Magnesite - Encyclopedia

    Class : Carbonates, nitrates, borates
    Subclass : Anhydrous carbonates
    Crystal system : Trigonal
    Chemistry : MgCO3
    Rarity : Common


Magnesite (or giobertite) is a carbonate of the calcite group. It forms a continuous series with siderite but not with calcite, since its CaO content does not exceed 6%. The intermediate terms of the magnesite - siderite series were formerly referred to as breunnerite and mesitine. Manganese, cobalt and nickel can also be present at low levels. Magnesite can result from different geological processes : alteration of magnesium-rich rocks (mainly serpentinites) by carbonate waters ; magnesium metasomatosis of limestones with passage through an intermediate stage of dolomitization ; more rarely evaporites. It is exceptional as a matrix for hydrothermal veins. It was named thus in reference to its chemical composition, the term magnesium itself comes from the Greek magnesia lithos (stone of Magnesia), Magnesia being a region of Thessaly in Greece. Transparent to translucent and usually vitreous in luster, magnesite has perfect cleavage according to {10-11}. It is colorless, white to bluish-white, sometimes yellow to brown, and forms compact to granular masses, or rhombohedra, more rarely hexagonal prisms. It is a common magnesium ore that was formerly used in pyrotechnics and photography. By calcination it produces magnesia (MgO). Magnesia is mainly used in the refractory industry, particularly for the interior linings of steel furnaces, and also in the chemical industry. Magnesite has additional uses in porcelain, ceramics, rubber, stationery and quick-setting cements. Finally, it should be noted that it is massive and is cut and polished into cabochons and trinkets and sold under the trade name "howlite" and "pinolite" (or chrysanthemum stone).

Main photo : Magnesite from Brumado, Bahia, Brazil © Rob Lavinsky

Magnesite from Brumado, Bahia, Brazil © Rob Lavinsky
Magnesite from Breitenau Mine, Styria, Austria © David J. Eicher
Magnesite from Kaswassergraben, Styria, Austria © Peter Neschen
Magnesite from the Bénesse-lès-Dax mine, Landes, France © Patrice Queneau

Magnesite in the World

Very good magnesite crystals are rare. Exceptional specimens come from Brumado (Bahia, Brazil): they are gem-like rhombohedra, slightly yellowish, sometimes measuring up to 30 cm on the edge, associated with talc. Magnesite was encountered in large, grayish-white, partially gem-like crystals at Oberdorf an der Laming (Styria, Austria). Serpentinites from Val Malenco (Lombardy, Italy) also produced good crystals reaching 15 mm.

Magnesite in France

In France, magnesite is known from the salt mine of Saint-Pandelon and the gypsum quarry of Bénesse-lès-Dax (Landes) which produced remarkable elongated crystals.

Twinning

Magnesite can present twins on {01-12}.

Pinolite cabochon or chrysanthemum stone (magnesite and graphite) from China
Howlite (magnesite) cabochon from Zimbabwe
Howlite dyed blue to imitate turquoise
Howlite dyed blue to imitate turquoise
Howlite nugget dyed blue to imitate turquoise
Howlite nugget dyed blue to imitate turquoise

Fakes and treatments

Massive magnesite sold under the name "howlite" is often dyed in various colors, notably blue to imitate turquoise.



Hardness : 3.5 to 4.5
Density : 2.98 to 3.02
Fracture : Conchoidal
Streak : White


TP : Translucent to transparent
RI : 1.509 to 1.700
Birefringence : 0.191
Optical character : Uniaxial -
Pleochroism : Visible
Fluorescence : Pale blue to pale green


Solubility : Hydrochloric acid

Magnetism : NoneRadioactivity : None

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