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Volcanoes and Earthquakes - Jordan R.

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Question
Answer
continental drift   Wegener's hypothesis that all continents were once connected in a single large landmass that broke apart about 200 million years ago and driften slowly to their current positions  
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Pangaea   large, ancient landmass that was composed of all the continents joined together  
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seafloor spreading   Hess's theory that new seafloor is formed when magma is forced upward toward the surface at a mid-ocean ridge  
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plate techtonics   theory that Earth's crust and upper mantle are broken into plates that float and move around on a plasticlike layer of the mantle  
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plate   a large section of Earth's oceanic or continental crust and rigid upper mantle that moves around on the asthenospere  
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lithosphere   rigid layer of Earth about 100 km thick, made fo the crust and a part of the upper mantle  
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asthenosphere   plasticlike layer of Earth on which the lithospheric plates float and move around  
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convection current   current in Earth's mantle that transfers heat in Earth's interior and is the driving force for plate techtonics  
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earthquake   vibrations produced when rocks break along a fault  
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primary waves   seismic wave that moves rock particles back-and-forth in the same direction that the wave travels  
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secondary waves   seismic wave that moves rock particles at right angles to the direction of the wave  
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surface waves   seismic wave that moves rock particles up-and-down in a backward rolling motion and side-to-side in a swaying motion  
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epicenter   point on Earth's surface directly above an earthquake's focus  
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seismograph   instrument used to register earthquake waves and record the time that each arrived  
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volcano   opening in Earth's surface that erupts sulfurous gases, ash, and lava; can form at Earth's plate boundaries, where plates move apart or together, and at hot spots  
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vent   opening when magma is forced up and flows out onto Earth's surface as lava, forming a volcano  
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crater   steep-walled depression around a volcano's vent  
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hot spot   the result of an unusually hot area at the boundary between Earth's mantle and core that forms volcanoes when melted rock is forced upward and breaks through the crust  
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shield volcano   broad, gently sloping volcano formed by quiet eruptions of basaltic lava  
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cinder cone volcano   steep-sided, loosely packed volcano formed when tephra falls to the ground  
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composite volcano   volcano built by alternating explosive and quiet eruptions that produce layers of tephra and lava; found mostly wher Earth's plates come together and one plate sinks below the other (subduction)  
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tephra   bits of rock or solidified lava dropped from the air during an explosive volcanic eruption; range sin size from volcanic ash to volcanic bombs and blocks  
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Created by: Jordan Raver
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