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continental crust
lower density
ocean crust
higher density
lithosphere
crust & uppermost mantle (tectonic plates)
Asthenosphere
weak, allows plates to move
upper mantle
670 km
lower mantle
2900 km
outer core
liquid, Fe-Ni
mantle
solid silicate minerals
inner core
solid, Fe-Ni
lithospheric plates
can be made up of both oceanic and continental crust
plate boundaries
divergent, convergent, transform
divergent
move away from each other; new oceanic crust created at mid-ocean ridges
convergent
move towards each other; subduction (sometimes)
shallow depth earthquakes
(0-50 km)
intermediate depth earthquakes
(50-250 km)
deep earthquakes
(250-500 km)