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Difference between revisions of "v0.31:Olivine"

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==Real-World Information==
 
==Real-World Information==
Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)<sub>2</sub>SiO<sub>4</sub>, it is defined by it's bright green color, gem quality examples of the mineral are known as [[Peridot]], an igneous intrusive stone comprised almost entirely of Olivine is called Peridotite (which is not present in Dwarf Fortress), and when Olivine is subjected to metamorphism in a low heat, high pressure environment, for example, in a subduction zone (where one tectonic plate slides underneath another tectonic plate) it becomes the mineral [[Serpentine]].
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Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)<sub>2</sub>SiO<sub>4</sub>, it is defined by it's bright green color; gem quality examples of the mineral are known as [[Peridot]]; an igneous intrusive stone comprised almost entirely of Olivine is called Peridotite (which is not present in Dwarf Fortress); and when Olivine is subjected to metamorphism in a low heat, high pressure environment, for example, in a subduction zone (where one tectonic plate slides underneath another tectonic plate) it becomes the mineral [[Serpentine]].
  
 
{{rocks}}
 
{{rocks}}

Revision as of 01:03, 20 April 2010

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.

Items built in Olivine will be Green.

Olivine is one of many worthless minerals that are Template:L, and can be used for floodgates and mechanisms used for the controlling of magma.

Real-World Information

Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)2SiO4, it is defined by it's bright green color; gem quality examples of the mineral are known as Peridot; an igneous intrusive stone comprised almost entirely of Olivine is called Peridotite (which is not present in Dwarf Fortress); and when Olivine is subjected to metamorphism in a low heat, high pressure environment, for example, in a subduction zone (where one tectonic plate slides underneath another tectonic plate) it becomes the mineral Serpentine.

Template:Rocks