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Geology 11
3RD LONG EXAM
GEOHAZARD EARTHQUAKES
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intese ground-shaking caused by sudden release in energy
earthquakes
tectonic is produced by
sudden movement along faults
plate boundaries
volcanoes are induced by
lava/magma rising beneath active volcanoes
study of earthquakes
seismology
device that records seismic waves
seismometer
recording of the seismic waves
seismogram
what is being record by the seismograph?
seismic waves
this states that the crust of the earth gradually stores elastic stress, and the energy is released during earthquake
elastic rebound theory
elastic rebound theory
is proposed by
harry fielding reid
this usually describes the origin of the energy of the earthquake
elastic rebound theory
state all parts of an earthquake
hypocenter
fault plane
epicenter
area of rupture; where the seismic waves emanate from
hypocenter
(focus)
surface where slippage occurs
fault plane
fault plane
upward -
reverse
fault
downward -
normal
fault
across -
strike-slip
fault
point where the focus is projected onto the surface
epicenter
2 types of seismic waves
body waves
surface waves
two types of body waves
primary waves
secondary waves
two types of surface waves
rayleigh waves
love waves
this emanate from the focus and radiate in all directions thru the earth's interior
body waves
true or false. some energy is converted into surface waves
true
this travel by compressing the mediums they travel on
primary waves
this wave can only travl thru solids
secondary waves
this wave can move thru
solid
and
liquid

primary waves
this travel along path nearby parallel to surface of the earth but not interior
surface waves
like water displacements
rayleigh waves
horizontal displacement of wavesor side-to-side motion felt when there's a presence of earthquake
love waves
intensity
describes the degree of ground-shaking at a given locale based on the amount of damage
magnitude
calculated from seismic records and estimates the amount of energy at the source
what does PHILVOCES use to measure the intensity
PHILIPPINE EARTHQUAKE INTENSITY SCALE
(
PEIS
)
this amount difference in type of structures and in materials used in local production
PHILIPPINE EARTHQUAKE INTENSITY SCALE
(
PEIS
)
where magnitude is being measured
richter scale of moment magnitude
true or false.
earthquakes can be predicted
false
true or false.
the patter and behavior of the earthquakes which in turn give us a good estimate
true
this states the sections of active fault that have relatively few earthquakes are likely sites of future strong earthquakes
gap hypothesis
these are areas along the fault where relatively small earthquakes have occurred
seismic gap
what is first located in the seismogram?
primary waves