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Chapter 17 voCaB!@#
voculary
| Question | Answer |
|---|---|
| which proposed that earth's continents had once been joined as a single landmass that broke apart. | Continental Drift |
| ancient landmass made up of all the continents that began to break apart about 200 mya. | Pangaea |
| device used to map the ocean floor that detects small changes in magnetic fields. | Magnetometer |
| when Earth's magnetic field changes polarity between normal and reversed. | magnetic reversal |
| study of Earth's magnetic record using data gathered from iron-bearing minerals in rocks that have recorded the orientation of Earth's magnetic field at the time of their formation. | paleomagnetism |
| imaginary line on a map that shows points of the same age, formed at the same time. | isochron |
| the hypothesis that new ocean crust is formed at mid-ocean ridges and destroyed at deep-sea trenches; occurs in a continuous cycle of magma intrusion and spreading. | seafloor spreading |
| are huge pieces of crust and rigid upper mantle that fit together at their edges to cover Earth's surface. | tectonic plate |
| regions where two tectonic plates are moving apart. | divergent boundary |
| when continental crust begins to separate, the stretched crust forms a long, narrow depression. | rift valley |
| two tectonics are moving toward each other. | convergent boundary |
| when two plates collide, the denser plate eventually descends below the other, less-dense plate. | subduction |
| a region where two plates slide horizontally past each other. | transform boundary |
| weight of the uplifted ridge is thought to push the oceanic plate toward the trench formed at the subduction zone. | ridge push |
| the weight of a subducting plate pulls the trailing slab into the subduction zone. | slab pull |