Atacamite
Atacamite is a copper halide mineral: a copper(II) chloride hydroxide with formula Cu2Cl(OH)3. It was first described for deposits in the Atacama Desert of Chile in 1802 by Dmitri de Gallitzin.[2] The Atacama Desert is also the namesake of the mineral.
Atacamite | |
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General | |
Category | Halide mineral |
Formula (repeating unit) | Cu2Cl(OH)3 |
IMA symbol | Ata[1] |
Strunz classification | 3.DA.10a |
Crystal system | Orthorhombic |
Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
Space group | Pnma |
Unit cell | a = 6.03, b = 9.12 c = 6.865 [Å]; Z = 4 |
Identification | |
Color | Bright green, dark emerald-green to blackish green |
Crystal habit | Slender prismatic crystals, fibrous, granular to compact, massive |
Twinning | Contact and penetration with complex twinned groupings |
Cleavage | Perfect on {010}, fair on {101} |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3 - 3.5 |
Luster | Adamantine to vitreous |
Streak | Apple green |
Diaphaneity | Transparent to translucent |
Specific gravity | 3.745 – 3.776 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.831 nβ = 1.861 nγ = 1.880 |
Birefringence | δ = 0.049 |
Pleochroism | X = pale green; Y = yellow-green; Z = grass-green |
2V angle | Calculated: 74° |
Dispersion | r < v, strong |
References | [2][3][4][5] |
Occurrence
Atacamite is polymorphous with botallackite, clinoatacamite, and paratacamite.[2] Atacamite is a comparatively rare mineral, formed from primary copper minerals in the oxidation or weathering zone of arid climates. It has also been reported as a volcanic sublimate from fumarole deposits, as sulfide alteration products in black smokers.[3] The mineral has also been found naturally on oxidized copper deposits in Chile, China, Russia, Czech Republic, Arizona, and Australia.[6] It occurs in association with cuprite, brochantite, linarite, caledonite, malachite, chrysocolla and its polymorphs.[3]
Synthetic Occurrence
Atacamite has been discovered in the patina of the Statue of Liberty, and as alteration of ancient bronze and copper artifacts. The mineral has been found as a pigment in sculpture, manuscripts, maps, and frescoes discovered in Eurasia, Russia, and Persia.[6]
Biomineral
Atacamite occurs as a biomineral in the jaws of bloodworms.[7][8]
- Atacamite prisms from Chile
- Atacamite from Chile displayed in the Harvard Museum of Natural History
- Atacamite from Mt. Gunson, South Australia
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.
- Atacamite on Mindat.org
- Handbook of Mineralogy
- Atacamite on Webmineral
- Mineralienatlas
- "Atacamite - CAMEO". cameo.mfa.org. Retrieved 2017-10-15.
- Lichtenegger HC, Schöberl T, Bartl MH, Waite H, Stucky GD (October 2002). "High abrasion resistance with sparse mineralization: copper biomineral in worm jaws". Science. 298 (5592): 389–92. Bibcode:2002Sci...298..389L. doi:10.1126/science.1075433. PMID 12376695. S2CID 14001250.
- Lichtenegger HC, Schöberl T, Ruokolainen JT, et al. (August 2003). "Zinc and mechanical prowess in the jaws of Nereis, a marine worm". Proc. Natl. Acad. Sci. U.S.A. 100 (16): 9144–9. Bibcode:2003PNAS..100.9144L. doi:10.1073/pnas.1632658100. PMC 170886. PMID 12886017.