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Name Earth and Space Science Course 320 Date Unit 2 Vocabulary Plate Tectonics crust solid, rocky outer layer of Earth mantle solid middle region of Earth inner core solid iron/nickel center of Earth.

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The movement of the plates creates three types of tectonic boundaries: convergent, where plates move into one another; divergent, where plates move apart; and transform, where plates move sideways in relation to each other.

Several basic principles underlie the theory of plate tectonics. Key concepts include: the lithosphere and the asthenosphere; "plates"; convection; the observation that the most active geology takes place on plate boundaries; and the Wilson Cycle, a concept that describes lifecycles of oceans and continents.

There are seven major plates: African, Antarctic, Eurasian, Indo-Australian, North American, Pacific and South American.

A tectonic plate (also called lithospheric plate) is a massive, irregularly shaped slab of solid rock, generally composed of both continental and oceanic lithosphere.

Divergent boundaries -- where new crust is generated as the plates pull away from each other. Convergent boundaries -- where crust is destroyed as one plate dives under another. Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other.

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