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Editing Semi-molten rock

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[[File:Semimolten.jpg|thumb|300px|right|Not as <del>cool</del> <ins>hot</ins> as full-blown lava...]]
 
[[File:Semimolten.jpg|thumb|300px|right|Not as <del>cool</del> <ins>hot</ins> as full-blown lava...]]
'''Semi-molten rock''' (SMR), represented by the tile {{Tile|░|4:0:1}}, is a unique type of obstacle generally found at the bottommost edges of [[Magma sea|great magma seas]]. Anywhere that [[magma]] is found rests on layer after layer of semi-molten rock, with no normal material to be found beneath it.  There is also a layer near the bottom of the map composed almost entirely of semi-molten rock even where magma does not overlie it. Freestanding formations are possible, though less common.<!--- ? is this true ? --->  Though its name suggests the rock is hot, it is not dangerous to nearby [[Dwarf|dwarves]]. SMR acts as a barrier, and cannot be mined through by conventional means, nor smoothed. Unlike magma, SMR does not react with [[water]], producing no [[steam]] or [[obsidian]].
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'''Semi-molten rock''' (SMR), represented by the tile {{Tile|░|4:0:1}}, is an unique type of obstacle generally found at the bottommost edges of [[Magma sea|great magma seas]]. Anywhere that [[magma]] is found rests on layer after layer of semi-molten rock, with no normal material to be found beneath it.  There is also a layer near the bottom of the map composed almost entirely of semi-molten rock even where magma does not overlie it. Freestanding formations are possible, though less common.<!--- ? is this true ? --->  Though its name suggests the rock is hot, it is not dangerous to nearby [[Dwarf|dwarves]]. SMR acts as a barrier, and cannot be mined through by conventional means, nor smoothed. Unlike magma, SMR does not react with [[water]], producing no [[steam]] or [[obsidian]].
  
 
The top of semi-molten rock, or its ''floor'' when observed from the layer above, is described as a [[magma flow]], appearing in blue text when examined with the Loo{{K|k}} cursor and resembling a river of magma slowly flowing to the south (just like it did in [[23a:magma flow|older versions]]).
 
The top of semi-molten rock, or its ''floor'' when observed from the layer above, is described as a [[magma flow]], appearing in blue text when examined with the Loo{{K|k}} cursor and resembling a river of magma slowly flowing to the south (just like it did in [[23a:magma flow|older versions]]).

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