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Earths' structure and Plate tectonics

AB
asthenosphereThe hot, plastic layer of the upper mantle below the lithosphere, extending some 350 to 650 kilometers (220 to 400 miles) below the surface. Convection currents within the asthenosphere power plate tectonics.
basaltThe relatively heavy crustal rock that forms the seabeds, composed mostly of oxygen, silicon, magnesium, and iron. Its density is about 2.9 g/cm3.
buoyancyThe ability of an object to float in a fluid by displacement of a volume of fluid equal to it in mass.
continental crustThe solid masses of the continents, composed primarily of granite.
continental driftThe theory that the continents move slowly across the surface of Earth.
convectionMovement within a fluid resulting from differential heating and cooling of the fluid. Convection produces mass transport or mixing of the fluid.
convergent plate boundaryA region where plates are pushing together and where a mountain range, island arc, and/or trench will eventually form; often a site of much seismic and volcanic activity.
divergent plate boundaryA region where plates are moving apart and where new ocean or rift valley will eventually form. A spreading center forms the junction.
echo sounderA device that reflects sound off the ocean bottom to sense water depth. Its accuracy is affected by the variability of the speed of sound through water.
faultA fracture in a rock mass along which movement has occurred.
hot spotA surface expression of a plume of magma rising from a stationary source of heat in the mantle.
lithosphereThe brittle, relatively cool outer layer of Earth, consisting of the oceanic and continental crust and the outermost, rigid layer of mantle.
magmaMolten rock capable of fluid flow; called lava above ground.
mantleThe layer of Earth between the crust and the core, composed of silicates of iron and magnesium. The mantle has an average density of about 4.5 g/cm3 and accounts for about 68% of Earth’s mass.
oceanic crustThe outermost solid surface of Earth beneath ocean floor sediments, composed primarily of basalt.
Pacific Ring of FireThe zone of seismic and volcanic activity that encircles the Pacific Ocean.
PangeaName given by Alfred Wegener to the original “proto- continent.” The breakup of Pangaea gave rise to the Atlantic Ocean and to the continents we see today.
plate tectonicsThe theory that Earth’s lithosphere is fractured into plates that move relative to each other and are driven by convection currents in the mantle. Most volcanic and seismic activity occurs at plate margins.
Richter scaleA logarithmic measure of earthquake magnitude. A great earthquake measures above 8 on the Richter scale.
magnetometerMeasures the amount of residual magnetism in a rock.
seafloor spreadingThe theory that new ocean crust forms at spreading centers, most of which are on the ocean floor, and pushes the continents aside. Power is thought to be provided by convection currents in Earth’s upper mantle.
seismographAn instrument that detects and records earth movement associated with earthquakes and other disturbances.
subductionThe downward movement into the asthenosphere of a lithospheric plate.
surface waveA wave that surges ashore without breaking.
transform faultA plane along which rock masses slide horizontally past one another.


High School Science teacher
Flanagan H.S.
Pembroke Pines, FL

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