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Editing Stone layers
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Further down, as things get hotter still, rocks melt into [[magma]], which may get forced upwards, filling and often widening cracks. If the magma escapes the heat, it may cool and harden while still underground, forming the [[igneous intrusive]] ("fiery [[inside]]") rocks. If the magma rises all the way up to the surface and is expelled by a [[volcano]], we call it lava. The lava cools down into [[igneous extrusive]] ("fiery [[outside]]") layers, which in DF replace the sedimentary layers in some [[biome]]s near volcanoes. | Further down, as things get hotter still, rocks melt into [[magma]], which may get forced upwards, filling and often widening cracks. If the magma escapes the heat, it may cool and harden while still underground, forming the [[igneous intrusive]] ("fiery [[inside]]") rocks. If the magma rises all the way up to the surface and is expelled by a [[volcano]], we call it lava. The lava cools down into [[igneous extrusive]] ("fiery [[outside]]") layers, which in DF replace the sedimentary layers in some [[biome]]s near volcanoes. | ||
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{{Category|Stone Layers|*}} | {{Category|Stone Layers|*}} | ||
[[ru:Stone layers]] | [[ru:Stone layers]] |