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Difference between revisions of "Olivine"

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'''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]]).
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'''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 may contain veins of [[native platinum]] (the other being [[magnetite]]).
  
Items built using olivine will be dark green.
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Items built using olivine will be yellow.
  
==In the real world==
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==In real life==
 
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.
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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, most frequently as an olivine-rich ultramafic rock known as peridotite.
  
 
<gallery>
 
<gallery>
 
File:Green sand close up.jpg|Green sand, or fragmented olivine. Some fragments are loose and some are visibly still embedded in the black lava rock below
 
File:Green sand close up.jpg|Green sand, or fragmented olivine. Some fragments are loose and some are visibly still embedded in the black lava rock below
File:Mineral Olivino GDFL046.jpg|A small olivine piece
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File:Mineral Olivino GDFL046.jpg|Olivine crystals in peridotite
 
File:Olivine magnesium iron silicate Jackson County, North Carolina 3059.jpg|Brighter olivine
 
File:Olivine magnesium iron silicate Jackson County, North Carolina 3059.jpg|Brighter olivine
File:Olivijn.gif|Small olivine pieces
 
 
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

Latest revision as of 16:12, 3 May 2024

Olivine
OlivineSample.png
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Graphic
Olivine sprite.png
Uses

Location

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

Wikipedia article

This article is about the current version of DF.
Note that some content may still need to be updated.

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 may contain veins of native platinum (the other being magnetite).

Items built using olivine will be yellow.

In real life[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, most frequently as an olivine-rich ultramafic rock known as peridotite.

Sedimentary
Igneous
Intrusive
Extrusive
Metamorphic
Ore
Economic
Other