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| − | '''Igneous rocks''' are formed when molten [[rock]] is either ejected directly on to the earth's surface ([[extrusive rock]]) or pushed up near the surface and cools beneath it ([[intrusive rock]]). Molten rock beneath the earth's crust is called [[magma]]; when magma is ejected throught the crust it is called [[lava]].
| + | Page Corrected by Anon. |
| − | | + | Anon is legion. Anon does not forgive. Anon does not forget. |
| − | Most igneous rocks are composed of an interlocking [[mosaic]] of [[crystal]]s. Lava rocks are often riddled with air holes.
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| − | ==Extrusive Igneous==
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| − | Crystals are generally small, often microscopic.
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| − | *[[Obsidian]]
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| − | *[[Basalt]]
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| − | *[[Pumice]]
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| − | ==Intrusive Igneous==
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| − | Crystals are generally large and visible to the naked eye. Intrusive igneous rocks are the source of many [[gemstone]]s.
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| − | *[[Granite]]
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| − | *[[Gabbro]]
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| − | *[[Granite Porphyry]]
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| − | Kavanaugh, Pocket Naturalist
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| − | ==Sources==
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| − | *Kavanaugh, James. ''Pocket Naturalist - Geology - An Introduction to familiar Rocks, Minerals, Gemstones & Fossils'', Waterford Press: Arizona (2000)
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| − | [[category:Igneous Rocks]]
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