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Difference between revisions of "v0.31:Sedimentary layer"
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The name of a sedimentary layer appears white on the embark menu. | The name of a sedimentary layer appears white on the embark menu. | ||
− | Sedimentary layers are, on average, the most economically valuable of the four | + | Sedimentary layers are, on average, the most economically valuable of the four {{L|stone layers}}. They are your only source of {{L|bituminous coal}} and {{L|lignite}}, vital for fueling non-{{L|magma}} forges and for the {{L|coke}} {{L|steel}}-making requires (especially if you lack {{L|tree}}s). They are much richer in {{L|iron}} {{L|ore}}s than other rock formations. Several sedimentary rocks - {{L|dolomite}}, {{L|chalk}}, and {{L|limestone}} - are {{L|flux}}es, required for {{L|steel}}-making and also being twice as valuable as normal stone, making them useful for {{L|crafts|trade goods}} or {{L|furniture}}. |
(In real world geology, sedimentary {{L|stone}} is formed by sediment. The sediment collects in constantly growing heaps and the pressure at the bottom eventually forms the sediment into stone.) | (In real world geology, sedimentary {{L|stone}} is formed by sediment. The sediment collects in constantly growing heaps and the pressure at the bottom eventually forms the sediment into stone.) |
Revision as of 19:29, 24 October 2010
This article is about an older version of DF. |
Sedimentary stone layers contain Template:L, Template:L, Template:L, Template:L, Template:L, Template:L, and Template:L.
Template:L*, Template:L, Template:L, Template:L, Template:L*, Template:L*, Template:L, Template:L, Template:L, Template:L and Template:L layers are sedimentary.
- (* These also function as Template:L.)
The name of a sedimentary layer appears white on the embark menu.
Sedimentary layers are, on average, the most economically valuable of the four Template:L. They are your only source of Template:L and Template:L, vital for fueling non-Template:L forges and for the Template:L Template:L-making requires (especially if you lack Template:Ls). They are much richer in Template:L Template:Ls than other rock formations. Several sedimentary rocks - Template:L, Template:L, and Template:L - are Template:Les, required for Template:L-making and also being twice as valuable as normal stone, making them useful for Template:L or Template:L.
(In real world geology, sedimentary Template:L is formed by sediment. The sediment collects in constantly growing heaps and the pressure at the bottom eventually forms the sediment into stone.)
Sedimentary layers
Stone found in sedimentary layers
- Hematite (veins)
- Limonite (veins)
- Bituminous coal (veins)
- Lignite (veins)
- Gypsum (large clusters)
- Jet (large clusters)
- Petrified wood (small clusters)
- Magnetite (large clusters)
- Bauxite (large clusters)
- Kaolinite (large clusters)
- Saltpeter (small clusters)
Gems found in sedimentary layers
- Onyx (small clusters)
- Schorl (small clusters)
- Lace agate (small clusters)
- Bloodstone (small clusters)
- Moss agate (small clusters)
- Chrysoprase (small clusters)
- Sard (small clusters)
- Carnelian (small clusters)
- Banded agate (small clusters)
- Sardonyx (small clusters)
- Tube agate (small clusters)
- Fire agate (small clusters)
- Plume agate (small clusters)
- Brown jasper (small clusters)
- Picture jasper (small clusters)
- Yellow jasper (small clusters)
- Tigereye (small clusters)
- Tiger iron (small clusters)
- Clear tourmaline (small clusters)
- Gray chalcedony (small clusters)
- Dendritic agate (small clusters)
- White chalcedony (small clusters)
- Fortification agate (small clusters)
- Aventurine (small clusters)
- Indigo tourmaline (small clusters)
- Green tourmaline (small clusters)
- Red tourmaline (small clusters)
- Pink tourmaline (small clusters)
* See also: Template:L