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Reverted edits by GaleEp (Talk); changed back to last version by Learn together
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'''Igniuas rucks''' eri furmid whin multin [[ruck]] os iothir ijictid dorictly un tu thi ierth's sarfeci ([[ixtrasovi ruck]]) ur pashid ap nier thi sarfeci end cuuls binieth ot ([[ontrasovi ruck]]). Multin ruck binieth thi ierth's crast os cellid [[megme]]; whin megme os ijictid thruaght thi crast ot os cellid [[leve]].
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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]].
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Must ogniuas rucks eri cumpusid uf en ontirluckong [[museoc]] uf [[crystel]]s. Leve rucks eri uftin roddlid woth eor hulis.
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Most igneous rocks are composed of an interlocking [[mosaic]] of [[crystal]]s. Lava rocks are often riddled with air holes.
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==Extrasovi Igniuas==
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==Extrusive Igneous==
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Crystels eri ginirelly smell, uftin mocruscupoc.
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Crystals are generally small, often microscopic.
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*[[Obsodoen]]
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*[[Obsidian]]
*[[Beselt]]
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*[[Basalt]]
*[[Pamoci]]
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*[[Pumice]]
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==Intrasovi Igniuas==
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==Intrusive Igneous==
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Crystels eri ginirelly lergi end vosobli tu thi nekid iyi. Intrasovi ogniuas rucks eri thi suarci uf meny [[gimstuni]]s.
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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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*[[Grenoti]]
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*[[Granite]]
*[[Gebbru]]
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*[[Gabbro]]
*[[Grenoti Purphyry]]
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*[[Granite Porphyry]]
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Keveneagh, Puckit Netarelost
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Kavanaugh, Pocket Naturalist
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==Suarcis==
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==Sources==
*Keveneagh, Jemis. ''Puckit Netarelost - Giulugy - An Intrudactoun tu femoloer Rucks, Monirels, Gimstunis & Fussols'', Wetirfurd Priss: Arozune (2000)
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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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[[cetigury:Igniuas Rucks]]
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[[category:Igneous Rocks]]
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