Chalcocite

Chalcocite
Chalcosite from Cornwall
General
Category Sulfide minerals
Formula
(repeating unit)		 copper(I) sulfide: Cu2S
Strunz classification 2.BA.05a
Crystal system Monoclinic
Crystal class Prismatic (2/m)
(same H-M symbol)
Space group P21/c
Unit cell a = 15.246(4) Å,
b = 11.884(2) Å,
c = 13.494(3) Å;
β = 116.35(1)°; Z = 48
Identification
Color Dark gray to black
Crystal habit Tabular to prismatic crystals also massive to granular, (pseudo-orthorhombic)
Twinning Common on {110} yielding pseudohexagonal stellate forms
Cleavage Indistinct on {110}
Fracture Conchoidal
Tenacity Brittle to sectile
Mohs scale hardness 2.5 - 3
Luster Metallic
Streak Shiny black to lead gray
Diaphaneity Opaque
Specific gravity 5.5 - 5.8
Fusibility 2-2.5
References [1][2][3][4]

Chalcocite (UK: /ˈkælkəˌsaɪt/[5]), copper(I) sulfide (Cu2S), is an important copper ore mineral. It is opaque and dark-gray to black with a metallic luster. It has a hardness of ​2 1⁄2 - 3 on the Mohs scale. It is a sulfide with an orthorhombic crystal system.

The term chalcocite comes from the alteration of the obsolete name chalcosine, from the Greek khalkos, meaning copper. It is also known as redruthite, vitreous copper and copper-glance.[6]

Occurrence

Chalcocite is sometimes found as a primary vein mineral in hydrothermal veins. However, most chalcocite occurs in the supergene enriched environment below the oxidation zone of copper deposits as a result of the leaching of copper from the oxidized minerals. It is also often found in sedimentary rocks.

It has been mined for centuries and is one of the most profitable copper ores. The reasons for this is its high copper content (66.6% atomic ratio and nearly 80% by weight) and the ease at which copper can be separated from sulfur.

Chalcocite crystals from the Mammoth Mine, Mount Isa - Cloncurry area, Queensland, Australia (size: 3.0 x 2.9 x 2.4 cm)

Since chalcocite is a secondary mineral that forms from the alteration of other minerals, it has been known to form pseudomorphs of many different minerals. A pseudomorph is a mineral that has replaced another mineral atom by atom, but it leaves the original mineral's crystal shape intact. Chalcocite has been known to form pseudomorphs of the minerals bornite, covellite, chalcopyrite, pyrite, enargite, millerite, galena and sphalerite.

See also

References

  1. ↑ Mineralienatlas
  2. ↑ Mindat.org
  3. ↑ Webmineral.com
  4. ↑ Handbook of Mineralogy
  5. ↑ https://www.collinsdictionary.com/dictionary/english/chalcocite
  6. ↑ Wikisource Chisholm, Hugh, ed. (1911). "Copper-glance". Encyclopædia Britannica. 7 (11th ed.). Cambridge University Press. p. 110.
  • Dana's Manual of Mineralogy ISBN 0-471-03288-3
  • Mineral Galleries
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