- 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 sea"
(Adamantine is highly likely on a 3x3 but only moderately common on a 2x2) |
(Rated article "Fine" using the rating script) |
||
| Line 1: | Line 1: | ||
| − | {{ | + | {{quality|Fine|08:00, 22 May 2010 (UTC)}}{{av}} |
| − | {{ | + | |
{{Minorspoiler}} | {{Minorspoiler}} | ||
Revision as of 00:38, 22 July 2010
| This article is about an older version of DF. |
 This article or section contains minor spoilers. You may want to avoid reading it.
|
The Magma sea is a large, multi-level 'sea' of magma that expands across the entire world. These can typically be found by around Z level -120 (though this seems to vary wildly (minimum -5 maximum -450 z level)[Verify]. The magma sea is always found below the last Cavern level.
It is not uncommon to find multiple z-levels of pillars of Template:L in the magma sea (in fact, it's almost guaranteed in a 3x3 embark square).
In addition, around and under the magma sea is Template:L. Which is impassible. There is Template:L however; Template:L, actually.
Any natural rock walls collapsed onto the magma sea (I believe onto the semi-molten rock, to be precise) vanishes[Verify], as if it fell out of the bottom of the map. Gone. Forever. Only thing that's left is some dust and magma mist.