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Magma (molten rock) rises from feeders or volcanic necks beneath the surface of the crust and flows from volcanic openings onto the surface. When magma reaches the surface, it is called lava.

When lava reaches the surface, it immediately begins to cool. During this cooling phase, the liquid lava solidifies much as liquid water would freeze if cooled sufficiently. The solidification occurs because of the crystallization of minerals from chemical components (iron, magnesium, silicon, oxygen) in the lava. The lava will transition from a liquid to either a form of natural glass, or to a rock, depending on the speed at which it cools. Obsidian, a natural glass, and basalt, an extrusive igneous rock, are both formed from cooling lava.

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14y ago

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