Article · Wikipedia archive · Last revised Aug 1, 2026

Brochantite

Brochantite is a sulfate mineral, one of a number of cupric sulfates. Its chemical formula is Cu4SO4(OH)6. Formed in arid climates or in rapidly oxidizing copper sulfide deposits, it was named by Armand Lévy for his fellow Frenchman, geologist and mineralogist A. J. M. Brochant de Villiers.

Last revised
Aug 1, 2026
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≈ 2 min
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382 w
Citations
11
Source
Brochantite
General
CategorySulfate minerals
FormulaCu4SO4(OH)6
IMA symbolBct1
Strunz classification7.BB.25
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupP21/a
Identification
ColorGreen, emerald green, or black
Crystal habitPrismatic crystals; acicular needle-like crystals; druse
CleavagePerfect [100]
FractureConchoidal
Tenacitybrittle
Mohs scale hardness3.5–4.0
LusterVitreous to pearly
StreakPale green
DiaphaneityTransparent to translucent
Specific gravity3.97
Optical propertiesBiaxial (−)
Refractive indexnα = 1.728 nβ = 1.771 nγ = 1.800
Birefringenceδ = 0.072
PleochroismWeak
2V anglemeasured: 72°
References234

Brochantite is a sulfate mineral, one of a number of cupric sulfates. Its chemical formula is Cu4SO4(OH)6.234 Formed in arid climates or in rapidly oxidizing copper sulfide deposits, it was named by Armand Lévy for his fellow Frenchman, geologist and mineralogist A. J. M. Brochant de Villiers.4

Crystals of brochantite can range from emerald green to black-green to blue-green, and can be acicular or prismatic. Brochantite is often associated with minerals such as malachite, azurite, and chrysocolla, and may form pseudomorphs with these minerals.

The mineral is found in a number of locations around the world, notably the southwestern United States (especially Arizona), Serifos in Greece and Chile.

Brochantite is a common corrosion product on bronze sculptures located in urban areas, where atmospheric sulfur dioxide (a common pollutant) is present. Brochantite forms mainly in exposed areas where weathering prevents accumulation copper ions and enhancement in the acidity of water films.5 In sheltered areas, the main corrosion product is antlerite.

Brochantite veins were mined for copper in Chuquicamata, Chile, from 1879 until 1912 when a more indiscriminate large-scale mining of low-grade ores began at the mine.67

References

References

  1. Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. Webmineral
  3. Mineral Handbook
  4. Mindat
  5. Leygraf C, Graedel TE. Atmospheric corrosion. New York: Wiley-Interscience; 2000. ISBN 0471372196
  6. Ossandon, Guillermo; Freraut, Roberto; Gustafson, Lewis; Lindsay, Darryl; Zentilli, Marcos (2001). "Geology of the Chuquicamata Mine: A Progress Report". Economic Geology. 96 (2): 249–270. Bibcode:2001EcGeo..96..249O. doi:10.2113/gsecongeo.96.2.249. S2CID 128812977.
  7. Orellana Retamales, Luis (2004). "La lucha de los mineros contra las leyes: Chuquicamata (1900-1915)". Historia. 37 (I): 169–206.
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