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chapterten
plate tectonics
| Question | Answer |
|---|---|
| continental drift | hypothesis that continents drifted across the ocean basins |
| Weneger | scientist that proposed the continental drift theory, but could not explain the force behind plate movement |
| convection currents | the force responsible for plate movement |
| mid-ocean ridge | landform created when two oceanic plates diverge |
| magnetic reversals | the alternating pattern of earth's magnetic field found in rocks near a mid-ocean ridge |
| volcanic mountain range | landform created when an oceanic plate is subducted beneath a continental plate |
| sea-floor spreading | the process where rising magma at mid-ocean ridges produces new crust |
| divergent | plate boundary where plates are moving apart |
| convergent | plate boundary where plates are moving together |
| transform | plate boundary where plates move sideways past each other |
| subduction zone | area on Earth's crust where one plate plunges down under another plate; produces a trench |
| oceanic crust | high density crust, made of rock similar in composition to basalt |
| continental crust | low density crust, made of rock similar in composition to granite |
| terrane accretion | lithospheric pieces becoming part of a continent at a convergent boundary |
| folded mountain range | landform created when two continental plates collide |
| lithosphere | the solid, outer layer of the Earth, consisting of the crust and the upper part of the mantle |
| Pangaea | the supercontinent that formed about 300 mya when all Earth's landmasses were joined together |
| island arc | landform created when one oceanic plate subducts beneath another oceanic plate |
| plate tectonics | theory that explains why and how continents move, and is the study of major landforms on Earth's surface |
| asthenosphere | the solid, plastic layer of the mantle beneath the lithosphere, which allows plates to move on top of it |