Lecture 6 - Earthquake Magnitude and Intensity Flashcards

1
Q

What does the magnitude scale describe?

A

The size of an earthquake.

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2
Q

How did Charles Richter’s original scale work? (1935)

A

Magnitude was determined using the peak amplitude of seismic waves and correcting for the earthquake- seismogram distance.
Example: a M 5 earthquake generates 23 mm peak motion 220 km away, where a M 4 earthquake would generate only 2.3 mm. The same M 5 event would generate 100 mm peak motion 100 km away.

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3
Q

What is seismic moment?

A

It is a truer measure of an earthquake’s energy.
It is the product of the earthquake rupture area (or rupture length × width), the average slip that occurs, and the shear modulus of the surrounding rock (its resistance to deformation by shear stress).

The shear modulus of Earth’s crust can be approximated as 3 × 10¹⁰ N/m²

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4
Q

How do you calculate Moment (Nm) ?

A

Moment (Nm) = Rupture area (m²) × slip (m) × shear modulus (N/m²)

The shear modulus of Earth’s crust can be approximated as 3 × 10¹⁰ N/m²

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5
Q

What is Moment magnitude (Mw) and how do you calculate it?

A

The moment magnitude (abbreviated Mw) is the modern earthquake magnitude scale. It approximates Richter’s original scale, but is related directly to the moment through the equation:
Moment magnitude = (log10 Moment − 9)/1.5

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6
Q

How much bigger is a magnitude n earthquake than a magnitude n-1 earthquake?
e.g. n=6 so n-1=5

A

31.6 times bigger

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7
Q

Why is rupture area key to governing the moment and moment magnitude of an earthquake?

A

The rupture area and average slip correlate across a wide range of earthquake magnitudes.

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8
Q

The 1,000 km-long Cascadia megathrust is thought capable of hosting Mw 9 earthquakes, yet the 1,000 km-long San Andreas fault is thought limited to Mw 8 ruptures. Why?

A

The Cascadia megathrust is a subduction zone so it will have a larger rupture area than the San Andreas Fault.

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9
Q

Of the twenty largest earthquakes since 1900 (M 8.4–9.5), how many were megathrust earthquakes?

A

seventeen, including the top eight largest events (M > 8.8)

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10
Q

Why are megathrust earthquakes so large?

A

They rupture long, gently-dipping plate interface faults.

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11
Q

By how much does each unit increase in Mw correspond to decrease in frequency?

A

ten-fold

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12
Q

What is the largest magnitude of earthquake possible and where would the earthquake occur?

A

10.1

Peru-Chile trench

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13
Q

In an earthquake sequence (large earthquakes) what is the largest event called?

A

the mainshock

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14
Q

What percentage of earthquake sequences have a foreshock?

A

5%

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15
Q

Are foreshocks useful for earthquake prediction?

A

Unfortunately, foreshocks look identical to “normal” small earthquakes that happen all the time, so in practice they are not very helpful.

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16
Q

What does intensity describe?

A

The severity of shaking felt in an earthquake, and is formalized in the Modified Mercalli Intensity Scale (MMI). It is descriptive, with Roman numerals expressing perceived levels of shaking.

17
Q

How can intensity be analysed?

A

Intensities can be plotted on a map, with lines of equal intensity termed isoseismals.
For pre-instrumental events, these may provide our best means for estimating the earthquake location and size.

18
Q

What two sources of data are used to routinely generate isoseismal maps in the present day?

A

Accelerometers: a type of seismometer designed to record strong ground motions from nearby earthquakes (but insensitive to small ground motions from distant events).
Felt reports: nowadays, these are collected using citizen science websites like the USGS “Did You Feel It?”

19
Q

Why did Wellington experience stronger shaking than Christchurch in the 2016 Mw 7.8 Kaikoura, NZ earthquake?

A

Wellington likely felt stronger shaking because of a directivity effect. The rupture migrated from SW to NE, amplifying surface waves in that direction.

20
Q

Why is there a difference in attenuation between eastern and western North America?

A

Due to their tectonic histories.

Rock type.

21
Q

What is basin amplification?

A

The increase in the size of seismic waves as they pass from hard bedrock into loose sediment.

22
Q

What is liquefaction?

A

How water-saturated soils lose strength during shaking, a common site effect in sedimentary basins.

23
Q

What are some examples of earthquakes where site effects was a factor in the damage?

A

2018 Mw 7.1 Anchorage intraslab earthquake
1964 Mw 9.4 Alaska megathrust earthquake
2015 Mw 7.8 Gorkha earthquake
2017 Mw 7.1 Puebla, Mexico intraslab earthquake