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The Dynamic Earth

A practice of concepts dealing with plate tectonics and the formations created by these processes.

AB
Divergent BoundaryWhen two plates move apart from one another.
Convergent BoundaryWhen two plates move towards one another.
Transform FaultWhen two plates slip past one another.
MountainsThese are formed when two continental plates collide.
VolcanoesThese are formed at convergent and divergent boundaries as well as hot spots.
LithosphereThe crust and the top part of the mantle. This area is ridgid and breaks into pieces called plates.
AsthenosphereThe putty like layer which consist of the bottom half of the mantle.
Inner coreA solid layer of the earth that consist of Iron and Nickle.
Outer coreA liquid layer of the earth that consist of Iron and Nickle.
MantleA plastic like layer of the earth that consist of Iron, Magnesium, Silcon, and Oxygen. This is the thickest layer.
CrustThe outer most layer of the earth.
PangaeaA supercontinent once thought to exist about 250 million years ago.
Continental Drift TheoryAlfred Wegener's theory that states there once was one supercontinent called Pangaea.
Sea-Floor SpreadingThe hypothesis that states molten material from the Earth's mantle is forced up to the surface at mid-ocean ridges and cools to form new seafloor.
MagnetometerThe tool used to take magnetic readings of the ocean floor igneous rocks and plotted the data on maps.
Plate tectonicsThe most current theory of how plates move.
North American PlateThe lithospheric plate that the North American continent is found on.
CaliforniaA location in the United States where the Juan de Fuca Plate and the North American Plate are sliding past one another. This create earthquake activity on the coast of this state.
Convection currentsThe currents caused by the rising of warm magma which cools and sinks. This is thought to be the mechanism behind plate movement.
GlossopterisA fossil fern found on many different continents. This was one of Wegener's bits of evidence for his Continental Drift theory.


Stephanie

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