Very rarely in visible crystals, which are prismatic and tabular. Most often acicular, radiating, earthy, grainy, encrusting, as fibrous masses, as dense bundles of acicular crystals, and as cotton-like, radiatingmasses. Sometimes as tiny twinned crystals that appear orthorhombic with rounded corners. Occasionally forms a pseudomorph after Azurite and Malachite, assume the crystal shape of those minerals.
Transparency
Transparent to opaque
Specific Gravity
4
Luster
Vitreous to silky
Cleavage
1,1 - pinacoidal
Fracture
Conchoidal, uneven, splintery
Tenacity
Brittle
In Group
Sulfates; Hydrous Sulfates
Striking Features
Intense green color, crystal habits, and mode of occurrence
Environment
Brochantite is a secondary copper mineral formed in the oxidation zone of copper deposits.