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| Earth's surface is divided into a few large, thick plates that move slowly and change in size. |
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| idea that continents move freely over Earth's surface, changing their positions relative to one another. |
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| a hypothesis that the sea floor forms at the crest of the mid oceanic ridge, then moves horizontally away from the ridge crest toward an oceanic trench. |
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aparent movement of the poles
ancient poles were in different positions than the present poles. |
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| sliding of the sea floor beneath a continent or island arc |
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| a circulation pattern driven by the rising of hot material and the sinking of cold material |
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| a large, mobile slap of rock that is part of earth's surface. |
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| plates are composed of this relatively rigid outer shell of Earth |
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| a zone of low seismic wave velocity that behaves in a ductile manner because of increased temperature and pressure |
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| boundary between plates that are moving apart |
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| convergent plate boundary |
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| lies between plates that are moving toward each other |
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| one at which two plates move horizontally past each other |
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| portion of fracture zone between two offset portions of ridge crest |
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| curved line of volcanoes that form a string of islands parallel to the oceanic trench |
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| both island arcs at sea and for belts of igneous activity on the edges of continents |
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| narrow columns of hot mantle rock that rise through the mantle, much like smoke rising from a chimney |
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