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Plate Movement

TermDefinition
Crust Earth's outer layer; The coolest and least dense layer of Earth. See also core , mantle
mantle The layer of Earth beneath the crust . It is about 2,900 km (1,800 mi) thick , and makes up about 83 percent of Earth's interior. See also core and crust
outer core a liquid layer, approximately 2,200 km (1,367 miles) thick, composed mainly of iron and nickel, located between Earth's mantle and inner core
inner core the solid, innermost layer of Earth, acting as a, "planet within a planet" at the planet's center
latitude the distance north or south of equator is measured in degrees . See also longitude
longitude The distance east or west of the prime meridian in Greenwich , England; measured in degrees . See also latitude
oceanic ridge a continuous, 65,000–80,000 km long underwater mountain range formed by plate tectonics, where tectonic plates diverge and magma rises to create new seafloor
sea-floor spreading a geological process where tectonic plates pull apart at mid-ocean ridges, allowing magma to rise from the mantle, harden, and create new oceanic crust
divergent boundary a linear feature where two tectonic plates move apart, creating a "constructive" boundary that forms 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 one another, neither creating nor destroying lithosphere
subduction the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate.
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 tom plate tectonics , is pushed by movement in the asthenosphere
lithosphere the rigid outer part of the earth, consisting of the crust and upper mantle
fracture the cracking or breaking of a hard object or material.
elasticity the ability of a material to return to its original shape after deformation or the measure of how sensitive one economic variable is to changes in another
stress the body’s natural, automatic reaction to challenges, demands, or threats
strain force (a part of one's body or oneself) to make a strenuous or unusually great effort.
plate boundary the edges where Earth's tectonic plates meet
continental crust the relatively thick part of the earth's crust that forms the large landmasses. It is generally older and more complex than the oceanic crust.
oceanic crust the relatively thin part of the earth's crust which underlies the ocean basins. It is geologically young compared with the continental crust and consists of basaltic rock overlain by sediments.
friction the resistance that one surface or object encounters when moving over another.
rift valley a large elongated depression with steep walls formed by the downward displacement of a block of the earth's surface between nearly parallel faults or fault systems.
Created by: user-2013421
 

 



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