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asthenosphere
solid layer w plasticity in the upper mantle located below lithosphere, lithospheric plates "float and mover here
convection current
circular movement of fluids caused by the rising of hotter less dense fluid and falling of cooler denser fluid
convergent boundary
place where two tectonic plates move toward each other and collide
core
two part layer of Earth below the Mantle w a liquid outer core and solid inner core
crust
thin solid outermost layer of Earth either continential or oceanic
divergent boundary
where two tectonic plates move away from each other
energy
ability of a system to do work required for changes to happen within a system
lithosphere
cool rigid outermost layer of Earth that consists of the crust and uppermost part of the Mantle, broken into pieces or segments called plates
magnetic field
area around a magnet or moving electrical charge that can exert a magnetic force
mantle
solid layer of Earth between the Crust and core made of dense siliciates
plasticity
characteristic of the material in asthenosphere, existing in a solid state having the ability to flow
plate boundary
place where two different plates have contact
rift valley
trench formed between highlands on a divergent boundary where plates separate
seafloor spreading
phenomenon by which magma from Earth's mantle comes up at the mid ocean ridges and creates new oceanic crust
seismic waves
waves of energy that travel through earth and are the result of an earthquake volcano or explosion
subduction
process in which a denser plate is pushed down beneath a less dense plate when plate converge
tectonic plate
huge piece of crust that slowly moves on the upper ductile part of the mantle
transform boundary
place where two tectonic plates slide past each other