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earth's layers

Terms

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continental drift
thery that continents were once a one continent but have since drifted apart; Wegner
scientific theroy
well tested concep that explains a wide range of observations
lithosphere
uppermust part of mantle related to the crust.
convection
heat trannsfering through currents within a fluid
transform boundry
when two plates past eachother in opposite direction; neither goes under; earthquakes
panagea
literally super continent; all the continets were together
conduction
heat transfering through contact with other particles within the substance; spoon to soup
water's density
1
sonar
finding location of by recording echos of sound waves, sound navigation ranging
crust
layer of rock that forms earth's outer surface; 100; 32 KM; granite/basalt
plate tectonics
S.T stating that listosheric plates are in a slow constant motion driven by convection currents in the mantle
pressure
force exerted on a surface divided by the total area over which a force is exerted
divergent boundry
when two plates move opposide direction; mid ocean ridge/land
fault
breaks in the earth's lithosphere where rocks have slipped past eachother
mid ocean ridge
a range of mt. in the middle of the ocean; new ocean floor is produced
granite
rock that makes up most of the continental crust
rift valley
in middle of mid ocean ridge; where new ocean floor is made- sea floor spreading
plates
irregular shaped pieces of the lithosphere; slowly moving over sthenosphere carring crust (both)
deep ocean trench
deep valley along ocean floor; subduction takes place
outer core
liquid; iron and nickle; 2200c; 5150KM
convection current
transfer haet through change in temp.
fossil
a preservation of an acient organism in rock
density
measure of the mass in a volume of a substance
siesmic wave
vibrations that travel through earth cring the energy of an earthquake, indirect evidence to whats happening in the core
mantle
second layer of the earth 2200c; magnesium, oxegen, iron, silicon; 2900KM
subduction
recycling of crust; when old ocean floor plunges int oa deep ocean trench
athenosphere
below lithoshsphere, morphish, part of mantle, still solid
radiation
transfers heat through space by electromagnetic waves
inner core
soild; 6500c, 6500KM; dense circle
basalt
rock that makes up most of the ocean floor's crust
convergent boundry
plate boundry where 2 plates come towards one another; dencer one goes on bottom

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