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earth's interior vocabulary

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Question
Answer
Crust   The thin rocky layer of the earth  
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Mantle   The 280-kilometer thick layer of the earth located below the crust  
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Core   The innermost layer of the earth, located beneath the mantle;  
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Asthenosphere   A weak plastic layer of the mantle situated below the lithosphere; The rock within this zone is easily deformed; it allows the tectonic plates to move due to its plasticity  
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Mesosphere   The layer of the atmosphere immediately above the stratosphere and characterized by decreasing temperatures with height  
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Lithosphere   The rigid outer layer of the earth, including the crust and upper mantle  
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Seismic wave   Waves produced by an earthquake; used to study the earth's interior.  
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S-wave   A seismic wave that shakes particles perpendicular to the direction the wave is traveling  
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P-wave   Earthquake wave that pushes and pulls rocks in the direction of the wave; also known as a compression wave.  
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Shadow zone   An area in which an S-wave is not detected due to it not being able to pass through the outter layer  
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Density   less dense toward surface of earth; Mass per unit volume of a substance, usually expressed as grams per cubic centimeter; increases with depth into the earth  
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Pressure   increases from the Earth's surface toward the core; the continuous physical force exerted on or against an object by something in contact with it.  
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Temperature   a measure of the average kinetic energy of individual atoms or molecules in a substance.  
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Convection   The transfer of heat by the movement of heated matter; currents form in mantle when heated material becomes less dense and rises then cools off and falls  
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Plasticity   Asthenosphere is an example of this; due to increased pressure solids are moveable (like plastic)  
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Radiation   The transfer of energy through space by electromagnetic waves  
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Magnetosphere   the reigon surrounding the earth or another astromical body in which magnetic field is the predominant effective magnetic field.  
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inner core   solid Ni and Fe  
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outer core   liquid Fe & S  
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Earth's magnetic field   caused by spinning of liquid outer core  
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tectonic plate movement   thought to be caused by convection currents in the mantle  
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oceanic crust   igneous rock, 7 km thick, 3 g/cm3 density, younger than continental crust  
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continental crust   granitic rock, 8-75 km thick, 2.7 g/cm3 density, older than oceanic crust  
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seismic wave velocity   speeds up as it enters the mantle, slows down when it reaches the outer core--a liuid (s waves stop and p waves bend), speeds up again as it enters the inner core (due to solid again)  
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asthenosphere   layer that allows the tectonic plates to move  
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Created by: tboever17
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