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Difference between revisions of "DF2014:Stone layers"

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(→‎Igneous extrusive: clarified where IE layers can appear, was even true in 0.34.11)
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{{main|Metamorphic layer}}
 
{{main|Metamorphic layer}}
  
Contains a small variety of [[vein]] ores, as well as [[marble]], the one non-sedimentary flux. Metamorphic layers generally contain moderately valuable gems, and if the sedimentary layer (or and especially igneous extrusive layer) above contains no flux stone, it is a useful early target for exploration in the hopes of finding flux. It does lack weapon-quality [[ore]]s (containing only [[copper]] and [[silver]]).
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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. It does lack weapon-quality [[ore]]s (containing only [[copper]] and [[silver]]).
  
 
Common stone types: [[schist]], [[gneiss]]
 
Common stone types: [[schist]], [[gneiss]]
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{{main|Igneous intrusive layer}}
 
{{main|Igneous intrusive layer}}
  
This is the deepest and often the widest level, and leads directly into the [[magma]] sea. Gems here are generally the most valuable, on average. The most valuable of them all, colored diamonds, are found within [[faint yellow diamond]]s within [[kimberlite]] within [[gabbro]] layers.
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Igneous intrusive layers can appear at any level except the top-most or above any sedimentary, and the deepest and often the thickest layer will always be igneous intrusive, just above the [[magma]] sea or [[semi-molten rock]]. Gems here are generally the most valuable, on average, with the most valuable of them all, colored diamonds, found in [[kimberlite]] in [[gabbro]] layers.
  
 
Common stone types: [[granite]], [[gabbro]]
 
Common stone types: [[granite]], [[gabbro]]
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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).
+
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]]. 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.
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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|biomes]] near volcanoes.
  
 
{{Category|Stone Layers|*}}
 
{{Category|Stone Layers|*}}
 
[[ru:Stone layers]]
 
[[ru:Stone layers]]

Latest revision as of 11:48, 28 September 2023

This article is about an older version of DF.
A cliff walls with stone layers.

There are four types of stone layers in Dwarf Fortress, very much based on real-life geology (see below). Stone layers are roughly homogeneous layers of rock, composed of the same kind of stone, that usually contain different ores. Each stone layer has its distinct markers and qualities; sometimes a clear dividing line can be drawn between two biomes from the stone layers underneath, sometimes not. Digging deeper, or into another local biome, will reveal differences between the layers' contents and a progression from sedimentary down to igneous.

These changes are usually quite sharp; fifteen layers may be mostly quartzite, but the next thirty may be dominated by gabbro. Three-dimensional variance is planned for the future, but for now, changes between stone layers also mark changes in ore and gem content.

Soil[edit]

Main article: Soil

Most maps have one layer of soil at the very top, although this layer may actually run the gamut from completely non-existent to ten or more layers deep. Note that on mountainous terrain soil tends to accumulate near edges; thus you can have partial soil "layers" down the side of the mountain for quite a few z-levels.

Soil is important for three reasons: it is easily farmed (not requiring irrigation like stone does), it is easily mined (taking less time than stone), and it does not leave any loose stone behind when mined. Soil layers can contain clay and sand, if your biome has any, as well as a high chance of being an aquifer, if your biome has one. Soil layers do not contain ores or gems, and at least one layer of soil is necessary to easily establish farming. It's not recommended you establish your main fortress in soil, as it cannot be smoothed or engraved to make it visually appealing/more valuable.

Sedimentary[edit]

Main article: Sedimentary layer

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 fluxes 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.

Common stone types: sandstone, limestone, shale

Igneous extrusive[edit]

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 volcanoes; the biggest stumbling block is that its presence means that the biome rarely contains any flux.

Common stone types: basalt, rhyolite

Metamorphic[edit]

Main article: 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. It does lack weapon-quality ores (containing only copper and silver).

Common stone types: schist, gneiss

Igneous intrusive[edit]

Igneous intrusive layers can appear at any level except the top-most or above any sedimentary, and the deepest and often the thickest layer will always be igneous intrusive, just above the magma sea or semi-molten rock. Gems here are generally the most valuable, on average, with the most valuable of them all, colored diamonds, found in kimberlite in gabbro layers.

Common stone types: granite, gabbro

In real life[edit]

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.

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 biomes near volcanoes.