Chrysocolla
Chrysocolla | |
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Chrysocolla and malachite from Australia |
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General | |
Category | Silicate mineral |
Formula (repeating unit) |
(Cu,Al)2H2Si2O5(OH)4·nH2O |
Strunz classification | 09.ED.20 |
Unit cell | a = 5.7 Å, b = 8.9 Å, c = 6.7 Å |
Identification | |
Color | Blue, Cyan or blue-green, green |
Crystal habit | Massive, nodular, botryoidal |
Crystal system | Orthorhombic |
Cleavage | none |
Fracture | Irregular/uneven, sub-conchoidal |
Tenacity | Brittle to sectile |
Mohs scale hardness | 2.5 - 3.5 |
Luster | Vitreous to dull |
Streak | white to a blue-green color |
Diaphaneity | Translucent to opaque |
Specific gravity | 1.9 - 2.4 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.575 - 1.585 nβ = 1.597 nγ = 1.598 - 1.635 |
Birefringence | δ = 0.023 - 0.050 |
References | [1][2][3] |
Contents |
Properties
Chrysocolla has a cyan (blue-green) color and is a minor ore of copper, having a hardness of 2.5 to 3.5.Name and discovery
The name comes from the Greek chrysos, "gold", and kolla, "glue", in allusion to the name of the material used to solder gold, and was first used by Theophrastus in 315 BCE.Formation and occurrence
It is of secondary origin and forms in the oxidation zones of copper ore bodies. Associated minerals are quartz, limonite, azurite, malachite, cuprite, and other secondary copper minerals.It is typically found as botryoidal or rounded masses and crusts, or vein fillings. Because of its light color, it is sometimes confused with turquoise.
Notable occurrences include Israel, Democratic Republic of Congo, Chile, Cornwall in England, and Arizona, Utah, Idaho, New Mexico, Michigan, and Pennsylvania in the United States.
Questions regarding mineral status
A 2006 study has produced evidence that chrysocolla may be a microscopic mixture of the copper hydroxide mineral spertiniite, amorphous silica and water.[4][2]References
Wikimedia Commons has media related to: Chrysocolla |
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