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38 Cards in this Set

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