Chemical Formula |
Cu6Si6O18 ·6H2O |
Composition |
Hydrous copper silicate |
Color |
Deep emerald green, dark green, bluish-green |
Streak |
Green |
Hardness |
5 |
Crystal System |
Hexagonal |
Crystal Forms |
In distinct, hexagonally-shaped crystals with pointed, rhombohedral ends. Crystals are almost almost always doubly terminated, and are usually short and stubby, although they are occasionally prismaticand elongated. Crystals may also be more typical rhombohedral, though this habit is very uncommon. Crystals are usually in dense groups of interconnected crystals, but may be as isolated individuals. Also drusy, radiating, acicular, botryoidal, grainy, encrusting, and massive. |
Transparency |
Transparent to nearly opaque |
Specific Gravity |
3.3 - 3.4 |
Luster |
Vitreous to adamantine |
Cleavage |
1,3 |
Fracture |
Uneven |
Tenacity |
Brittle |
In Group |
Silicates; Cyclosilicates |
Striking Features |
Distinctive color and crystal habits |
Environment |
As a secondary mineral in hydrothermal replacement copper deposits. |
Rock Type |
Sedimentary, Metamorphic |
Popularity (1-4) |
2 |
Prevalence (1-3) |
3 |
Demand (1-3) |
1 |
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