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Difference between revisions of "v0.31:Microcline"

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:''You have struck microcline!''
  
You have struck Microcline!
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'''Microcline''' is one of the most common stone types found in Dwarf Fortress, showing up pretty much everywhere. Its distinct cyan color is shared only by [[raw adamantine]] and [[ice]].
  
==In-Game Information==
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==In Real Life==
Microcline is the only cyan colored stone except for raw adamantine (or ice, if you count it as a stone) and it is found in all stone layers.
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Microcline is the low-temperature form of alkali feldspar. It is a potassium aluminum silicate with a chemical formula of (KAlSi<sub>3</sub>O<sub>8</sub>). [[Orthoclase]] is a mineral of the same composition that forms at higher temperatures.
 
 
==Real-Life Information==
 
Microcline is the low-temperature form of alkali feldspar, it is a potassium aluminum silicate with a chemical formula of (KAlSi<sub>3</sub>O<sub>8</sub>). {{L|Orthoclase}} is a mineral of the same composition that forms at higher temperatures.
 
  
 
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Latest revision as of 17:10, 8 December 2011

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Uses

Location

Properties
Fire-safe Not magma-safe

Wikipedia article

This article is about an older version of DF.
You have struck microcline!

Microcline is one of the most common stone types found in Dwarf Fortress, showing up pretty much everywhere. Its distinct cyan color is shared only by raw adamantine and ice.

In Real Life[edit]

Microcline is the low-temperature form of alkali feldspar. It is a potassium aluminum silicate with a chemical formula of (KAlSi3O8). Orthoclase is a mineral of the same composition that forms at higher temperatures.

Sedimentary
Igneous
Intrusive
Extrusive
Metamorphic
Ore
Economic
Other