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Editing v0.34:Caverns

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Exploring the underground world, you may find a variety of special geographical features. When your dwarves discover a feature, an announcement window will let you know of it.
 
Exploring the underground world, you may find a variety of special geographical features. When your dwarves discover a feature, an announcement window will let you know of it.
  
'''[[Deep pit]]s:''' Deep pits are... deep pits, that connect one cavern level to the next.  They have a fixed shape. The top z-level, where the pit meets the next cavern level, is un-muddied rough rock floor where the normal space of the deep pit and the random rock spires of the cavern collide.
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'''Deep pits:''' Deep pits are... deep pits, that connect one cavern level to the next.  They have a fixed shape. The top z-level, where the pit meets the next cavern level, is un-muddied rough rock floor where the normal space of the deep pit and the random rock spires of the cavern collide.
  
 
If your map has an unseen [[cave-in]] at the beginning of embark, the caverns may have a deep pit somewhere. This occurs because some stone in the cavern above the deep pit is unsupported and falls down. This may be a bug.
 
If your map has an unseen [[cave-in]] at the beginning of embark, the caverns may have a deep pit somewhere. This occurs because some stone in the cavern above the deep pit is unsupported and falls down. This may be a bug.
  
'''[[Magma pool]]s:''' Despite the name, magma pools are not actual pools, but tubes extending up from the [[magma sea]]. Their shape is fixed and their presence random.  A magma tube might extend all the way to the top cavern, or merely a few z-levels. Magma pools can be distinguished from the magma sea even if they are only a single Z-level high due to two important features: they will always be walled by obsidian as opposed to the standard stone of the layer and, more importantly, will (very slowly) refill to their top if any magma is drained.
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'''Magma pools:''' Despite the name, magma pools are not actual pools, but tubes extending up from the [[magma sea]]. Their shape is fixed and their presence random.  A magma tube might extend all the way to the top cavern, or merely a few z-levels. Magma pools can be distinguished from the magma sea even if they are only a single Z-level high due to two important features: they will always be walled by obsidian as opposed to the standard stone of the layer and, more importantly, will (very slowly) refill to their top if any magma is drained.
  
 
'''[[Passage]]s:'''
 
'''[[Passage]]s:'''

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