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magnesite

File:Magnesite-121892.jpg · Wikimedia Commons · See Wikimedia Commons

EntityQ425450· pop 52· linked from 291 articles

Also known as giobertite, carbonate magnesium, magnesium carbonate, magnesium(II) carbonate

Magnesite is a mineral with the chemical formula (magnesium carbonate). Iron, manganese, cobalt, and nickel may occur as admixtures, but only in small amounts. Magnesite occurs naturally in both cryptocrystalline and crystalline forms depending on the conditions of formation.

Key facts

Mineral.name
Magnesite
Mineral.category
Carbonate mineral
Mineral.image
Magnesite-121892.jpg
Mineral.imagesize
260px
Mineral.caption
Magnesite crystals from Brazil (11.4 × 9.2 × 3.6 cm)
Mineral.formula
MgCO3
Mineral.IMAsymbol
Mgs
Mineral.strunz
5.AB.05
Mineral.system
Trigonal
Mineral.class
Hexagonal scalenohedral (m)H-M symbol: ( 2/m)
Mineral.symmetry
Rc
Mineral.color
Colorless, white, pale yellow, pale brown, faintly pink, lilac-rose
Mineral.habit
Usually massive, rarely as rhombohedrons or hexagonal prisms
Mineral.cleavage
[101] perfect
Mineral.fracture
Conchoidal
Mineral.tenacity
Brittle
Mineral.mohs
3.5–4.5
Mineral.luster
Vitreous

via Wikipedia infobox

~11 min read

Encyclopedic overview

10 sections
Contents
  • Occurrence
  • Formation
  • Isotopic evidence
  • Uses
  • Refractory material
  • Other uses
  • Artworks
  • Occupational safety and health
  • United States
  • References

Magnesite is a mineral with the chemical formula (magnesium carbonate). Iron, manganese, cobalt, and nickel may occur as admixtures, but only in small amounts. Magnesite occurs naturally in both cryptocrystalline and crystalline forms depending on the conditions of formation.

Magnesite is used in the production of magnesium oxide for the refractory lining of kilns and furnaces, as well as artistically in jewelry and sculpture. Since it may be formed by carbonation of magnesium serpentine, there have also been efforts to use magnesite for carbon sequestration.

Excerpted from Wikipedia’s “magnesite” article, available under the CC BY-SA 4.0 licence.

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