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14 Cards in this Set
- Front
- Back
plate tectonics
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it describes continental movement but also proposes a possible explaination of why and how continents move. States: 1) Lithosphere broken into 30 plates
2) Plates dift ontop of convection Asthosphere |
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oceanic crust
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the crust that lies beneath. the meterial on the ocean floor makes the oceanic crust think 5-10 km thick and dense
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continental crust
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the crust that lies beneath continents. also material that makes up landmasses Dense and it is 32-70 km thick (thickest under mountains)
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lithosphere
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thin outer shell of the earth consisting of the crust and the rigid upper mantle 65-100 km thick
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asthenosphere
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zone of mantle beneath the lithosphere that consists of slowly flowing solid rock 200 km thick
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divergent boundary
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boundary formed by two lithospheric plates that are moving apart
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rift valley
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steap narrow valley formed as lithospheric plates separate
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convergen boundary
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boarder formed by the driect collision of two lithospheric plate
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subduction zone
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reigion where one lithospheric plate moves under another
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ocean trench
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deep valley in the ocean floor that forms along the subduction zone
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island arc
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chain of valcanic islands formed along in ocean trench resualts when one ocean plate subducts under a ocean plate Ex: japan
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transform fault boundary
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boundary formed where two lithospheric plates slide past each other Ex: San Andrea's Fault
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convection
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transfer of heat through the movement of fluid material hot rises and cool sinks
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convection current
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movement in a fluid caused by uneven heating
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