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Science Chapter 9

Terms

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plate tectonics
theory that pieces of the lithosphere are in constant motion (because of convection currents)
convective flow
motion of matter resulting from convection
paleomagnetism
preserved in the sequence of lava flows at oceanic ridges
pangaea
supercontinent of all land with continents that joined together over time, the name means "all land". The large landmass that was once all of the continents connected together.
seafloor spreading
process by which plate tectonics produces new oceanic lithosphere
convergent boundary
two plates move together resulting in the oceanic lithosphere plunging beneath an overridingplate, and descending into the mantle
continental drift
Wegener's hypothesis proposed that the continents changed position on Earth's surface
plate
divided lithosphere segements that move and change shape
divergent boundary
two plates that move apart resulting in upwelling of material from the mantle to create new seafloor
subduction zone
destructive plate margins where one oceanic plate is forced down into the mantle beneath a second plate
oceanic ridge
longest physical feature on earth; formed by seafloor elevation along well developed divergent boundaries
transform-fault boundary
margins where two plates grind past each other without the production or destruction of lithosphere
ridge-push
causes oceanic lithosphere to slide down the sides of the oceanic ridge
slab-pull
primary downward armof convective flow in the mantle
continental volcanic arc
volcanic activity that is caused by the subduction of oceanic lithosphere

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