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plate movement

TermDefinition
Crust Earth's outer layer; the coolest and least dense layer of Earth. See also core, and mantle
mantle The layer of Earth beneath the crust. It is about 2,900 km thick
outer core a liquid, metallic layer of Earth, approximately 2,260–2,300 km (1,400–1,800 miles) thick, composed mainly of iron and nickel.
inner core Earth's deepest layer, a solid,5,000–6,000°C (up to 10,000°F) hot sphere at the planet's center, approximately 2,500 km (1,550 miles) wide
latitude The distance north or south of the equator measured in degrees.
longitude The distance east or west of the prime meridian in Greenwich, England; measured in degrees
oceanic ridge a continuous, 65,000-km long underwater mountain range formed by plate tectonics, where divergent plates move apart, allowing magma to rise and create new seafloor
sea-floor spreading a geologic process occurring at mid-ocean ridges where tectonic plates diverge, allowing magma from the mantle to rise, cool, and create new oceanic crust
divergent boundary occurs where two tectonic plates move apart, causing magma to rise from the mantle, solidify, and create new crust.
convergent boundary a location where two or more tectonic plates move toward each other and collide
transform boundary a tectonic plate boundary where two plates slide horizontally past each other, neither creating nor destroying lithosphere
subduction The process by which one plate of the lithosphere sinks and slides under another
ocean trench Long, deep formation on the ocean floor that develops where two tectonic plates are moving toward each other, and one is moving under the other
tectonic plate A piece of earth's crust that, according to plate tectonics, is pushed by movement in the asthenosphere
lithosphere The cool, solid outer shell of earth. It consists of the crust and the rigid uppermost part of the mantle and is broken up into segments, or plates
fracture The breakage of a rock into two or more pieces
elasticity The ability of rock to be stretched and then return to its original position once the stress has been removed
stress The amount of force being applied to a rock or surface
strain Change in volume, size, or shape that results from stress
plate boundary A place where pieces of the broken lithosphere meet. Boundary types include convergent, divergent, and transform
continental crust Crust that contains mostly land, ranging from 15 to 70 kilometers (9 to 43 miles) thick
oceanic crust Crust that lies beneath the ocean, ranging from 5 to 10 km thick
friction A force that opposes the motion of objects, which are in contact
rift valley The valley formed by a diverging plate boundary
Created by: user-2013416
 

 



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