Chapter 10 - Earthquakes and Earth's Interior Flashcards

1
Q

Seismology

A

Study of earthquakes

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2
Q

Seismometer

A

used to record shocks and vibrations from earthquakes

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3
Q

Inertial Seismometer

A

Relies on resistance of stationary mass to movement

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4
Q

Focus

A

point where earthquake starts to release elastic strain of surrounding rock

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5
Q

Epicenter

A

point on earth’s surface lying vertically above focus

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6
Q

Seismic Waves

A

vibrational waves that spread out in all directions initially from focus

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7
Q

Body waves

A

seismic waves that travel through earth’s interior

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8
Q

Primary (P) Wave

A

compressional - can pass through solids or fluids - rock vibrates back and forth in line of wave motion - fastest

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9
Q

Secondary (S) Wave

A

cannot pass through fluids - rock moves sideways perpendicular to direction of wave travel - slower that P waves

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10
Q

Surface Wave

A

pass around earth rather than through it - slower than either P waves or S waves - different wavelengths develop different velocities (dispersion)

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11
Q

Determining Epicenter

A

locate from arrival times of P waves and S waves at 3 or more seismometers

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12
Q

Richter Magnitude Scale

A

estimated by measuring amplitudes of seismic waves - divided into steps representing 30 times increase in energy

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13
Q

Earthquake Hazard

A

most large earthquakes occur along plate boundaries - seismic risk maps based on acceleration relative to gravity used to design roadways and public buildings

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14
Q

Earthquake Disasters

A

Based on number of people killed

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15
Q

Earthquake Damage

A

1) Ground motion - 2) displacement along faults - 3) fire - 4) landslides - 5) liquefaction - 6) tsunamis

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16
Q

Ground Motion

A

results from movement of seismic waves: especially surface waves

17
Q

Displacement Along Faults

A

Features that cross or sit on faults can be broken

18
Q

Fire

A

started by broken gas mains and electrical wires - water mains also broken

19
Q

Landslides

A

earthquakes may trigger rapid mass wasting movements

20
Q

Liquefaction

A

shaking can turn saturated sediment/regolith into liquid mass

21
Q

Tsunamis (Seismic Sea Waves)

A

High velocities - low amplitude in deep water but dramatic increase in shallow water

22
Q

Modified Mercalli Scale

A

Based on amount of vibration felt and building damage - depends on distance from epicenter as well as magnitude

23
Q

World Distribution

A

plate boundaries most subject to frequent earthquakes

24
Q

Circum-Pacific Belt

A

accounts for 80% of all earthquakes

25
Q

Mediterranean Himalayan Belt

A

accounts for 15% of all earthquakes

26
Q

Benioff Zone

A

depth of focus up to 700km

27
Q

First Motion Studies

A

can determine movement direction if fault orientation is known

28
Q

Elastic Rebound Theory

A

Energy stored in elastically deformed rock bodies - when fault slips rocks rebound to original shapes

29
Q

Seismic Gaps

A

Strain is steadily increasing but no earthquakes for a long time

30
Q

Earthquake Precursors

A

One case of odd animal behavior before earthquake

31
Q

Foreshocks

A

smaller earthquakes preceding a large earthquake

32
Q

Fluids in Faults

A

Will decrease friction that holds rock faces in place

33
Q

Discontinuities (Boundaries)

A

detected from refraction and reflection of body waves

34
Q

Moho

A

boundary between crust and mantle

35
Q

Oceanic Crust

A

8 km thick - Basalt then Gabbro

36
Q

Continental Crust

A

20-70 km thick - Granite then Diorite

37
Q

Mantle

A

Comprised of peridotite (rock made up of olivine and pyroxene)

38
Q

Core

A

P & S wave shadow zones indicate - outer core is liquid - composed of iron - inner core is solid