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inner core
soild core about 733 miles in diameter, made mostly of iron crystals
outer core
same elements as inner core, but liquid because it is under less pressure; about 1410 miles thick
mantle
mostly silicon and oxygen with some iron and magnesium; made of hot, dense magma (molten rock); thick and fluid like; about 1800 miles thick
crust
mainly oxygen, silicon, magnesium and iron, rigid solid layer, on average 5 miles (oceanic) to 25 miles thick (continental)
oceanic crust
about 70 to 180 million years old, 4-7 miles, mostly basalt, which has a dark, fine and gritty volcanic structure. it is formed out of liquid lava that quickly cools.
continental crust
3 billion years old; 20-25 miles, mostly igneous rock, the upper part is mostly granite rocks, while the lower part consists of basalt and diorite, lightly colored, coarse grain magma
lava
molten rock that has exited through an opening in the earth’s crust
igneous rock
rock solidified from cooled magma or lava or below the surface of the earth
erosion
the process that carries weathered rock, soil, and organic material from one place to another, for example, through wind, water, and glacial movement
sediment
accumulated organic and inorganic particles
magma
molten rock beneath earth’s surface
rift valley
a deep valley formed by the divergence of tectonic plates, often found at mid-ocean ridges or continental boundaries.
seafloor spreading
is the process by which new oceanic crust forms as magma rises to the surface / divergent boundaries
subducted
where one plate sinks beneath another
transform fault
a boundary where 2 plates slide past another
seasat
the first satellite for ocean studies
alvin
ocean submersible
sonde
slightly more complex than a ctd
goes
satellite type that orbits yet stays in place
jason2
the most recently launched low orbit satellite