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.