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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 |