Malachite | |
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General | |
Category | Carbonate mineral |
Formula (repeating unit) | Cu2CO3(OH)2 |
IMA symbol | Mlc[1] |
Strunz classification | 5.BA.10 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/a |
Identification | |
Formula mass | 221.1 g/mol |
Color | Bright green, dark green, blackish green, with crystals deeper shades of green, even very dark to nearly black commonly banded in masses; green to yellowish green in transmitted light |
Crystal habit | Massive, botryoidal, stalactitic, crystals are acicular to tabular prismatic |
Twinning | Common as contact or penetration twins on {100} and {201}. Polysynthetic twinning also present. |
Cleavage | Perfect on {201} fair on {010} |
Fracture | Subconchoidal to uneven |
Mohs scale hardness | 3.5–4 |
Luster | Adamantine to vitreous; silky if fibrous; dull to earthy if massive |
Streak | light green |
Diaphaneity | Translucent to opaque |
Specific gravity | 3.6–4 |
Optical properties | Biaxial (–) |
Refractive index | nα = 1.655 nβ = 1.875 nγ = 1.909 |
Birefringence | δ = 0.254 |
References | [2][3][4][5] |
Malachite is a copper carbonate hydroxide mineral, with the formula Cu2CO3(OH)2. This opaque, green-banded mineral crystallizes in the monoclinic crystal system, and most often forms botryoidal, fibrous, or stalagmitic masses, in fractures and deep, underground spaces, where the water table and hydrothermal fluids provide the means for chemical precipitation. Individual crystals are rare, but occur as slender to acicular prisms. Pseudomorphs after more tabular or blocky azurite crystals also occur.[5]