WPR 2 Vocab Flashcards

0
Q

interplate boundary

A

earthquake at boundary of 2 plates

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1
Q

elastic rebound theory

A

rocks on either side of fault bending or deforming instead of slipping. continue until slip and straighten out, releasing energy

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2
Q

intraplate boundary

A

earthquake at the interior of a plate

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3
Q

convergent boundary

A

tectonic plate boundary along 2 plates. comes together by subduction (one goes under other, lighter goes over) or collision
force = compression
depth = 400km deep
magnitude = highest

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4
Q

divergent boundary

A

spreading plate boundaries, force = tension
depth = <10km
weakest magnitude

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5
Q

transform boundary

A

fault boundary where 2 plates slide past each other, force = shear
intermediate depth
intermediate magnitude

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6
Q

focus

A

origin of where fault first slipped, center of seismic waves

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7
Q

epicenter

A

point on map directly above focus, strongest shaking occurs

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8
Q

S Wave

A
secondary wave, 
shear waves or wiggling motion, moving at 90 degree angles
2nd to arrive
3.5km/s velocity
force = shear
change in shape 
travels through solids
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9
Q

p waves

A

primary waves: compressional waves, sudden jolt
velocity = 6 km/s
1st to arrive
motion parallel, force = compression
change in volume and travel through all mediums

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10
Q

surface waves

A

along surface, series of rolling motions
travel only at earth’s crust
most destructive, but slower than P or S waves

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11
Q

Body waves

A

travels through the earth

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12
Q

period

A

cycle between peak to peak

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13
Q

wavelength

A

distance between wave crest

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14
Q

amplitude

A

amount of positive or negative shift in the earth

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15
Q

frequency

A

number of peaks per second

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16
Q

seismograph

A

records shaking of earthquakes on record. time travel graph helps find epicenter
tool

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17
Q

seismology

A

scientific study of earthquakes and propogation of elastic waves through earth

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18
Q

seismogram

A

recorder (paper with the information on it)
know P&S wave time, distance between P & S
magnitude found from time of arrival and height of amplitude
multiple magnitudes find location of earthquake

19
Q

focal mechanism

A

direction of slip in an earthquake and orientation of the fault

goes from negative (tension) to positive (compression). creates image of movement for EQ

20
Q

beach ball

A

represents focal mechanism
P waves produce characteristic motion
first motion describe solution

21
Q

fault plane

A

3 dimensional movement parallel to plate movement

22
Q

auxiliary plane

A

line drive pass hypocenter/focus perpendiclar to movement of plates

use to determine push (big up) or pull (big down) motion of earthquake
push= compression, pull = tension

23
Q

magnitude

A

measure of the amplitude and time of arrival from earthquake.
measures energy released

24
intensity
based on observation of individuals during and after earthquake. severity of shaking
25
Richter Scale
standardized system of magnitude measurement, log 10 scale
26
Mercalli Scale
quantify intensity of earthquake. based on how people felt
27
acceleration
designated as proportion of gravity. most <1g
28
liquefaction
soils that ordinarily seem stable become almost liquid during shaking requires loose soils and saturation
29
ML and Mw
local magnitude | measure of total energy expended
30
shaking
duration depends on size, distance | severity material dependent
31
isoseismal
used to show lines of equal felt seismic intensity
32
tsunami
harbor wave, rise highest when forced onto harbor, generated by EQ long wavelength in ocean generated by sudden displacement of water column E = h^2*wavelength V = SQRT(g*D) gravity * depth high wave comes from continuing energy
33
precursor
signs that forecast EQ. tectonic plate movement, micro earthquakes, change in Radon, ground elevation change, zones of fluid pressure, etc.
34
foreshock
minor earthquakes preceding major
35
paleoseismology
study of prehistoric EQ and fault movements
36
prediction
utilizing warning systems to determine when, where, how large EQ will occur
37
forecasting
utilizing warning system to generate general location, frequency, magnitude of EQ. likelihood over given time
38
seismic gap theory
segments of major faults with less EQ than neighboring segments more likely to have EQ over time. strain accumulates over time and record of past events help determine likely frequency
39
peak ground acceleration
designated as proportion to gravity
40
risk map
estimation based on probability of risk. where and when EQ will shake based on post activity and given time
41
reinforced concrete
breaks in EQ, leaves enclosed steel frame to fail
42
retrofitting
modifying existing buildings to minimize the damage during strong earthquakes
43
base isolation
isolate buildings from shaking grounds buildings break if weak floors due to lateral movement. sway related to frequency: resonance more sway,
44
isoseismal map
shows lines of equal felt seismic intensity
45
seismic risk
depicts probability of impact within specified area