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Earth's Layers

TermDefinition
Pangea name of single land mass that broke apart 225 million years ago
plate tectonics theory that pieces of Earth's lithosphere are in constant motion driven by convection currents in the mantle
asthenosphere soft layer of the mantle on which the lithosphere floats
sonar system that determines distance of an object under water by recording echoes of sound waves
mantle layer of a hot, solid material between Earth's crust and core
conduction transfer of heat from ne substnace to another by direct contact of particle matters
convection currents movement of fluid, caused by differences in temperature, that transfer heat from part liquid to another
radiation transfer of energy through deep empty space by electromagnetic waves
sea-floor spreading process by which molten material adds new oceanic crust to the ocean floor
MOR undersea mountain chain where new ocean floor is produced; a divergent boundary
lithosphere rigid layer made up of the uppermost part of the mantle and crust
convergent boundary plate boundary where two plates move toward eachother
convection transfer of heat by movement of a fluid
continental drift hypothesis that continents slowly move across the Earth's surface
transform boundary plate boundary where two plates move past each other in opposite directions
outer core layer of molten iron and nickel that surrounds the inner core
inner core dense sphere of solid nickel and iron in the center of the Earth
divergent boundary plate boundary where two plates move away from each other
subduction process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at convergent boundary
crust layer of rock that forms Earth's outer surface
temperature the measure of how hot or cold something is
Created by: cj_ritter
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