Earthquake Flashcards

1
Q

Fractures in earth’s surface

A

Faults

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2
Q

Location where slippage begins

A

Hypocenter or focus

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3
Q

Point on Earth’s surface directly above the focus or hypocenter

A

Epicenter

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4
Q

States that large slabs of Earth’s lithosphere are continually grinding past each other

A

Plate tectonics

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5
Q

Earth’s strongest earthquakes most often occur in

A

Convergent plate boundaries

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6
Q

Plate boundary between a subducting slab of oceanic lithosphere and an overlying continental plate

A

Megathrust fault

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7
Q

Faults in which the dominant displacement is horizontal and parallel to the direction of fault trace

A

Strike-slip faults

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8
Q

Instrument that makes a record of seismic waves

A

Seismograph or seismometer

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9
Q

Records obtained from seismograph

A

Seismogram

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10
Q

Earthquakes generate four principal types of elastic waves

  • 2
  • 2
A

Body waves - travel within the earth

Surface waves - travel along its surface

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11
Q

Body waves are further divided into

A
P waves (primary waves)
S waves (secondary waves)
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12
Q

*back and forth motion in the direction of the path of propagation, stretching or compressing the medium as the wave passes any point

A

P waves (compressional or longitudinal)

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13
Q

*move back and forth perpendicular to the direction of propagation

The medium is sheared first in one direction and then in another

A

S waves (shear waves)

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14
Q

P waves temporarily change the * of material while S waves change the * of the material that transmits them

A

Volume

Shape

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15
Q
  • travel faster and it moves the ground from side to side

Displacement of the medium is entirely perpendicular to the direction of propagation and has no vertical or longitudinal components

Produce entirely horizontal motion

A

Love waves

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16
Q

Their motion is a combination of longitudinal compression and dilation that results in an elliptical motion of points on the surface

Rolls the ground: moves the ground up and down and side to side

A

Rayleigh waves

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17
Q

Arrange the waves in order of arrival and increasing amplitude (power/damage)

A

P - S - Love - Rayleigh

P: 70% faster than S waves
S: 10% faster than surface waves

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18
Q

Zone of greatest seismic activity

A

Circum-Pacific Belt

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19
Q

Circumpacific belt encompasses the coastal region of

A

Chile, Central America, Indonesia, Japan, Alaska

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20
Q

Measures the intensity of an earthquake through *

A

Modified Mercalli Scale

Damage

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21
Q

Measures the magnitude of earthquake through *

A

Richter scale

Energy released

22
Q

Tsunamis are generated by displacement along a * fault that suddenly lifts a large slab of sea floor

A

Megathrust fault

23
Q

Changes in shape, position, or orientation of a rock mass

A

Deformation

24
Q

The chemical bonds of the minerals within a rock are stretched but do not break

*first response

A

Elastic deformation

25
Once the elastic limit (strength) is surpassed, it either flows * or fractures *
Ductile deformation Brittle deformation
26
Rock near the surface where temperatures and confining pressures are low exhibit...
Brittle deformation
27
At depth, where temperatures and confining pressures are high, rocks exhibit...
Ductile deformation
28
Flat-lying sedimentary and volcanic rocks are often bent into a series of wavelike undulations called * Mostly caused by * that result in the shortening and thickening if thrust
Folds Compressional forces
29
Upfold (arrching of sedimentary layers)
Anticlines
30
Downfolds or troughs
Synclines
31
In anticline, * is found in Center In syncline , * is found in center
Oldest strata Youngest
32
Structures with approximately circular or slightly elongate, closed outcrop patterns * convex upward * concave upward
Domes and basins Dome convex Basin concave
33
Large, step-like folds in otherwise horizontal sedimentary strata
Monoclines
34
Upper or overlying block Block below
Hanging wall | Footwall
35
Dipslip faults where the hanging wall block moves down relative to the footwall block
Normal faults
36
A block that has dropped relatively downward between two normal faults dipping toward each other
Graben
37
Block that has been relatively uplifted between two normal faults that dip away from each other
Horst
38
Dipslip faults in which the hanging wall block moves up relative to the footwall block
Reverse fault
39
Normal faults occur in * environments, reverse faults result from strong *
Tensional ~ lengthening Of Earth’s crust Strong compressional forces - shortening or contraction of Earth’s crust
40
Reverse faults that dip less than 45 degrees
Thrust faults
41
Thrust faults with very low angle of dip and very large displacement
Overthrust
42
Fault in which the dominant displacement is horizontal and parallel to the strike of the fault surface *horizontal compression
Strike-slip fault
43
Example of strike slip faut
San Andreas Fault
44
Fractures along which no appreciable displacement has occurred
Joints
45
Mountain building *plate boundary
Orogenesis Convergent
46
Main driving force of orogenesis
Subduction of oceanic lithosphere
47
Oceanic lithosphere subducts beneath an oceanic plate
Volcanic island arc
48
Subduction beneath a continental block
Continental volcanic arc
49
Chaotic accumulation of sedimentary and metamorphic rocks with occasional scraps of ocean crust
Accretionary wedge
50
Relatively small crustal fragment which may be accreted to continents when subduction brings them to trench
Terranez
51
Himalayas and Appalachians were formed by
The collision of landmasses formerly separated by now-subducted ocean basins