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Dynamic Earth, Chap3, Plate Tectonics

AB
fossilan imprint or mold of an ancient organism
Pangaeaa giant landmass that existed more than 200 million years ago
theory of continental driftthe continents were once joined together and have since drifted apart
mid-ocean ridgean undersea mountain range where new ocean floor is produced
ocean-floor spreadingold ocean floor is pushed away from the mid-ocean ridge by the formation of new ocen floor
Alfred Wegenerresponsible for the continent drift theory
trencha V-shaped valley on the ocean floor where the old ocean floor is subducted
subductionthe crust plunges back into the mantle and melts
theory of plate tectonicslinks the ideas of continental drift and ocean-floor spreading and explains how the Earth has changed over time
platea moving irregular slab that makes up the Earth's lithospere
tectonicsa branch of geology that deals with the movements that shpae the Earth's crust
lithospherethe topmost solid part of the Earth
divergent boundarya plate boundary where plates move apart
convergent boundarya plate boundaryat which plate come together or collide with one another
strike-slip boundarya plate boundary where two plates slip past one another horizontally
convection currenta movement of material caused by differences in temperature
Harry Hessdeveloped the theory of sea-floor spreading

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