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.
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Hydrozincite |
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Category | Carbonate mineral |
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Formula | Zn5(CO3)2(OH)6 |
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IMA symbol | Hznc[1] |
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Strunz classification | 5.BA.15 |
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Crystal system | Monoclinic |
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Crystal class | Prismatic (2/m) (same H-M symbol) |
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Space group | C2/m |
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Unit cell | a = 13.58 Å, b = 6.28 Å, c = 5.41 Å; β = 95.51°, Z = 2 |
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Color | White to grey, stained pale pink, or pale yellow or brown; colourless in transmitted light. |
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Crystal habit | Lathlike or bladed crystals uncommon, in fibrous, stalactitic, reniform, pisolitic aggregates; also earthy, chalky, massive |
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Twinning | Contact twinning on {100} |
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Cleavage | Perfect on {100} |
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Fracture | Irregular/uneven |
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Tenacity | Very brittle |
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Mohs scale hardness | 2–2+1⁄2 |
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Luster | Silky, pearly, dull, earthy |
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Streak | White |
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Diaphaneity | Transparent, translucent |
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Specific gravity | 3.5–4 |
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Optical properties | Biaxial (−) |
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Refractive index | nα = 1.630 nβ = 1.642 nγ = 1.750 |
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Birefringence | δ = 0.120 |
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2V angle | Measured: 40°, calculated: 40° |
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Dispersion | relatively strong |
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Ultraviolet fluorescence | Fluoresces pale blue to lilac under UV |
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Solubility | Readily soluble in acids. |
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References | [2][3][4] |
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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]