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Geology: Plate Tectonics

Match the terms.

AB
geologistsscientists who study forces that shape Earth
constructive forcesbuild up mountains and landmasses
destructive forceswear away mountains and other features on Earth
crustlayer of rock that forms Earth's outer skin
mantlelayer of hot rock below crust
lithosphererigid layer of uppermost mantle and lower crust
asthenospheresoft layer of mantle, convection currents here move the plates
outer corelayer of molten metal around inner core
inner coredense ball of solid iron and nickel that spins, causing Earth's magnetic field
radiationtransfer of heat by electromagnetic waves
conductionheat transfer by direct contact with particles of matter
convectionheat transfer because of movement of heated fluids
Alfred Wegenerdeveloped the idea of continental drift
Pangaeasuper continent, one land
continental drifttheory that says the continents are slowly moving over Earth's surface
Evidence supporting Wegener's theoryevidence from landforms, from fossils, and from climate
Why scientists rejected Wegener's theoryHe could not explain the cause of the movement of the continents
mid-ocean ridgelongest mountain chain, continuous
sea-floor spreadingthe process occurring at mid ocean ridges that adds new material to the ocean floor
subductionprocess by which the ocean floor sinks beneath continental crust, forming a deep-ocean trench
plateslarge sections of the lithosphere that are moved by convection currents
plate tectonicsgeological theory that states pieces of Earth's lithosphere are in constant slow motion
faulta deformation of the Earth's crust that results in a break
transform boundaryplace where two plates slip past each other
divergent boundaryplace where two plates move apart
convergent boundaryplace where two plates come together or collide
land subsidenceoccurs when land sinks because of geologic process or human activities
foldcrustal deformation caused by compression that results in folded layers of rock
synclinea downward fold of rock
anticlinean upward fold of rock
Rift ValleyFormed by extensional stress
Island arcsformed by the subduction of oceanic crust below oceanic crust
fault block mountainsformed by land between two faults cause by extensional stresses

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