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Bunsenite is the naturally occurring form of nickel(II) oxide, NiO. It occurs as rare dark green crystal coatings. It crystallizes in the cubic crystal system and occurs as well formed cubic, octahedral and dodecahedral crystals. It is a member of the periclase group.

Key facts

Mineral.name
Bunsenite
Mineral.image
Bunsenite - Kochhütte, Helbra, Mansfeld-Südharz, Saxony-Anhalt, Germany.jpg
Mineral.caption
Bunsenite with unknown colorless crystals from the collection of the „Verein zur Förderung der Lithothek“, Munich (collection number A022658). Field of view 1 mm. Locality: Kochhütte, Helbra, Mansfeld-Südharz, Saxony-Anhalt, Germany
Mineral.category
Oxide mineral
Mineral.formula
NiO
Mineral.IMAsymbol
Bus
Mineral.strunz
4.AB.25
Mineral.system
Cubic
Mineral.class
Hexoctahedral (mm) H–M symbol: (4/m 2/m)
Mineral.symmetry
Fmm
Mineral.unit cell
a = 4.1769 Å; Z = 4
Mineral.color
Dark pistachio-green
Mineral.habit
Octahedral crystal coatings, also cube or dodecahedron forms
Mineral.twinning
Observed
Mineral.cleavage
None
Mineral.mohs
5.5
Mineral.luster
Vitreous
Mineral.streak
Brownish-black

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Wikidata facts

Image
Bunsenite - Kochhütte, Helbra, Mansfeld-Südharz, Saxony-Anhalt, Germany.jpg
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Strunz 8th edition (series ID, updated)
IV/A.04
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
4.AB.25
Commons category
Bunsenite
chemical formula
NiO
Nickel-Strunz 9th edition (updated 2009)
4.AB.25
IMA Mineral Symbol
Bse

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Bunsenite is the naturally occurring form of nickel(II) oxide, NiO. It occurs as rare dark green crystal coatings. It crystallizes in the cubic crystal system and occurs as well formed cubic, octahedral and dodecahedral crystals. It is a member of the periclase group.

It was first described in 1868 for a sample from a hydrothermal nickel–uranium vein from Johanngeorgenstadt, Ore Mountains, Saxony, Germany and named for German chemist Robert Bunsen (1811–1899). Other occurrences include west of the Scotia talc mine near Bon Accord, Barberton district, Transvaal, South Africa and from Kambalda south of Kalgoorlie, Western Australia. The South African occurrence has evidence of thermal metamorphism of a nickel-rich meteorite. It occurs associated with native bismuth, annabergite, aerugite, xanthiosite in Germany; and with liebenbergite, trevorite, nickeloan serpentine, nickeloan ludwigite, violarite, millerite, gaspeite, nimite and bonaccordite in the South African occurrence.

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