In this article, the topic Atacamite will be addressed from a broad and detailed perspective, with the aim of providing readers with a complete and enriching vision of this matter. Through a comprehensive and rigorous analysis, different aspects and approaches related to Atacamite will be explored, in order to provide relevant and up-to-date information. The various implications and consequences that Atacamite can have in different contexts will also be examined, as well as possible solutions or recommendations to address this issue effectively. With a critical and reflective perspective, this article aims to offer the reader solid and well-founded knowledge about Atacamite, thus promoting greater understanding and awareness about it.
Atacamite | |
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General | |
Category | Halide mineral |
Formula (repeating unit) | Cu2Cl(OH)3 |
IMA symbol | Ata |
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 ; 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 |
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. The Atacama Desert is also the namesake of the mineral.
Atacamite is polymorphous with botallackite, clinoatacamite, and paratacamite. 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. The mineral has also been found naturally on oxidized copper deposits in Chile, China, Russia, Czech Republic, Arizona, and Australia. It occurs in association with cuprite, brochantite, linarite, caledonite, malachite, chrysocolla and its polymorphs.
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.
Atacamite occurs as a biomineral in the jaws of bloodworms.