v50 Steam/Premium information for editors
- 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.
This notice may be cached—the current version can be found here.
Editing 40d Talk:Obsidian
Jump to navigation
Jump to search
Warning: You are not logged in.
Your IP address will be recorded in this page's edit history.
You are editing a page for an older version of Dwarf Fortress ("Main" is the current version, not "40d"). Please make sure you intend to do this. If you are here by mistake, see the current page instead.
The edit can be undone. Please check the comparison below to verify that this is what you want to do, and then save the changes below to finish undoing the edit.
Latest revision | Your text | ||
Line 41: | Line 41: | ||
:if by "technically" you mean "in real life", then... well, we don't have time to even start to scratch that surface. It's not magma-safe in the game, and that's all this wiki addresses. There are mods that change the melting temperatures of the stones in the game - see the "modding" subsection of the [[forums]].--[[User:Albedo|Albedo]] 05:16, 2 March 2010 (UTC) | :if by "technically" you mean "in real life", then... well, we don't have time to even start to scratch that surface. It's not magma-safe in the game, and that's all this wiki addresses. There are mods that change the melting temperatures of the stones in the game - see the "modding" subsection of the [[forums]].--[[User:Albedo|Albedo]] 05:16, 2 March 2010 (UTC) | ||
− | == | + | == Obsidian casing around pipes == |
− | I | + | |
+ | I have a magma pipe, and the obsidian is only 1 tile thick, consistently. No "2-5 tiles thick".--[[User:Albedo|Albedo]] 04:00, 20 April 2010 (UTC) | ||
+ | :Wrong namespace? This is for 0.28.181.40d. Though you're right about 0.31 - the obsidian is only 1 tile thick there. --[[User:Quietust|Quietust]] 04:15, 20 April 2010 (UTC) |