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Unit 3 Vocab Rachel
Plate Tectonics
| Term | Definition |
|---|---|
| Asthenosphere | The upper layer on the Mantel |
| Subduction | Where one tectonic plate goes beneath a other tectonic plate |
| Seafloor spreading | An educated guess that new new ocean crust if formed at mid-ocean ridges and then destroyed in deep sea trenches. It occurs in a cycle of magma and spreading. |
| Mantel convection | A motion on the solid mantel |
| Ridge push | The weight of an elevated plate pushes a oceanic plate into a subduction zone |
| Slab pull | A tectonic process when the convection currents in the mantel which pulls the trailing lithosphere into a subduction zone. |
| Lava | Melted rock on the outside of the Earths crust. |
| Magma | Melted rock on the inside of the Earths crust. |
| Tectonic Plate | large pieces of earths crust that cover its surface. |
| Theory of Continental drift | The theory of how all the continents were once all together. |
| Convergent boundary | Where two tectonic plates move together and can make things like trenches. |
| Divergent boundary | Where two tectonic plates move away which can make earthquakes. |
| Transform boundary | Where two tectonic plates slide horizontally past each other and can create shallow earthquakes. |
| Hot spot | Unusual hot areas in the earths mantel where plumes rise to the surface. |
| Epicenter | A point on the Earths surface that is directly above the focus on an earthquake. |
| Focus | The point where a earthquake originates from. |
| Pangaea | The name for when the all the continents where all together. |
| Geohazard | Where something geologically is very dangerous. |
| Reverse fault | Where one fault or wall moves up on another fault. |
| Strike-slip fault | This forms when rock's move past each other horizontally. |
| Normal fault | This occurs when a hanging wall moves down to the foothill. |
| Compression | A squeezing force that can cause intense deformation, folding, etc. |
| Tension | A stress that pulls rocks into 2 different directions. |
| Shearing | When brittle rocks can cause things like textures or fractures. |
| Felsic | Lighter igneous rocks. |
| Mafic | The ones that are classified as dark igneous rocks. |