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A theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates that move slowly over the underlying mantle.

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The gradual movement of the continents across the earth's surface through geological time.

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The sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate.

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A divergent tectonic plate or constructive plate boundary located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world

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A major area in the basin of the Pacific Ocean where a large number of earthquakes and volcanic eruptions occur

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The upper layer of the earth's mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur.

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Places where plates slide sideways past each other

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A region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle

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A linear feature that exists between two tectonic plates that are moving away from each other

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An extended break in a body of rock, marked by the relative displacement and discontinuity of strata on either side of a particular surface.