Test 1 stuff Flashcards
_____ are common and seismic hazard is high throughout the carribean
earthquakes
earthquakes cannot be reliably ___ or ___
predicted or mitigated
earthquake is composed of 3 forces
stress, strain, strneght
stress of an earthquake is
force per area
strain of an earthquake is
% distortion
strength of an earthquake is
rocks break at critical values
rocks deform ____, then rebound during an earthquake rupture
elastically
when the stress exceeds the strength of the rocks along the fault, it ___
slips
when the fault slips, it ____
releases the stress suddenly which causes an earthquake
____ ____ are ground vibrations caused by rocks slipping along opposite sides of a fault
seismic waves
why do earthquakes occur
elastic rebound theory,
fault rupture
where does the rupture of an earthquake begin
focus
machines that record seismic waves generated by earthquakes
seismographs
where are seismic waves generated
generated at earthquake focus
___ ___ travel over earth’s surface
surface waves
___ ___ and ___ ____ travel through earth’s interior
primary waves and secondary waves
seismic waves arrive in which order
primary, secondary, and surface
body waves travel where
through earth
surface waves travel where
along earth’s surface
2 types of surface waves
Rayleigh and love waves
2 types of body waves
P/S waves
have a push/ pull compressional motion (slinky)
travel through solids, liquids, and gases,
greatest velocity of all earthquake waves
4.8km/sec in continental crust
primary (P) waves
up-down motion
travels only through solids
slower velocity than P waves
3km/sec in continental crust
S waves
place within earth where earthquake waves originate
focus
point on the surface directly above the focus
epicenter
intersection of 3 circles from 3 recording stations is the
epicenter
each release in magnititude releases ___ times more energy
32
measure of the degree of earthquake shaking at a given locale based on the amount of damage
mercalli intensity
introduced by Charles Richter in 1935
measures the amplitude of sesmic waves
magnitude
measure very large earthquakes
derived from the amount of displacement that occurs along a fault zone and rupture area
moment magnitude (Mw)
causes pressure in pores between grains to increase and turns the substrate into a fluid
liquefaction of the ground
during liquefaction
saturated material turns fluid and underground objects may float to the surface
when is amplitude of shaking the ground greatest?
unconsolidated sediment and artificial fill
liquefactions sometimes causes
sand volcanoes or sand boils
harbor wave
tsunami
formed by something that rapidly moves large amounts of water
tusanmi
uplift of seawater during thrust faulting produces surge of water
tsunami
a tsunami is only a few ____ high in the deep ocean
cm
how fast do tsunamis travel
speed of a jetliner , so early warning systems are possible
tsunami sources from most frequent to less frequent
oceanic earthquakes, submarine landslides, volcanoes, meteor impact
estimates the probability that an earthquake of a certain magnitude will occur in a particular area during a specific time
earthquake forecasting
usable earthquake prediction has these factors
time interval in which quakes occur,
region where quakes occur
magnitude range of predicted quake
two forecasting strategies for earthquakes
find a specific precursor
forecast a general pattern
earthquake clustering theory
quakes are more likely when there are other quakes
seismic gap theory
quakes are due if they have not happened in a while
precursors to earthquakes
change in # of quakes, slow ground motion, radon’s emission, electrical resistivity, electromagnetic waves, water chemistry, seismic wave velocity, changes in animal behavior
estimate of the avg amount f time between large eq’s in a given location or on a given fault
recurrence interval
reduces eq’s generated forces acting on buildings
base isolation
more cohesive to less cohesive
damp sand, dry sand, water saturated snad
most common type of meteorite, 75-90% silicon, 10-25% Nickel-iron alloy
stony asteroid
likely from core of asteroid, mostly nickel-iron alloy
iron asteroid
shows which minerals are stable at depth
High P + T experiments
does earth’s magnetic field wander?
yes
has earth’s magnetic field reversed/
yes
dipole points ot south
normal polarity
dipole points to the north
reverse polarity
earth’s chemical layers
core(iron /nickl/sulfur) –> mantle (silicate material) –> crust (granite/ basaltic rocks)
earth’s physical layers
inner core (rigid) –> outer core (liquid) –> mesosphere (rigid) –> asthenosphere –> plastic –> lithosphere (rigid) –. ocean
seismic waves ____/____ at the interfaces between layers within the earth
reflect / refract
S waves DO NOT travel where
outer core
higher density in ____ vs mantle
outer core
describe S waves speed
increase in strong lithosphere
slight decrease in speed in weak asthenosphere
increase below asthenosphere in upper mantle
increase below the 410 KM mantle discontinutiy
increase below the upper / lower mantle transition.
geothermal gradient in normal continental crust is ___ to ____ per km
20 to 30 C
temperature near base of lithospehre
1400 C
outer core temperature
3000 C
inner core temperature
5000 C
in the p-wave shadow zone
no P or S waves recorded
in S wave shadow zone
only P waves recorded
p wave shadow zone is from
105 -142 due to reaction when they enter / leave the core
S wave shadow zone is from
105-180 because they cannot travel through outer core
sphere’s radius or inner core radius is
1216 kim
what makes up the inner core
iron nickel / iron nickel alloy
outer core radius
2270 km
what makes up outer core
iron and nickl
lower mantle is call dhte
mesophere
lower mantle is made up of
peridotite
part of upper mantle
asthenosperhe
velocity of seismic waves increases where
mohorovicic discontinuity
what separates crust from underlying mantle
mohorovicic discontinuity
is part of the crust / upper mantle
lithospehree