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SLHS PLATE TECTONICS

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Question
Answer
theory proposed by Alfred Wegener that states that the continents were once joined as a super continent   Continental Drift  
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large, ancient landmass that was composed of all the continents joined together     Pangea  
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Hess's theory that new seafloor is formed when magma is forced upward toward the surface at a mid-ocean ridge     Seafloor Spreading  
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theory that Earth's crust and upper mantle are broken into plates that float and move around on a plasticlike layer of the mantle     Plate Tectonics  
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a large section of Earth's oceanic or continental crust and rigid upper mantle that moves around on the athenosphere   Plate  
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Large pieces of earth's crust   plates    
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Theory based on evidence that plates are moving slowly and constantly.     Theory of Plate Tectonics    
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Supercontinent     Pangea    
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Cracks between the plates     plate boundaries    
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force that acts on rock to change its shape or volume     stress    
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stress that pushes a mass of rock in two opposite directions     shearing    
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stress that squeezes rock until it folds or breaks     compression    
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stress force that pulls on the crust, stretching rock to become thinner   tension  
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shaking and trembling that results from the movement of rock beneath Earth's surface     earthquake    
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break in the Earth's crust where slabs of crust pass by each other     fault    
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Shearing creates this type of fault     slip-strike    
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Compression produces this type of fault     reverse    
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Tension forces in Earth's crust produce this type of fault     normal    
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Half the fault that lies above the fault     hanging wall    
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Half the fault that lies below the fault     footwall    
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bends in the rock     folds    
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large area of flat land elevated high above sea level     plateau    
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point beneath surface where rock is under stress and breaks     focus    
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point on surface directly above the focus     epicenter    
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first waves (compressional similar to a slinky)     p waves    
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secondary waves (move perpendicular to direction of movement)     s waves    
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move slower, but produce severe ground movements (making the ground roll like a water wave)   surface waves  
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Rates earthquakes according to intensity     Mercalli scale    
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a rating of the size of seismic waves measured by a seismograph     Richter scale    
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Scale used today by geologists     Moment Magnitude Scale    
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the theory that continents can drift apart from one another and have done so in the past     continental drift    
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the process by which new oceanic lithosphere is created at mid-ocean ridges as older materials are pulled away from the ridge     sea-floor spreading    
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the theory that the Earth's lithosphere is divided into tectonic plates that move around on top of the asthenosphere     plate tectonics    
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the boundary between two colliding tectonic plates     convergent boundary    
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the region where an oceanic plate sinks down into the asthenosphere at a convergent boundary, usually between continental and oceanic plates   subduction zone  
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the boundary between two tectonic plates that are moving away from each other     divergent boundary    
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the boundary between two tectonic plates that are sliding past each other horizontally     transform boundary    
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a break in the Earth's crust along which two blocks of the crust slide relative to one another     fault    
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the bending of rock layers due to stress in the Earth's crust     folding    
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the type of stress that occurs when an object is squeezed     compression    
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the type of stress that occurs when forces act to stretch an object     tension    
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the amount of force per unit area that is put on a given material     stress    
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a layer of hot rock     mantle    
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the part of the mantle that is made of soft rock that bends like plastic     asthenosphere    
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a dense ball of solid metal     inner core    
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the transfer of energy through empty space     radiation    
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heat transfer within a fluid     convection currents    
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the continents were once joined together in a single landmass     continental drift    
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the name of the supercontinent that existed millions of years ago     Pangaea    
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any trace of an ancient organism that has been preserved in rock     fossil    
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are found in all of Earth's oceans     mid-ocean ridges    
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technology used by scientists used in the mid-1900s to map the mid-ocean ridge     sonar    
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the process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle     subduction    
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the geological theory that states that pieces of Earth's lithosphere are in constant, slow motion     plate tectonics    
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forms at a divergent plate boundary     rift valley    
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molten material rises from the mantle and erupts along mid-ocean ridges     sea-floor spreading    
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produced by a collision between two pieces of continental crust at a converging boundary     mountain range    
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when you touch a hot pot or pan and energy moves from the pot to your hand     heat transfer    
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a place where two plates slip past each other, moving in opposite directions     transform boundary    
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Wegener's hypothesis taht all continents were once connected in a single large landmass that broke apart about 200 million years ago and drifted slowly to their current positions     Continental Drift    
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large, ancient landmass that was composed of all the continents joined together     Pangea    
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Hess's theory that new seafloor is formed when magma is forced upward toward the surface at a mid-ocean ridge     Seafloor Spreading    
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theory that Earth's crust and upper mantle are broken into plates that float and move around on a plasticlike layer of the mantle     Plate Tectonics    
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a large section of Earth's oceanic or continental crust and rigid upper mantle that moves around on the athenosphere     Plate    
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plasticlike layer of Earth on which the lithospheric plates float and move around     Asthenosphere    
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rigid layer of earth about 100 km thick made of the crust and a part of upper mantle     Lithosphere    
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current in Earth's mantle that transfers heat in Earth's interior and is the driving force for plate tectonics     Convection Current    
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vibrations produced when rocks break along a fault     Earthquake    
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seismic wave that moves rock particles back and forth in the same direction that the wave travels     Primary Waves    
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seismic wave that moves rock particles at right angles to the direction of the wave     Secondary Waves    
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seismic wave that moves rock particles up and down in a backward rolling motion and side to side in a swaying motion     Surface waves    
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point on earth's surface directly above an earthquake's focus     Epicenter    
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instrument used to register earthquake waves and record the time that each arrived     seismograph    
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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     volcano    
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opening where magma is forced up and flows out onto earth's surface as lava forming a volcano     vent    
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steep-walled depression around a volcano's vent     crater    
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the result of an unusually hot area at the boundary between earth's mantle and core that forms volcanoes when melted rock si forced upward and breaks through the crust     hot spot    
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broad, gently sloping volcano formed by quiet eruptions of basaltic lava     shield volcano    
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steep-sided, loosely packed volcano formed when tephra falls to the ground     cinder cone volcano    
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volcano built by atlernating explosive and quiet eruptions that produce layers of tephra and lava; found mostly where earth's plates come together and one plate sinks below the other     composite volcano    
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bits of rock or solidified lava dropped from the air during an explosive volcanic eruption; ranges in size from volcanic ash to volcanic bombs and blocks     Tephra    
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