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Editing DF2014:Stone layers

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== In real life ==
 
== In real life ==
  
Being modelled on basic geology, much of the way stone layers work in ''Dwarf Fortress'' also applies to our planet: At the surface of the world there's a thin covering of [[soil]], a soft mixture of minerals (the building blocks of stones), small rocks ([[sand]], [[silt]], [[clay]] etc.), liquids, living things and so on. Below that there's a [[sedimentary layer]] of stones; these are made of particles of minerals, organic detritus and other stuff, which, after tumbling around, end up settling down below ("sedimenting"). Those grains and particles are then glued together into new rocks ("cemented") by various processes; for example, by mineral growth of substances carried by water (similar to how stalactites grow).
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Being modelled on basic geology, much of the way stone layers work in ''Dwarf Fortress'' also applies to our planet: At the surface of the world there's a thin covering of [[soil]], a soft mixture of minerals (the building blocks of stones), small rocks ([[sand]], [[silt]], [[clay]] etc.), liquids, living things and so on. Below that there's a [[sedimentary layer]] of stones; these are made of particles of minerals, organic detritus and other stuff, which, after tumbling around, end up settling down below ("sedimenting"). Those grains and particles are then glued together into new rocks ("cemented") by various processes; for example, by mineral growth of substances carried by water (similar to how stalactites grow).
  
Below the sedimentary layer, the rocks are subjected to heat from below, and pressure, stretching etc. from the movement of continental plates. Those forces transform them into different kinds of rocks, called [[Metamorphic layer|metamorphic]].
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Below the sedimentary layer, the rocks are subjected to heat from below, and pressure, stretching etc. from the movement of continental plates. Those forces transform them into different kinds of rocks, called [[Metamorphic layer|metamorphic]].                                                        
  
Further down, as things get hotter still, rocks melt into [[magma]], which may get forced upwards filling and often widening cracks. If 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|biomes]] near volcanoes.
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Further down, as things get hotter still, rocks melt into [[magma]]. If magma escapes the heat, it may cool and harden while still underground, forming the [[igneous intrusive]] ("fiery [[inside]]") rocks. In DF, these form a layer below the metamorphic stones, but in real life they may form anywhere there are cracks for the magma to fill in.  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|biomes]] near volcanoes.
  
 
{{Category|Stone Layers|*}}
 
{{Category|Stone Layers|*}}
 
[[ru:Stone layers]]
 
[[ru:Stone layers]]

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