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Oxide mineral

Cuprite

Cuprite
All data from the card 23
Category
Oxide mineral
Formula
Cu2O
IMA symbol
Cpr
Strunz classification
4.AA.10
Dana classification
4.1.1.1
Crystal system
Cubic
Crystal class
Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m)
Space group
Pn3m
Unit cell
a = 4.2685 Å; V = 77.77 Å3; Z = 2
Color
Dark red to cochineal red, sometimes almost black
Crystal habit
Cubic, octahedral, and dodecahedral crystals; as hairlike capillary forms, earthy, compact granular and massive
Twinning
Penetration twins
Cleavage
Fair in four directions forming octahedrons
Fracture
Conchoidal to uneven
Tenacity
Brittle
Mohs scale hardness
3.5 to 4
Luster
Adamantine, sub-metallic, earthy
Streak
Shining metallic brownish-red
Diaphaneity
Transparent, translucent
Specific gravity
6.14
Optical properties
Isotropic
Refractive index
n = 2.849
Pleochroism
Visible
Cuprite from Tsumeb Mine (size:2.3 x 2.1 x 1.2 cm
Cuprite from Tsumeb Mine (size:2.3 x 2.1 x 1.2 cm
Chalcotrichite from Ray, Arizona
Chalcotrichite from Ray, Arizona
2 images

Cuprite is an oxide mineral composed of copper(I) oxide Cu2O, and is a minor ore of copper.

Its dark crystals with red internal reflections are in the isometric system hexoctahedral class, appearing as cubic, octahedral, or dodecahedral forms, or in combinations. Penetration twins frequently occur. In spite of its nice color, it is rarely used for jewelry because of its low Mohs hardness of 3.5 to 4. It has a relatively high specific gravity of 6.1, imperfect cleavage and is brittle to conchoidal fracture. The luster is sub-metallic to brilliant adamantine. The "chalcotrichite" (from Ancient Greek: χαλκός θρίξ τριχός, "plush copper ore") variety typically shows greatly elongated (parallel to [001]) capillary or needle like crystals forms.

It is a secondary mineral which forms in the oxidized zone of copper sulfide deposits. It frequently occurs in association with native copper, azurite, chrysocolla, malachite, tenorite and a variety of iron oxide minerals. It is known as ruby copper due to its distinctive red color.

Cuprite was first described by Wilhelm Karl Ritter von Haidinger in 1845 and the name derives from the Latin cuprum for its copper content.

Cuprite is found in the Ural Mountains, Altai Mountains, and Sardinia, and in more isolated locations in Cornwall, France, Arizona, Chile, Bolivia, and Namibia.

As a gemstone

Though almost all crystals of cuprite are far too small to yield faceted gemstones, one unique deposit from Onganja in Seeis, Namibia, which was discovered in the 1970s, has produced crystals which were both large and gem quality. Virtually every faceted stone over one carat (0.2 g) in weight is from this single deposit, which has long since been mined out. The number of faceted gems over two carats (0.4 g) is difficult to estimate, but according to Joel Arem, one-time curator for the Smithsonian National Gem and Mineral Collection in Washington, D.C., faceted cuprite of any size is considered one of the most collectible and spectacular gems in existence, with its deep garnet coloring and higher brilliance than a diamond. Only the gem's soft nature prevents it from being among the most valuable jewelry stones.

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Text from Wikipedia, CC BY-SA 4.0 · Source article