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Difference between revisions of "v0.31:Igneous intrusive layer"
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'''Igneous intrusive stone layers''' can consist of {{L|granite}}, {{L|diorite}}, or {{L|gabbro}}, all of which typically contain {{L|gold}} and {{L|tetrahedrite}}. | '''Igneous intrusive stone layers''' can consist of {{L|granite}}, {{L|diorite}}, or {{L|gabbro}}, all of which typically contain {{L|gold}} and {{L|tetrahedrite}}. | ||
Revision as of 11:40, 26 December 2010
| This article is about an older version of DF. |
Igneous intrusive stone layers can consist of Template:L, Template:L, or Template:L, all of which typically contain Template:L and Template:L.
Gabbro can also contain Template:L (the ore of Template:L), Template:L (which may contain Template:Ls), and Template:L (which may contain Template:L). Granite can contain Template:L (the ore of Template:L), Template:L (the ore of Template:L), and Template:L (the ore of lead, plus a 50% chance of silver).
Igneous intrusive layers
Stone found in igneous intrusive layers
- Orthoclase (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 intrusive layers
- Lapis lazuli (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: Template:L
In the real world
Igneous intrusive Template:L is formed by magma solidification occurring below the surface, as opposed to Template:L stone which forms above the surface of the earth.