Locating and measuring EQs Flashcards

1
Q

Earthquake waves and propogation

A

deformation leading to strain and elastic stresses: stick and slip

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2
Q

P waves

A

Primary/comPressional

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3
Q

S waves

A

Secondary/Shear

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4
Q

Surface waves [2]

A

Love or Rayleigh

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5
Q

speed of waves

A

P, S, Surface

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6
Q

Shear waves can’t

A

travel through liquid - shadow beyond 104 degrees

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7
Q

Refraction of P waves

A

shadow 104-140 degrees

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8
Q

Seismometers

A

Detect passage of seismic waves
Masses and springs
Anchored to bedrock

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9
Q

Seismograms

A

Smoked drum or paper roll. Record rotates continuously, pen moves and leaves wiggles

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10
Q

Seismic measuring

A

vertical, N/S, E/W

Amplitude recorded proportional to velocity of the ground motion

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11
Q

WWSSN

A

World Wide Standard Seismic Network in the 1960s

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12
Q

Triangulation

A

epicentral distance to 3 stations + (P and S time differences

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13
Q

General magnitude

A
M= log(A/T) + f(d,h) + Ceq + Crec
A = amplitude, T = period, f = correction for epicentre distance D and focal depth H
Ceq = region correction
Crec = station correction
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14
Q

Local magnitude [ML]

A

Richter scale, invalid for M>8

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15
Q

Surface wave magnitude [Ms]

A
Ms = log10(A/T)max + 1.66log10 delta + 3.3
A = amplitude of ground motion in units 10^6m
T = time in seconds
delta = epicentral distance in degrees
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16
Q

Ms correlates with

A

damage

17
Q

Body wave magnitude [Mb]

A

For deep focus >50km
Mb = log10 (A/T)max + q (delta, h)
q= correction function based on epicentral range

18
Q

Seismic moment [Mo]

A
Mo = U A u
A = area of fault plane
U = shear modulus of deformed rocks
U = avergae slip
unbounded
19
Q

Moment Magnitude [Mw]

A

Mw = (log Mo) / 1.5 - 6.0

20
Q

Magnitude and Energy

A

log10 E = 5.24 + 1.44 Ms

21
Q

European Macroseismic Intensity Scale

A

worded descriptions but relies upon accurate reporting, presence of people