v50 Steam/Premium information for editors
- v50 information can now be added to pages in the main namespace. v0.47 information can still be found in the DF2014 namespace. See here for more details on the new versioning policy.
- Use this page to report any issues related to the migration.
This notice may be cached—the current version can be found here.
Difference between revisions of "Igneous extrusive layer"
Jump to navigation
Jump to search
m (Interwiki link) |
|||
| Line 20: | Line 20: | ||
<small>* See also: [[stone found everywhere]]</small> | <small>* See also: [[stone found everywhere]]</small> | ||
| − | ==In | + | ==In Real Life== |
| − | In real world | + | 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}} | {{stones}} | ||
{{Category|Stone Layers}} | {{Category|Stone Layers}} | ||
[[ru:Igneous extrusive layer]] | [[ru:Igneous extrusive layer]] | ||
Revision as of 13:43, 27 April 2019
v50.14 · v0.47.05 This article is about the current version of DF.Note that some content may still need to be updated. |
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 with the caveat that it is magma-safe, and obsidian is... unique.
Igneous extrusive layers
Stone found in igneous extrusive layers
- Hematite (veins)
- Native copper (veins)
- Galena (veins)
- Cinnabar (veins)
- Brimstone (small clusters)
- Realgar (small clusters)
- Orpiment (small clusters)
- Stibnite (small clusters)
- Magnetite (small clusters)
- Native aluminum (small clusters)
- Alunite (large clusters)
Stone appearing in both igneous intrusive and igneous extrusive layers
- Native gold (veins)
- Cobaltite (veins)
- Pyrolusite (small clusters)
- Hornblende (small clusters)
Gems found in igneous extrusive layers
- Turquoise (small clusters)
Gems appearing in both igneous intrusive and igneous extrusive layers
- 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
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 | |||||
|---|---|---|---|---|---|
| Igneous |
| ||||
| 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 | ||||