Chapter 10 - Earthquakes and Earth's Interior Flashcards

(38 cards)

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
Mediterranean Himalayan Belt
accounts for 15% of all earthquakes
26
Benioff Zone
depth of focus up to 700km
27
First Motion Studies
can determine movement direction if fault orientation is known
28
Elastic Rebound Theory
Energy stored in elastically deformed rock bodies - when fault slips rocks rebound to original shapes
29
Seismic Gaps
Strain is steadily increasing but no earthquakes for a long time
30
Earthquake Precursors
One case of odd animal behavior before earthquake
31
Foreshocks
smaller earthquakes preceding a large earthquake
32
Fluids in Faults
Will decrease friction that holds rock faces in place
33
Discontinuities (Boundaries)
detected from refraction and reflection of body waves
34
Moho
boundary between crust and mantle
35
Oceanic Crust
8 km thick - Basalt then Gabbro
36
Continental Crust
20-70 km thick - Granite then Diorite
37
Mantle
Comprised of peridotite (rock made up of olivine and pyroxene)
38
Core
P & S wave shadow zones indicate - outer core is liquid - composed of iron - inner core is solid