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 and Aggregates
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.