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Editing Stone layers

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== Sedimentary ==
 
== Sedimentary ==
 
{{main|Sedimentary layer}}
 
{{main|Sedimentary layer}}
The [[sedimentary layer]] has an 80% chance of being the first stone layer that appears after any soil, including any [[lignite]] or [[bituminous coal]], if you are lucky enough to have some. [[Iron]] [[ore]] and all but one of the [[flux]]es is common here as well, making the sedimentary layer make-or-break for [[steel]] production. Note that this layer and the igneous extrusive are mutually exclusive, and will never be found in one place. Sedimentary layers are generally where the bulwark of the fortress will find itself, will contain most of the ores marked on the [[embark]] screen as "shallow metals", and is a good choice for [[exploratory mining]].
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The [[sedimentary layer]] has an 80% chance of being the first stone layer that appears after any soil. It will include any [[lignite]] or [[bituminous coal]], if you are lucky enough to have some. [[Iron]] [[ore]] and all but one of the [[flux]]es is common here as well, making the sedimentary layer make-or-break for [[steel]] production. Note that this layer and the igneous extrusive are mutually exclusive, and will never be found in one place. Sedimentary layers are generally where the bulwark of the fortress will find itself, will contain most of the ores marked on the [[embark]] screen as "shallow metals", and is a good choice for [[exploratory mining]].
  
 
Note, however, that it is poor in [[gem]] content - those found in sedimentary layers are generally less valuable than those further down. Some types of sedimentary rock may contain an aquifer.
 
Note, however, that it is poor in [[gem]] content - those found in sedimentary layers are generally less valuable than those further down. Some types of sedimentary rock may contain an aquifer.
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{{main|Igneous extrusive layer}}
 
{{main|Igneous extrusive layer}}
  
In certain regions, igneous extrusive layers replace the sedimentary layers, but when present, are not limited to the topmost layers, and can appear anywhere except the bottom-most layer. Although being made of different rocks, they are similar to sedimentary layers, with the exception being that they often indicate the presence of [[magma]] above the [[magma sea]] itself. This is always the topmost layer near [[volcano]]es; the biggest stumbling block is that its presence means that the biome rarely contains any flux.
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In certain regions, igneous extrusive layers replace the sedimentary layers, but when present are not limited to the top-most layers and can appear anywhere except the bottom-most layer. Although being made of different rocks, they are similar to sedimentary layers, with the exception being that they often indicate the presence of [[magma]] above the [[magma sea]] itself. This is always the topmost layer near [[volcano]]es; the biggest stumbling block is that its presence means that the biome rarely contains any flux.
  
 
Common stone types: [[basalt]], [[rhyolite]]
 
Common stone types: [[basalt]], [[rhyolite]]
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{{main|Metamorphic layer}}
 
{{main|Metamorphic layer}}
  
Can appear at any level, except the bottom-most layer, or above any sedimentary layer. Contains a small variety of [[vein]] ores, moderately valuable gems, and possibly can be [[marble]], the one non-sedimentary flux stone. Less likely to provide iron than sedimentary, containing only small clusters of hematite or magnetite.
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Can appear at any level except the bottom-most layer or above any sedimentary layer. Contains a small variety of [[vein]] ores, moderately valuable gems, and possibly can be [[marble]], the one non-sedimentary flux stone. Less likely to provide iron than sedimentary, containing only small clusters of hematite or magnetite.
  
 
Common stone types: [[schist]], [[gneiss]]
 
Common stone types: [[schist]], [[gneiss]]
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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]].
 
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 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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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]]s near volcanoes.
  
 
== See Also ==
 
== See Also ==

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