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Difference between revisions of "DF2014:Igneous extrusive layer"
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LethosorBot (talk | contribs) (LethosorBot moved page DF2014:Igneous extrusive layer to Igneous extrusive layer: Migrating v50 page (2145/4618) (content)) Tag: New redirect |
LethosorBot (talk | contribs) (Migrating v50 page (2145/4618) (content)) Tag: Removed redirect |
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+ | [[File:igneous_extrusive_preview.png|thumb|260px|right|Created when magma exits a volcano and cools above the Earth's surface.]]'''Igneous extrusive stone layers''' are formed from [[andesite]], [[basalt]], [[dacite]], [[obsidian]], and [[rhyolite]]. Of these five, andesite, dacite, and rhyolite are functionally identical, different only in appearance and name, basalt is like the other three except that it is magma-safe, and obsidian is... unique. | ||
+ | |||
+ | ==Igneous extrusive layers== | ||
+ | {{Layerlookup/layers|IGNEOUS_EXTRUSIVE}} | ||
+ | |||
+ | ==Stone found in igneous extrusive layers== | ||
+ | {{Layerlookup/stones|IGNEOUS_EXTRUSIVE}} | ||
+ | |||
+ | ====Stone appearing in both igneous intrusive and igneous extrusive layers==== | ||
+ | {{Layerlookup/stones|IGNEOUS_ALL}} | ||
+ | |||
+ | ==Gems found in igneous extrusive layers== | ||
+ | {{Layerlookup/gems|IGNEOUS_EXTRUSIVE}} | ||
+ | |||
+ | ====Gems appearing in both igneous intrusive and igneous extrusive layers==== | ||
+ | {{Layerlookup/gems|IGNEOUS_ALL}} | ||
+ | |||
+ | <small>* See also: [[stone found everywhere]]</small> | ||
+ | |||
+ | ==In Real Life== | ||
+ | In real-world geology, Igneous extrusive [[stone]] is formed by lava solidifying above the surface, open to the air. This is the main point of difference from [[igneous intrusive layer|igneous intrusive]] stone, which solidifies below the surface. This distinction is not kept in ''Dwarf Fortress'' geology, in which the difference is simply the name and contents of the two types of stone. | ||
+ | |||
+ | {{stones}} | ||
+ | {{Category|Stone Layers}} | ||
+ | [[ru:Igneous extrusive layer]] |
Latest revision as of 03:35, 20 December 2022
This article is about an older version of DF. |
Igneous extrusive stone layers are formed from andesite, basalt, dacite, obsidian, and rhyolite. Of these five, andesite, dacite, and rhyolite are functionally identical, different only in appearance and name, basalt is like the other three except that it is magma-safe, and obsidian is... unique.
Igneous extrusive layers[edit]
Stone found in igneous extrusive layers[edit]
- Hematite (veins)
- Native copper (veins)
- Galena (veins)
- Cinnabar (veins)
- Brimstone (small clusters)
- Realgar (small clusters)
- Orpiment (small clusters)
- Stibnite (small clusters)
- Native aluminum (small clusters)
- Alunite (large clusters)
Stone appearing in both igneous intrusive and igneous extrusive layers[edit]
- Native gold (veins)
- Cobaltite (veins)
- Pyrolusite (small clusters)
- Hornblende (small clusters)
Gems found in igneous extrusive layers[edit]
- Turquoise (small clusters)
Gems appearing in both igneous intrusive and igneous extrusive layers[edit]
- Black zircon (small clusters)
- Green zircon (small clusters)
- Red zircon (small clusters)
- Brown zircon (small clusters)
- Yellow zircon (small clusters)
- Clear zircon (small clusters)
* See also: stone found everywhere
In Real Life[edit]
In real-world geology, Igneous extrusive stone is formed by lava solidifying above the surface, open to the air. This is the main point of difference from igneous intrusive stone, which solidifies below the surface. This distinction is not kept in Dwarf Fortress geology, in which the difference is simply the name and contents of the two types of stone.
Sedimentary | |||||
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Igneous |
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Metamorphic | |||||
Ore | |||||
Economic | |||||
Other |
Alunite · Anhydrite · Bauxite · Borax · Brimstone · Chromite · Cinnabar · Cobaltite · Cryolite · Graphite · Hornblende · Ilmenite · Jet · Kimberlite · Marcasite · Mica · Microcline · Olivine · Orpiment · Orthoclase · Periclase · Petrified wood · Pitchblende · Puddingstone · Pyrolusite · Realgar · Rutile · Saltpeter · Serpentine · Slade · Stibnite · Sylvite · Talc |