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Compositional Layers
Determined by their components (crust, mantle, core).
Oceanic Crust
Portion of Earth's crust, usually below the oceans, thinner and higher in density that continental crust, and basaltic rather than granitic in composition. 0-7km thick.
Lithosphere
Includes the crust and uppermost mantle. Its average thickness is 100km but ranges from about 75km beneath ocean basins to about 125km under the continents. Temperatures range from 300-500 degrees Celsius.
Asthenosphere
The upper layer of the earth's mantle, plastic and partly molten, in which convection is thought to occur, about 350km thick. Average temperature of 1,800 degrees Celsius.
Inner Core
A dense sphere of solid iron and nickel at the center of Earth. Up to 7,000 degrees Celsius.
P waves
A type of seismic wave that compresses and expands the ground. The fastest; (6-8 km/s) they are the first to arrive.
S waves
A type of seismic wave that moves the ground up and down or side to side. Also known as shear waves, slower than P Waves.
Surface Waves
Most destructive, travel in the Earth’s surface, and are the slowest to arrive.