Hydrozincite
Hydrozincite, also known as zinc bloom or marionite, is a white carbonate mineral consisting of Zn5(CO3)2(OH)6. It is usually found in massive rather than crystalline form.
Hydrozincite | |
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General | |
Category | Carbonate mineral |
Formula (repeating unit) | Zn5(CO3)2(OH)6 |
IMA symbol | Hznc[1] |
Strunz classification | 5.BA.15 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | C2/m |
Unit cell | a = 13.58 Å, b = 6.28 Å, c = 5.41 Å; β = 95.51°, Z = 2 |
Identification | |
Color | White to grey, stained pale pink, or pale yellow or brown; colourless in transmitted light. |
Crystal habit | Lathlike or bladed crystals uncommon, in fibrous, stalactitic, reniform, pisolitic aggregates; also earthy, chalky, massive |
Twinning | Contact twinning on {100} |
Cleavage | Perfect on {100} |
Fracture | Irregular/uneven |
Tenacity | Very brittle |
Mohs scale hardness | 2 - 2+1⁄2 |
Luster | Silky, pearly, dull, earthy |
Streak | White |
Diaphaneity | Transparent, translucent |
Specific gravity | 3.5 - 4 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.630 nβ = 1.642 nγ = 1.750 |
Birefringence | δ = 0.120 |
2V angle | Measured: 40° , calculated: 40° |
Dispersion | relatively strong |
Ultraviolet fluorescence | Fluoresces pale blue to lilac under UV |
Solubility | Readily soluble in acids. |
References | [2][3][4] |
It occurs as an oxidation product of zinc ores and as post mine incrustations. It occurs associated with smithsonite, hemimorphite, willemite, cerussite, aurichalcite, calcite and limonite.[2]
It was first described in 1853 for an occurrence in Bad Bleiberg, Carinthia, Austria and named for its chemical content.[3]
References
- Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- Handbook of Mineralogy
- Mindat
- Webmineral data
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