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Unit II (Our Restless Earth) Vocab

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AB
asthenosphereouter layer of the mantle
collision boundarytwo colliding plates both are carrying continents
converging boundarytwo plates come together
diverging boundarytwo plates pull apart
cratonthe ancient core of a continent
faulta crack in the earths crust
lithospherethe outer solid layer of the earth
plate tectonicsthe theory of moving plates
spreading centersridges where plates move apart and new crust is formed
subduction boundarya convering boundary where the oceanic plate goes under the continental plate
terranea section of plate that has been added to a continent
batholithan extremely large igneous intrusion
dikea vertical igneous intrusion
felsiclight coloured, high in silica magma
maficdark coloured, low in silica magma
hot spotan area of volcanic activity in the middle of a plate
laccolitha dome shaped igneous intrusion
lavamagma that has escaped the earth
magmamolten rock in the earth
plutonmagma that has cooled in the earth (igneous intrusion)
rift eruptionvolcanic eruption at a narrow crack in the crust
silla horizontal pluton
subduction boundary eruptioneruption where an oceanin plate goes under a continent
tephraextremely light rock from volcanic ash
shield volcanoa very low, wide volcano which flows lava
cinder cone volcanosteep sided volcano
composite (strato) volcanolarge, mountain like volcano that erupts violently
earthquakeshaking of earth due to plate movement
elastic reboundwhen a plate deforms then releases
epicenterthe point directly above the focus of an earthquake
focuswhere a plate first moves
L wavessurface earthquake waves
P wavesthe first earthquake waves to arrive
S wavesthe second waves to arrive in an earthquake
mohorovic discontinuitya layer in mantle where waves slow down
richter scaleused to measure damage from earthquakes
seismograma record of the earth's shaking
seismographinstrument the records the earth's shaking
shadow zonezone of earth where earthqauke waves don't show up
time-travel graphshows the time it takes for waves to arrive
active continental marginthe edge of a continent that is also a plate boundary
passive continental marginthe edge of continent built up by sediments
anticlinean upward fold in rock layers
synclinea downward fold in rock layers
dome mountainin individual moutain resulting form folding
fault-block mountainsmountains resulting from uplifting
jointa crack in rock where here is no movement
normal faulta fault where one piece drops down
reverse faultone piece is driven up over the other piece
strike-slip faultone piece slides past the other piece


Rutland Senior Secondary
BC

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