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Igneous rocks are formed when liquid rock (magma underground, or lava on the surface) cools down and solidifies. If cooling is slow, usually underground, the minerals have time to form large, visible crystals, e.g. in granite. If cooling is faster, on the surface of the Earth, the crystals can usually only be seen with a microscope. Occasionally, the lava cools extremely rapidly, for instance when lava hits cold water, and there is no time for any crystal formation. This results in a volcanic glass such as obsidian.

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