- 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.
Sedimentary layer
This article was migrated from DF2014:Sedimentary layer and may be inaccurate for the current version of DF (v50.14). See this page for more information. |
v50.14 · v0.47.05 This article is about the current version of DF.Note that some content may still need to be updated. |
Sedimentary stone layers contain hematite, limonite, magnetite, tetrahedrite, bituminous coal, lignite, and gypsum.
Chalk*, chert**, claystone, conglomerate, dolomite*, limestone*, mudstone, rock salt, sandstone**, siltstone and shale layers are sedimentary.
- (* These also function as flux. **These are also magma-safe.)
Sedimentary layers are, on average, the most economically valuable of the four stone layers. They are your only source of bituminous coal and lignite, vital for fueling non-magma forges and for the coke steel-making requires (especially if you lack trees). They are much richer in iron ores than other rock formations. Several sedimentary rocks - dolomite, chalk, and limestone - are fluxes, required for steel-making and also being twice as valuable as normal stone, making them useful for trade goods or furniture.
Sedimentary layers can be tricky to locate. If you are starting off and you want access to an embark area with sedimentary layers, use the "Find Desirable Location" function before embark and set your parameters to include sites with flux stone. Since most flux stones are found in sedimentary layers, this will increase your chances that a suitable site will have sedimentary rock near the surface. Be careful when using the "Find Desirable Location" function as it will sometimes list green sites that have flux stone but it will not indicate that it does, actually, have flux stone.
(In real world geology, sedimentary stone 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)
- Cassiterite
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: stone found everywhere
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 |