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What Is The Theory That Explains How Large Pieces Of Earth's Outermost Layer Move And Change Shape

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F4: Plate Tectonics-Vocabulary

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chaff the sparse and solid outermost layer of the Earth to a higher place the drapery
mantle the layer of rock betwixt the Globe'due south crust and core
core the central part of the Globe below the drape
lithosphere the solid, outer layer of the Earth that consists of the crist and the rigid upper function of the pall
asthenosphere the soft layer of the mantle on which the tectonic plates motion
mesosphere the strong, lower office of the mantle between the asthenosphere and the outer core
tectonic plate a block of lithosphere that consists of the crust and the rigid, outermost part of the mantle
continental drift the hypothesis that states the continents once formed a single landmass, broke upwards, and drifted to their nowadays locations
sea-flooring spreading the process by which new oceanic lithosphere forms every bit magma rises torward the surface and solidifies
plate tectonics the theory that explains how big pieces of the Earth'south outermost layer, called tectonic plates, move and change shape
convergent purlieus the purlieus formed past the collision of ii lithospheric plates
divergent purlieus the boundary between two tectonic plates that are moving away from each other
transform boundary the boundary between the tectonic plates that are sliding past each other horizontally
compression stress that occurs when forces act to squeeze an object
tension stress that occurs when forces deed to stretch an object
folding the bending of rock layers due to stress
mistake a break in a torso of rock along which one block slides relative to another
uplift the rising of regions of the Earth's crust to higher elevations
subsidence the sinking of regions of the Globe'due south crust to lower elevations


Mrs. Martindale

St. James Catholic School

Millstadt, IL
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