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Earth Science - Pangaea / continental drift

AB
pressurethe amount of force pushing on a surface or area
crustthe layer of rock that forms Earth's outer surface
mantlethe layer of hot, solid material between Earth's crust and core
lithospherea rigid layer made up of the uppermost part of the mantle and the crust. One of the four spheres into which scientists divide Earth
asthenospherethe soft layer of the mantle on which the lithosphere floats
outer corea layer of molten iron and nickel that surrounds the inner core of Earth
inner corea dense sphere of solid iron and nickel in the center of Earth
convectionthe transfer of heat bymovements of a fluid
convection currentthe movement of a fluid, caused by differences in temperature, that transfers heat from one part of the fluid to another
Pangaeathe name of the single landmass that broke apart 225 million years ago and gave rise to today's continents
continental driftthe hypothesis that the continents slowly move across Earth's surface
fossilthe preserved remains or traces of living things
mid-ocean ridgethe undersea mountain chain where new ocean floor is produced; a divergent plate boundary
sonara system that determines the distance of an object under water by recording echoes of sound waves; gets its name from sound navigation and ranging
sea-floor spreadingthe process by which molten material adds new oceanic crust to the ocean floor
deep-ocean trencha deep valley along the ocean floor through which oceanic crust slowly sinks toward the mantle
subductionthe process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary
platea section of the lithosphere that slowly moves over the asthenosphere, carrying pieces of continental and oceanic crust
scientific theorya well-tested concept that explains a wide range of observations
plate tectonicsthe theory that pieces of Earth's lithosphere are in constant motion, driven by convection currents in the middle



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