Pseudomalachite | |
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General | |
Category | Phosphate minerals |
Formula (repeating unit) | Cu5(PO4)2(OH)4 |
IMA symbol | Pmlc[1] |
Strunz classification | 8.BD.05 |
Dana classification | 41.04.03.01 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/c |
Unit cell | a = 4.47 Å, b = 5.75 Å, c = 17.05 Å; β = 91.06°; Z = 2 |
Identification | |
Formula mass | 575.7 g/mol |
Color | Dark emerald green to blackish green |
Crystal habit | Crystals, which are rare, are prismatic, usually with uneven faces. Pseudomalachite is commonly compact, reniform or botryoidal, or it may be fibrous or in crusts and films. |
Twinning | On {100} |
Cleavage | Perfect on {100}, distinct on {010} |
Fracture | Splintery or conchoidal |
Mohs scale hardness | 4.5–5 |
Luster | Vitreous |
Streak | Blue green, paler than the mineral |
Diaphaneity | Translucent to subtranslucent |
Specific gravity | (Measured) 4.15 to 4.35 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.791 nβ = 1.856 nγ = 1.867 |
Birefringence | δ = 0.076 |
Pleochroism | Weak; X = bluish green to pale green; Y = yellowish green; Z = deep bluish green to blue-green |
2V angle | 48° |
Dispersion | Strong r<v. Also biaxial (+) r>v |
Solubility | Soluble in acids but without effervescence (in contrast to malachite which effervesces with warm HCl) |
Other characteristics | Not fluorescent, not radioactive |
References | [2][3][4][5] |
Pseudomalachite is a phosphate of copper with hydroxyl, named from the Greek for "false" and "malachite", because of its similarity in appearance to the carbonate mineral malachite, Cu2(CO3)(OH)2. Both are green coloured secondary minerals found in oxidised zones of copper deposits, often associated with each other. Pseudomalachite is polymorphous with reichenbachite and ludjibaite. It was discovered in 1813. Prior to 1950 it was thought that dihydrite, lunnite, ehlite, tagilite and prasin were separate mineral species, but Berry analysed specimens labelled with these names from several museums, and found that they were in fact pseudomalachite. The old names are no longer recognised by the IMA.[6]