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Plate Boundaries
| Term | Definition |
|---|---|
| Plate Tectonics | Theory that the lithosphere is divided into tectonic plates that slowly move on top of the asthenosphere. |
| Convection Currents | A cyclical motion occurs because of density differences in the mantle. Hotter rock rises, cooler rock sinks. This motion moves the plates. |
| Convergent boundary | Occurs when two tectonic plates move toward each other and collide. |
| Divergent boundary | The boundary between two tectonic plates moving away from each other. |
| Transform boundaries | Occurs when two tectonic plates slide past each other. |
| Fault | Any fracture or system of fractures in the crust. |
| Subduction | The process in which a denser plate is pushed downward beneath a less dense plate when plates converge; occurs at continental / oceanic boundaries and oceanic / oceanic boundaries. |
| Trench | A deep and narrow depression in the seafloor where the subducted plate moves into the asthenosphere. |
| Rift valley | A low region formed between continental plates on a divergent boundary where the plates separate. |
| Mid-ocean ridge | Underwater mountain range created when magma rises between two tectonic plates at a divergent boundary. |
| Volcano | Forms at some convergent boundaries, both continental/oceanic and oceanic/oceanic |
| Earthquake | A sudden movement of Earth's crust caused by the release of stress accumulated along geologic faults or by volcanic activity. |
| volcanic island arc | A series of volcanoes formed at a subduction zone where oceanic crust and oceanic crust meet at a convergent boundary. |