- v50 information can now be added to pages in the main namespace. v0.47 information can still be found in the DF2014 namespace. See here for more details on the new versioning policy.
- Use this page to report any issues related to the migration.
Difference between revisions of "Olivine"
m (Creating page for DF2014 (22/82)) |
(Added graphic.) |
||
(18 intermediate revisions by 13 users not shown) | |||
Line 1: | Line 1: | ||
− | {{ | + | {{Quality|Exceptional}} |
− | + | {{stonelookup/0 | |
+ | |graphic=olivine_sprite.png}} | ||
+ | {{av}} | ||
− | '''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 | + | '''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 | + | Items built using olivine will be yellow. |
− | ==In | + | ==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 | + | 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| | + | 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: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
| ||||||||||||||||||||||||||||||||||||
Graphic | ||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Uses | ||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
Location | ||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
Properties | ||||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
v50.14 · v0.47.05 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.
[INORGANIC:OLIVINE]
[USE_MATERIAL_TEMPLATE:STONE_TEMPLATE]
[STATE_NAME_ADJ:ALL_SOLID:olivine][DISPLAY_COLOR:2:7:0][TILE:'%']
[ENVIRONMENT_SPEC:GABBRO:CLUSTER:100]
[IS_STONE]
[MELTING_POINT:13168]
[SOLID_DENSITY:3320]
[STATE_COLOR:ALL_SOLID:YELLOW_GREEN] |
Sedimentary | |||||
---|---|---|---|---|---|
Igneous |
| ||||
Metamorphic | |||||
Ore | |||||
Economic | |||||
Other |
Alunite · Anhydrite · Bauxite · Borax · Brimstone · Chromite · Cinnabar · Cobaltite · Cryolite · Graphite · Hornblende · Ilmenite · Jet · Kimberlite · Marcasite · Mica · Microcline · Olivine · Orpiment · Orthoclase · Periclase · Petrified wood · Pitchblende · Puddingstone · Pyrolusite · Realgar · Rutile · Saltpeter · Serpentine · Slade · Stibnite · Sylvite · Talc |