- 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.
Difference between revisions of "v0.31:Magma"
(intro section) |
(forgot kilns; also, arrange in likely order of usage (smelters always come first)) |
||
| Line 1: | Line 1: | ||
{{ArticleVersion}} | {{ArticleVersion}} | ||
{{elven}} | {{elven}} | ||
| − | '''Magma''' is a red-hot liquid that wells up from deep within the earth - but not too deep to be found by dwarves. It serves as an energy source, powering {{L|magma forge}}s, {{L|magma glass furnace}}s and {{L|magma | + | '''Magma''' is a red-hot liquid that wells up from deep within the earth - but not too deep to be found by dwarves. It serves as an energy source, powering {{L|magma smelter}}s, {{L|magma forge}}s, {{L|magma glass furnace}}s, and {{L|magma kiln}}s, which do not "use it up" in any way. It is ''extremely'' dangerous, {{L|fun|and has led to the death of many dwarfs, and many fortresses}}. |
Magma never cools, but can {{L|evaporation|evaporate}} if left at a depth of 1/7 for long enough. If mixed with water it can form obsidian (see below). | Magma never cools, but can {{L|evaporation|evaporate}} if left at a depth of 1/7 for long enough. If mixed with water it can form obsidian (see below). | ||
Revision as of 20:01, 20 April 2010
| This article is about an older version of DF. |
Template:Elven Magma is a red-hot liquid that wells up from deep within the earth - but not too deep to be found by dwarves. It serves as an energy source, powering Template:Ls, Template:Ls, Template:Ls, and Template:Ls, which do not "use it up" in any way. It is extremely dangerous, Template:L.
Magma never cools, but can Template:L if left at a depth of 1/7 for long enough. If mixed with water it can form obsidian (see below).
Lava is the same substance. Magma is what it is called underground, while it is called lava if it is above ground.
Magma sea
The Magma sea is located at the bottom of every map, forming an (almost) impenetrable barrier. They also provide a great source of magma. Template:L can also be found around the magma sea, and cannot be dug through.
Magma pipes
Magma pipes are present in the new version of Dwarf Fortress as well. They can be found underground, however they rarely reach the upper z-levels (40+). Most end just a few z-levels above the magma sea, though some span up to more than 100 z-levels. Magma pipes seem to be always connected to a magma sea, and the sea and pipe can occasionally reach up to the same level, making them hard to separate. However, magma pipes can be identified by the obsidian walls which surround them. Magma pipes will slowly refill themselves, giving the player an infinite source of magma.
Volcanos
Volcanos can be found which extend all the way to the surface, but on a standard map they are exceedingly rare, if you even have any at all on your map.
Properties of magma
Magma behaves the same way as water with the exception of not being affected by Template:L, unless pressurized by a Template:L, and apparently not showing Template:L. Magma will turn into Template:L if it touches Template:L. Modding information: The rock that is used when magma mixes with water is the first rock encountered to have the [LAVA] tag during worldgen.
Dangers of magma
Magma is not immediately fatal when first touched. It is dangerous to stand in magma, but dwarves will generally only suffer minor burns when running from a flow. Most creatures can survive standing on even a completely filled magma tile for a single turn, but any more and they will likely die.