond to plate boundaries, earthquakes here are called plate-boundary earthquakes

39
Q

intraplate earthquakes

A

earthquakes that occur away from plate boundaries