Unit 2 - Earthquakes Flashcards

(19 cards)

1
Q

About how many total earthquakes of any size occur globally each year.

A

1.3 million, but most are very small.

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2
Q

The largest earthquake to occur on Earth over the past 100 years

A

Occurred in Chile in 1960, magnitude of 9.5, lasted 11 minutes

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3
Q

Where most earthquakes occur

A

plate boundaries

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4
Q

earthquake

A

A sudden break in the crust after a long period of stress buildup due to motions of tectonic plates.

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5
Q

The concept of elastic rebound

A

When the crust bends like rubber (storing energy), then unbends (releasing energy), like it’s a piece of rubber

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6
Q

The concept of stick-slip behavior

A

When faults remain stuck while energy builds, then suddenly slip when energy is released.

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7
Q

asperities

A

the rough edges that grind each other down

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8
Q

why does slipstick occur

A

Stick-slip occurs because friction and rough spots (protrusions) along the fault (called asperities) prevent the fault from sliding until they can be overcome.

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9
Q

How we observe the buildup of stress on a fault.

A

Can be observed using very precise GPS

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10
Q

Where thrust faults occur.

A

Occurs in compressional settings like subduction zones

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11
Q

Where normal faults occur.

A

Occurs in extensional settings like mid ocean ridges

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12
Q

Where transform (strike-slip) faults occur

A

Occurs in settings where plates slide laterally past each other like transform boundaries

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13
Q

What an earthquake hypocenter is.

A

Location at depth where the earthquake started.

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14
Q

Characteristics of P waves.

A

(Stands for primary or pressure waves)
push-pull motion (compresses then expands like a sound wave)
Travels through solids, liquids, and gasses
Fastest seismic waves (first to arrive), but cause the least shaking

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15
Q

Characteristics of S waves.

A

(S for secondary or shear)
Side to side motion (shear)
Travel only through solids
S-waves’ energy can convert into P-waves so it may travel through the liquid outer core
P-waves can also convert back to S-waves in the solid inner core
Slower than P-waves (second to arrive)

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16
Q

Characteristics of surface waves

A

Love Waves
Side to side motion
Travel only along the surface of a solid
Rayleigh Waves
Up-down motion like an ocean wave
Travel only along the surface of a solid
Surface waves are the last to arrive, but cause the most deformation

17
Q

How we know that the outer core of the Earth is liquid

A

The refraction of p-waves as they crossed over to the inner core shows us that the inner core is solid
discover outer core was liquid from the s-wave shadow zone

18
Q

How much the amount of shaking varies between different magnitude earthquakes.

A

Each unit increase in earthquake magnitude corresponding to a factor of 10 increase in shaking
ex. M5 is 10 times amount of shaking from M4

19
Q

The theoretical maximum magnitude earthquake that can occur.

A

M9.5 because that’s the largest fault that could slide.