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Earth's Layers,Boundaries, and Tectonic Plates - 2017

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


6th Grade Science Teacher
Bethel Middle School
Waynesville, NC

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