Chemical Formula |
Cu2H2Si2O5(OH)4 |
Composition |
Basic copper silicate, often with some aluminum. The composition of this mineral is usually variable and it therefore lacks a definitive chemical composition. |
Variable Formula |
(Cu2-x,Alx)H2-xSi2O5(OH)4 · nH2O |
Color |
Bright green, bluish-green, sky blue, gray. May be mottled or multicolored green and blue. |
Streak |
White to pale blue |
Hardness |
2 - 4 |
Crystal System |
Orthorhombic |
Crystal Forms |
Chrysocolla is never in visible crystals. It is almost always in botryoidal, reniform, or stalactitic groups, in rounded balls, and in massive form. Also in solid and fibrous veins, in tufts of fibrous crystals, and in crusts. Frequently forms pseudomorph after other minerals, especially Azurite. |
Transparency |
Translucent to Opaque |
Specific Gravity |
2.0 - 2.2 |
Luster |
Vitreous to greasy |
Cleavage |
None |
Fracture |
Conchoidal to uneven |
Tenacity |
Brittle |
In Group |
Silicates; Phyllosilicates |
Striking Features |
Bright color, hardness, and habits |
Environment |
As a secondary alteration mineral in the oxidation zone of copper deposits, hydrothermal replacement deposits, and in igneous rocks. |
Rock Type |
Igneous, Sedimentary, Metamorphic |
Popularity (1-4) |
2 |
Prevalence (1-3) |
2 |
Demand (1-3) |
2 |
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