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Plate Tectonics & CF
| Term | Definition |
|---|---|
| Asthenosphere | the soft layer of the mantle on which pieces of the lithosphere float |
| convergent boundary | the boundary between two colliding tectonic plates |
| divergent boundary | the boundary between two tectonic plates that are moving away from each other |
| inner core | the solid dense center of our planet that extends from the bottom of the outer core to the center of the Earth |
| lithosphere | the outermost rigid layer of Earth that consists of the crust and the rigid upper mantle |
| mantle | the layer of Earth between the crust and the core |
| ocean ridge | a long mountain chain that forms on the ocean floor where tectonic plates pull apart |
| mid-ocean ridge | a long mountain chain that forms on the ocean floor where tectonic plates pull apart |
| outer core | the liquid layer of Earth's core that lies beneath the mantle |
| Plate tectonic theory | the outermost layer of the Earth (lithosphere) is divided into contiguous sections (plates) that move relative to each other causing continental drift, seafloor spreading, and the formation of major physical features of the Earth’s surface |
| subduction zone | the region where two plates collide and one plate sinks below the other; Usually an oceanic plate sinks below a continental plate and down into the asthenosphere at a convergent boundary |
| transform boundary | the boundary between two tectonic plates that are sliding past each other horizontally |
| sea-floor spreading | the process by which new oceanic lithosphere is created at mid-ocean ridges as older material is pulled away from the ridges |