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
Powder-blue chrysocolla as stalactitic growths and as a thin carpet in vugs inside a boulder of nearly solid tyrolite from the San Simon Mine, Iquique Province, Chile (size: 14.1 x 8.0 x 7.8 cm)
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
Banded white to blue green chrysocolla from Bisbee, Arizona (size: 12.2 x 5.5 x 5.2 cm)
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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