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50 Cards in this Set

  • Front
  • Back
lithosphere
brittle
where there are earthquakes
100 km
asthenosphere
plastic
flows over very long time scales (millions of years)
mesophere
'solid'
will flow very slowly
100s of millions of years
outer core
liquid
magnetic field generates high temperature
inner core
solid
very high temp, high pressure
crust
very light weight material
silicon & oxygen
mantle
denser, heavier stuff
(lower part of lithosphere/ asthenosphere)
core
very heavy stuff
iron & nickel
radioactive decay (current source of heat)
P-wave
body
any material
longitudinal
S-wave
body
transverse
only solid
L wave
(love waves)
surface waves
transverse
R wave
(rayleigh waves)
surface waves
long/ tran
transverse wave
particle motion perpendicular to wave propagation
longitudinal wave
particle motion parallel to wave propagation
3 fault types
normal
reverse
strike slip
What kind of stress is normal fault?
tensional stress
What kind of stress is reverse fault?
compressional stress
What kind of stress is strike slip fault?
shear stress
oblique fault
the fault combined dip slip & strike slip
oceanic crust
thin, under oceans
7-10 km
young-> created/ destroyed continuously 200 million years/ denser
continental crust
less dense then oceanic crust, deep roots up to 70 km thick as old as 4 billion yrs.
isostasy
iceberg-> floating equilibrium
light things float and have things sink
high mountains have very deep crusted roots
Lord Kelvin
Caclulated the earth to be 24 million years old
radioactive decay
current source of heat
heat generated in core & lower mantle
theory of plate tectonics
plates move, created, destroyed
mid ocean ridges do what?
create oceanic crust
subduction zone does what?
destroy oceanic crust
transform plates do what?
plates move sideways
how do we know that the continents was just a big mass of land?
1. fit of continents
2. mountain belts matched across continental boundary
3.dwelling animal fossils found on widely spread continents
continents are made mostly of what? do they sink or are they light?
granite which are light
oceanic rocks are made of what? and are they heavy or light
they are made of basalt which is heavier
divergent plate boundary
mid ocean ridge/ spreading ridge
plates move apart
create new oceanic crust
convergent plate boundary
(continent/ ocean convergence a.k.a. subduction zone)
plates move towards each other
subduction zones
do what? and what do we get?
what kind of crust? how old?
deep earthquakes
destroy oceanic crust
we get volcanoes
ocean crust
0-200 million yrs
example of subduction zone
Wadate Benioff
transform plate boundary
crust moves horizontally
seismic wave definition
wave disturbance traveling through medium (air, water, rock)
energy is transfered from on particle to the next
amplitude
height of strength of wave
wave length
distance between two successive crests
frequency
# of waves that pass by you in a given amount of time
period
duration (in time) of the wave cycle (T)
wavefront
where the front of a wave is at a given time
ray
direction the wave is moving perpendicular to wave front
body waves
travel through earth
surface wave
travel on outer part of earth
travel time
how long it takes to get between two points
arrival time
time determined on our seismogram
p-wave
arrives first fastest wave
seismoscope
measure direction of waves not time
first type of seismic record
chinese