Inside Earth-Chapter 1

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Created by:

wwilk  on September 12, 2010

Description:

Includes all chapter 1 vocabulary and terms from the first earth science lecture (powerpoint)

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Inside Earth-Chapter 1

rotate
to move around an axis inside the object (internal axis); the axis can be real or imaginary
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rotate to move around an axis inside the object (internal axis); the axis can be real or imaginary
revolve to move around an axis outside the object (external axis); the axis can be real or imaginary
Protoplanet Hypothesis favored explanation for the formation of the solar system and our planet; rotating cloud of gas and dust, spins faster, 90% becomes Sun, 10 % becomes protoplanets, comets, meteors, and asteroids
crust thinnest, outer layer of the Earth; broken up into plates; "floats" on the asthenosphere; oceanic crust is made of basalt; continental crust is made of mostly granite
mantle below the crust; has 3 parts-upper, middle, and lower; largest layer; made of mostly silica, iron and magnesium
lithosphere consists of the earth's crust and the upper mantle
asthenosphere middle mantle; flows like hot asphalt; reason the crustal plates move (convection currents)
convection currents the repeating cycle of the rising and falling of the hot material in the mantle (asthenosphere); contributes to the movement of the crustal plates; the movement of fluid, caused by differences in temperature, that transfers heat from one part of the fluid to another
outer core the outer portion of the core of the Earth; in a liquid state; made of iron and nickel
inner core the very deepest part of the Earth; in a solid state, due to pressure; made of iron and nickel
seismic waves vibrations that travel through Earth carrying energy released during an earthquake
pressure the force exerted on a surface divided by the area over which the force is exerted
basalt a dark, dense, igneous rock with fine texture, found in oceanic crust
granite a usually light-colored igneous rock that is found in continental crust
radiation the transfer of energy through space
conduction the transfer of heat within a material or between materials that are touching
convection the transfer of heat by movement of a fluid
density the amount of mass in a given space; mass per unit volume
continental drift the hypothesis that the continents slowly move across Earth's surface
Pangaea the name of the single land mass that broke apart 200 million years ago
fossil a trace of an ancient organism that has been preserved in rock
mid-ocean ridge an undersea mountain chain where new ocean floor is produced; a divergent plate
sonar a device that determines the distance of an object under water by recording echos of sound waves
sea-floor spreading the process by which molten material adds new oceanic crust to the ocean floor
deep-ocean trench a deep valley along the ocean floor beneath which oceanic crust slowly sinks toward the mantle
subduction the process by which oceanic crust sinks beneath a deep ocean trench and back into the mantle at a converget plate boundary
plate a section of the lithosphere that slowly moves over the asthenosphere, carry pieces of continental and oceanic crust
scientific theory a well tested concept that explains a wide range of observations
plate tectonics the theory that pieces of Earth's lithosphere are in constant motion, driven by convection currents in the mantle
fault a break in the Earth's crust where masses of rock slip past one another
divergent boundary a plate boundary where two plates move away from each other
rift valley a deep valley that forms where two plates move apart
convergent boundary a plate boundary where two plates move toward each other
transform boundary a plate boundary where two plates move past each other in opposite directions

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