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Difference between revisions of "v0.34:Olivine"

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(Importing content from v0.31 (0979/1015))
 
 
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Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)<sub>2</sub>SiO<sub>4</sub>.
 
Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)<sub>2</sub>SiO<sub>4</sub>.
 
It is defined by its bright green color. Gem-quality examples of the mineral are called [[peridot]].
 
It is defined by its bright green color. Gem-quality examples of the mineral are called [[peridot]].
 +
 +
It is also the most common rock in the world, taking up an estimated 80% of the world's volume, of course most of this is in the mantle 7km underground in the sea and an average 35km beneath the continent. Even dwarves can't dig that far down.
  
 
<gallery>
 
<gallery>
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File:Olivine-23909.jpg|Olivine, clear high quality crystals are called peridot if they are gem-quality
 
File:Olivine-23909.jpg|Olivine, clear high quality crystals are called peridot if they are gem-quality
 
File:Olivine (peridot).jpg|Another sample of olivine/peridot
 
File:Olivine (peridot).jpg|Another sample of olivine/peridot
File:Chryzolit (perydot, oliwin) - Kohestan, Pakistan. 02.jpg|Olivine/peridot
 
 
</gallery>
 
</gallery>
  
 
{{gamedata}}
 
{{gamedata}}
 
{{stones}}
 
{{stones}}

Latest revision as of 17:36, 18 January 2013

Olivine
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Uses

Location

  • Found within gabbro as large clusters
Properties
Fire-safe Magma-safe
Contains

Wikipedia article

This article is about an older version of DF.

Olivine is one of many low value minerals that are magma-safe, and can be used for floodgates and mechanisms used for the controlling of magma. It is also one of the few minerals that contains native platinum (the other being magnetite).

Items built using olivine will be dark green.

In the real world[edit]

Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)2SiO4. It is defined by its bright green color. Gem-quality examples of the mineral are called peridot.

It is also the most common rock in the world, taking up an estimated 80% of the world's volume, of course most of this is in the mantle 7km underground in the sea and an average 35km beneath the continent. Even dwarves can't dig that far down.

Sedimentary
Igneous
Intrusive
Extrusive
Metamorphic
Ore
Economic
Other