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Casteel Erosion etc.
Casteel changing Earth
| Term | Definition |
|---|---|
| The crust is composed primarily of | rocky material. |
| The mantle is composed mostly of | solid rock with some molten rock. |
| The innermost layers are composed mostly of | iron and nickel. |
| Pressure and temperature | increase with depth beneath the surface. |
| Large continent-size blocks are called | plates |
| Most earthquakes and volcanoes are located at | the boundaries of the plates (faults). |
| when plates move together | convergent boundaries |
| when plates move apart | divergent boundaries |
| when plates slip past each other horizontally | transform boundaries, also called strike-slip or sliding boundaries |
| moving sediments to a new location | erosion |
| dropping sediments in a new location | deposition |
| Ring of Fire | The area of tectonic plates with the most amount of active volcanoes in the world. |
| Lava | This is magma outside of the Earth. |
| Pangaea | This is the theory of a "super continent", when the Earth was a single landmass. |
| mantle | The thickest layer of the Earth. |
| Earthquakes | Caused by shifting of tectonic plates usually at a transform boundary |
| Transform Faults | plates slide or slip past each other; cause earthquakes |
| volcanoes | Magma from the mantle comes out of these |
| Trenches | When convergent plates come together and push downward, these form. |
| Mountains | When convergent plates come together and push upward, these form. |
| Mid-ocean ridges | When divergent plates come apart, and magma seeps up, forming new crust. |
| faults | These are the boundary lines between tectonic plates. |
| Divergent Faults | plates move away from each other; Mid-ocean ridges and rift valleys are formed by these |
| Convergent Faults | plates move towards each other; cause mountains, volcanic arcs, and deep ocean trenches |