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Earth's Structure and Tectonic Plates

AB
inner coremost dense layer of earth; extreme pressure; solid iron and nickel
outer coreliquid layer of earth; iron and nickel; responsible for earth's magnetic field
continental crustthickest layer of crust; mostly granite
oceanic crustthinnest, more dense layer of crust; mostly basalt
mantlethickest layer of earth; molten rock material
convection currentsmovement occurring in asthenosphere; causes tectonic plates to move
densityreason structure of earth is in layers
lithosphereall of crust and uppermost part of mantle; broken into tectonic plates
plate boundarieswhere two plates meet; most earthquakes and volcanoes occur here
divergent boundarywhere two plates separate away from each other
convergent boundarywhere two plates collide
oceanic-oceanictype of convergent boundary where deep ocean trenches and island arcs form
continental-continentaltype of convergent boundary where mountains form
transform boundarywhere two plates slide past each other; earthquakes commonly occur here
subductionprocess where one tectonic plate sinks beneath another tectonic plate and into the mantle
sea-floor spreadingprocess when two plates diverge and new ocean crust is created as magma from the mantle rises and spreads out
mid-ocean ridge and rift valleytwo geographic features that form when plates separate
ocean trencha deep depression in the ocean floor at a subduction zone
magma chamberwhere magma is stored under a volcano
volcanoan opening in Earth's crust through which molten rock, rock fragments, and hot gases erupt
shield volcanousually largest type of volcano; gentle sloping sides; non-violent fluid lava flows
cinder cone volcanosmall and simple type of volcano; usually has only one vent; short violent eruptions
craterhollowed out bowl-shaped area at the top of a volcano
lavaname for magma when it reaches earth's surface
composite volcanostratovolcano; eruptions for layers; often violent eruptions; most common type; tall and steep sided
earthquakethe shaking of the ground caused by the sudden movement of large blocks of rock along a fault
epicenterthe point on earth's surface directly above the focus of an earthquake
focusthe point underground where tectonic plates first begin to move during an earthquake
secondary wavesseismic waves that cannot travel through core (liquids); slower than primary waves
surface wavesslowest moving seismic waves; can cause ground to roll like ocean waves; damage structures on earth's surface
magnitudemeasurement of an earthquakes strength based on seismic waves and movement along faults
primary wavesfastest seismic waves; first released during an earthquake; travel through all layers of earth
tsunamigiant wave caused by an underwater earthquake


6th Grade Science Teacher
Bethel Middle School
Waynesville, NC

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