lecture 6 Flashcards

1
Q

magnitude scale

A

descirbes the size of an earthquake

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2
Q

Richter original scale

A

magnitude determined using peak amplitude of waves

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3
Q

seismic moment

A

truer measure of an earthquakes energy

- product of earthquake rupture area and the average slip that occurs and the shear modulus

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4
Q

earthquake moment equation

A

moment (nm) = rupture area (m2) x slip (m) x shear modulus (n/m2)

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5
Q

moment magnitude

A

Mw - modern earthquake magnitude scale

- more related to moment than Richters scale

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6
Q

moment magnitude equation

A

(log10 moment - 9) / 1.5

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7
Q

relationship of rupture area and average slip

A

rupture area is key to governing the moment and moment magnitude of an earthquake
ex. smalle arthquakes rupture small areas

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8
Q

cascadia vs san andreas- same length

A

cascadia is subducting at a low angle and can host an earthquake at a larger area
has larger rupture availability

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9
Q

megathrust earthquakes

A
rupture long, gently dipping interface faults
very large (Mw> 8.4)
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10
Q

largest possible magnitude of earthquake

A

10.0
- 6000km length, 100m slip, 80km dip
(log10moment -9 ) / 1.5)

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11
Q

mainshocks and aftershocks

A

mainshock - largest event
aftershock- series of smaller events
as you go forward in time they get less frequent (decays with time)

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12
Q

MMI scale

A

modified mercalli intensity scale- describes the severity of shaking felt in an earthquake
- every earthquake has a range of intensities depending on how close you are

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13
Q

isoseismals

A

lines of equal intensities

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14
Q

2 ways to report earthquake intensity

A
  1. accelerometers: seismometer records strong ground motion from earthquakes
  2. felt reports: websites
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15
Q

directivity effect

A

rupture amplifies surface waves in direction

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16
Q

attenuation

A

The waves are largest where they are formed and gradually get smaller as they move away
- furthur from hypocenter the lower the intensity

17
Q

what do contours show

A

the depth of the top of subducting oceanic lithosphere

18
Q

basin amplification

A

increase in the size of seismic waves as they pass from hard bedrock (fast v) into loose sediment (slow v)
damage during earthquake is affected by intensity of shaking and engineering

19
Q

liquefaction

A

water saturated soils lose strength during shaking

20
Q

earthquake fatalities

A

continental earthquakes killed more people than subduction zone earthquakes despite being smaller