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Chapter 17 Voab
Section 1-4
| Question | Answer |
|---|---|
| Continental drift | Wegener's hypothesis that Earth's continents were joined as a single landmass, called Pangaea, that broke apart about 200 mya and slowly moved to their present positions. |
| pangaea | ancient landmas smade up of all the contents that began to break apart about 200 mys. |
| Magnetometer | device used to map the ocean floor that detects small changes in magnetic fields. |
| Magnetic reversal | when earth's magnetic field changes polarity from normal to reversed |
| Palcomagnetism | study of earth's magnetic record using data gathered from iron-bearing minerals in rock s that have recorded the orientation of earth's magnetic fields at the time of their formation. |
| isochron | imaginary line on a map that shows points of the same age formed at the same time |
| seafloor spreading | the hypothesis that new ocean crust is formed at mid-ocean ridges and destroys at deep-sea trenches occurs in a continuous cycle of magma institution and spreading. |
| tectonic plates | huge pieces of earth's crust that cover it surface and fit together at their edges. |
| divergent boundaries | Place where two of Earth's tectonic plates ate moving apart is associated with volcanic earthquakes and high heat flow and is found primarily on the seafloor. |
| rift valley | long narrow depression that forms when continental crust begins to separate at a divergent voundary |
| convergent boundaries | place where two tectonic plates are moving toward each other is associated with trench s islands arcs and folded mountains |
| subduction | process by which one tectonic plate slips beneath another tectonic plate. |
| transform boundary | Place where two tectonic plates slide horizontally past each another is characterized by long faults and shallow earthquakes. |
| ridge push | tectonic process associated with convection currents in earth's mantle that occurs when the weight of an elevated ridge pushes an oceanic plate toward a subjection zone. |
| slab pull | tectonic process associated with convection current in earth's mantle that occurs as the weight of the subduction plate pulls the trailing lithosphere into a subduction zone. |