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38 Cards in this Set
- Front
- Back
outside 'skin' of earth
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crust
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boundary between the Earth's crust and the mantle
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moho
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innermost part of earth-solid(nickel)
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inner core
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surrounding inner core; like a liquid, nickel
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outer core
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layer surrounding outer core; solid, but flows like a liquid
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mantle
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plasticity
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a solid that flows like a liquid
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which layer of earth exhibits plasticity?
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mantle
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oceanic crust is mostly made of...
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basalt
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continental crust is mostly made of...
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granite
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plate tectonics
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theory that pieces of earths lithosphere are in constant motion; driven by convection currents in mantle
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theory of plate tectonics is supported by...(7)
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fossil evidence, climate changes, shapes of continents, glacial grooves, coal deposits, rock type, convection currents
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movement of lithospheric plates is believed to be caused by...
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convection currents, difference in temp.
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convection currents are...
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movement of fluid caused by different temps, that transfers thermal energy from 1 part of fluid to another...hot rises, cool sinks
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pangaea
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single landmass that broke apart 225mil yrs ago & gave rise to today's continents
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sea floor spreading
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process by which molten material adds new oceanic crust to the ocean floor
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divergent boundary
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where 2 plates slide away from each other <>
mid ocean ridge |
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convergent boundary
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where 2 plates come together ><
mts & ocean trenches |
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transform boundary
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where 2 plates slide past each other ^>
san andreas |
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what happens when 2 cont. plates collide? example?
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mts form; himilaya mts
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earths history spans about...
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4.6bil yrs
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1st era in history? longest era?
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precambrian(both)
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principle of cross-cutting
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thing being cut is older than the thing cutting it
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principle of inclusions
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rock fragments within larger body of rock is older than the surrounding larger body of rock
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principle of superposition
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layer on bottom is oldest, layer on top is youngest
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principle of uniformitarianism
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present is key to past...erosion and deposition (today)
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principle of unconformities
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gaps in geologic record
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principle of original horizontality
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sedimentary layers are initially deposited in horizontal layers
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tension
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causes rocks to pull apart
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shearing
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causes rocks to slip past each other
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principle of unconformities
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gaps in the geologic record
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compression
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causes rocks to shorten; compressed together
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where is footwall and hanging wall in normal fault? what stress?
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fw-top, hw-bottom; tension
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where is footwall and hanging wall in reverse fault? what stress?
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fw-bottom, hw-top; compression
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topographic/contour map
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map showing different elevations of an area
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contour line
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lines connecting points of equal elevation
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contour interval
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elevation difference btwn adjacent contour lines
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how are lines like if a steep slope? gentle slope?
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close together; far apart
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how do you know which direction a river is flowing?
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arrow-like things point to the head of river (upstream)
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