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Unit Test Three H plate tectonics, earthquakes, and volcanoes

AB
Alfred WegenerGerman meteorologist
Earth's magnetic fieldreverses its polarity periodically
South America and AfricaTwo continents that strongly demonstrate the "jigsaw" fit
lithosphererigid layer made of crust and upper mantle
Earthquakesthese may occur when the elastic limit of rocks is passed
rift valleyWhen magma flows through the fissure created by continental plates moving apart
Pangaeathe name of the supercontinent that began breaking apart close to 200 million years ago
San Andreas Faulta noteable transform fault located on land
magmahot molten material beneath Earth's surface
Hot spotsstationary plumes of magma rising in the middle of a plate
Shield volcanoesbroad dome-shaped volcanoes Volcanoes covering the largest area.
Quiet volcanoestype of eruptions produced by magma that is low in silica (basaltic), low in viscosity, and hotter
Asthenospherethe weaker plastic region of the upper mantle
continental volcanic arcsAndes, and Cascades are prime examples of these type of volcanic mountains
Continental to continental convergenceThe Appalachians, Alps, and Himalayas were formed by this type of convergence
hot spot plumesthe site of most intraplate (within the plate) volcanic activity
paleomagnetismancient magnetic fields preserved in rocks
trenchformed at the subduction zone directly above the point of subduction
HawaiiPrime examples of shield volcanoes are located here
explosive eruptionstype of explosions produced from lava that is high in silica, high viscosity, and cooler
subduction zoneformed by oceanic lithosphere going down into the asthenosphere and maked by an ocean trench
Plate tectonicsthe theory that explains the movements, collisions, and destruction of the Earth's lithosphere
convectionthe process by which hot material from deep within the Earth rises while cooler material sinks


NC

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