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7E6.5 A Plate Tectonics

AB
Plate TectonicsThe theory that explains how large pieces of the lithosphere, called plates, move and change shape
Scientific TheoryA system of ideas that EXPLAINS many related observations and is supported by a large body of evidence acquired through scientific investigation
Continental DriftThe hypothesis that a single large landmass broke up into smaller landmasses to form the continents, which
PangaeaThe supercontinent that formed 300 million years ago and that began to break up 200 million years ago
Continental CrustThis crust is thicker and less dense than oceanic.
Oceanic CrustEarths crust located under the ocean that is usually thinner but more dense than continental crust
Subduction ZoneBoundaries where one plate sinks beneath another plate
VolcanoesA vent or fissure in Earth's surface through which magma and gases are expelled
Convection CurrentsAny movement of matter that results from differences in density; may be vertical, circular, or cyclical
MagmaThe molten or partially molten rock material containing trapped gases produced under the Earth's surface
LavaMagma that flows onto Earth's surface; the rock that forms when lava cools and solidifies
Convergent BoundaryThe boundary between tectonic plates that are colliding
Divergent BoundaryThe boundary between two tectonic plates that are moving away from each other
Transform BoundaryThe boundary between tectonic plates that are sliding past each other horizontally
FaultA break in a body of rock along which one block moves relative to another
EarthquakesA movement or trembling of the ground that is caused by a sudden release of energy when rocks along a fault move
Mid-ocean RidgesA long, undersea mountain chain that forms along the floor of the major oceans
tectonic platesSections of the Earth's crust that move due to convection currents.
Densitymass/volume
LithosphereA rigid layer made up of the uppermost part of the mantle and the crust. Consists of the moving earth plates.
ocean trenchA steep, long depression in the deep-sea floor that runs parallel to a chain of volcanic islands or a continental margin
rift valleyA deep valley that forms where two plates move apart, new crust is made here
AsthenosphereThe soft layer of the mantle on which the tectonic plates move
Heat Flow in the EarthHeat is convected out of the core then conducted through the mantle then convected to the plates (lithosphere)
Alfred WegenerGerman meteorologist who developed the idea of continental drift



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