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40d:Stone
Stone or rock is a naturally occuring solid aggregate of minerals. It sometimes leaves behind material after being mined or collapsing. Other types of minable tiles include soil and sand.
Stone is divided into a few key categories:
- Metal ore: stone that produces metal bars when smelted
- Rough gems: rough gems can be cut, then used to encrust objects and create windows.
- Other stone: Stone that is not an ore or a gem. Few of these have a use outside of items and structures. (Obsidian is one exception).
Economic stones are types of stone that can be reserved for a special purpose. For ores, this is smelting and for fluxes, this is steel production. Bituminous coal and lignite can be reserved for making coke.
Having created loose stone, many times you'll want to get rid of it or at least move it someplace else. See stone management for advice.
This article is about DF geology and the distribution of stones, and does not contain the specific locations of metal ores or gems.
Main layer types
There are four types of stone layers (all others are soil). The type of layer is the primary indicator of what kind of ore you will find on the map, as well as a sign of volcanic activity. The types are sedimentary layers, igneous intrusive layers, igneous extrusive layers, and metamorphic layers.
The primary types of rock only occur in their own layers. (e.g. you won't find limestone in a marble layer.)
Stones forming entire layers
These types of stone occur as entire layers, containing some veins and pockets of other minerals (see below). If one of the following types of stone is present on your map, it will be listed in one of the biomes on the embark screen.
Sedimentary | Igneous intrusive | Igneous extrusive | Metamorphic |
---|---|---|---|
|
Other Stone
Stones found on this table will occur as pockets and veins inside their respective stone layers (see above). When your miners encounter one of them, the game will pause and you will receive an announcement; even for the ones that have no use other than to build constructions of unusual colors. Note that the veins or clusters can spread into other layers, and may cause some layers to contain stones they usually wouldn't.
Non-layer stone occurs in these forms:
- Large cluster - An oval that occupies nearly half of a 48x48 block, area-wise. Only one appears per block. These average 750 stones each.
- Vein - A sinuous line of the material crosses the block. These average 100 stones each.
- Small cluster - A sprinkle of 1 to 9 adjacent tiles. Multiple small clusters of different materials may be in the same block. These average 5 stones each and do not span more than three tiles in each direction.
The following table does not contain ores and gems. The types of stone listed here that do not link to their own article are generic.v0.28.181.40d
Icons | Name | Found in | Found how |
---|---|---|---|
^ ● | Alabaster | Gypsum | Small clusters |
` ● | Alunite | All Igneous extrusive, Kaolinite | Large clusters |
v ● | Anhydrite | Gypsum, Satinspar, Alabaster, Selenite | Single |
+ ● | Bauxite | All Sedimentary | Large clusters |
☼ ☼ | Bituminous coal | All Sedimentary | Veins |
` ● | Borax | Gypsum, Rock salt | Small clusters |
% ● | Brimstone | All Igneous extrusive, Gypsum | Small clusters |
" ● | Calcite | Limestone, Marble | Small clusters |
= ● | Chromite | Olivine | Veins |
£ * | Cinnabar | All Igneous extrusive, Shale, Quartzite | Veins |
£ * | Cobaltite | All Igneous All Metamorphic | Veins |
- ● | Cryolite | Granite | Small clusters |
o ● | Graphite | Gneiss, Quartzite, Marble, Schist | Small clusters |
# ● | Gypsum | All Sedimentary | Large clusters |
" ● | Hornblende | All Igneous, All Metamorphic | Small clusters |
. ● | Ilmenite | Gabbro | Small clusters |
░ ● | Jet | All Sedimentary | Large clusters |
= ● | Kaolinite | All Sedimentary | Large clusters |
% ● | Kimberlite | Gabbro | Veins |
* ● | Lignite | All Sedimentary | Veins |
% ● | Marcasite | Kaolinite | Small clusters |
v ● | Mica | All Metamorphic, Granite | Large clusters |
% ● | Microcline | All Stone | Large clusters |
% ● | Olivine | Gabbro | Large clusters |
- ● | Orpiment | All Igneous extrusive | Small clusters |
% ● | Orthoclase | All Igneous intrusive, All Metamorphic | Large clusters |
, ● | Periclase | Marble | Small clusters |
% ● | Petrified wood | All Sedimentary | Small clusters |
* ● | Pitchblende | Granite | Small clusters |
Θ ● | Puddingstone | Conglomerate | Large clusters |
% ● | Pyrolusite | All Igneous | Small clusters |
% ● | Realgar | All Igneous extrusive | Small clusters |
` ● | Rutile | All Metamorphic, Granite | Small clusters |
x ● | Saltpeter | All Sedimentary | Small clusters |
- ● | Satinspar | Gypsum | Small clusters |
; ● | Selenite | Gypsum | Small clusters |
≈ ● | Serpentine | Olivine | Small clusters |
% ● | Stibnite | All Igneous extrusive | Small clusters |
= ● | Sylvite | Rock salt | Large clusters |
| ● | Talc | Dolomite | Large clusters |
DF Geology and real-world Geology
The geology and stones of Dwarf Fortress are based on real-world geology and mineralogy. To understand the terms used here, you may want to crack open a geology textbook (a high school one should suffice). If you don't happen to have one close by, the Wikipedia articles for geology, mineralogy, or the terms in question might help.