Linarite
In today's world, Linarite has become a relevant topic for a wide spectrum of society. Since its appearance, Linarite has caused a great impact in different areas, generating discussions, debates and conflicting opinions. Its influence has crossed borders and has aroused the interest of experts on the subject, as well as the population in general. Given its relevance, it is important to analyze in detail and objectively all aspects related to Linarite, understanding its implications, consequences and possible solutions. In this article, we will thoroughly explore the phenomenon of Linarite, from its origins to its current situation, with the aim of providing a complete and enriching perspective on this topic of global interest.
| Linarite | |
|---|---|
 | |
| General | |
| Category | Sulfate minerals |
| Formula (repeating unit) | PbCu |
| IMA symbol | Lna |
| Strunz classification | 7.BC.65 |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | P21/m |
| Unit cell | a = 9.701(2), b = 5.65 c = 4.69 ; β = 102.65°; Z = 2 |
| Identification | |
| Color | Deep azure blue |
| Crystal habit | Crystals elongated and tabular; in crusts and aggregates |
| Twinning | Common on {100}, also on {001} |
| Cleavage | Perfect on {100}, imperfect on {001} |
| Fracture | Conchoidal |
| Mohs scale hardness | 2.5 |
| Luster | Sub-adamantine, vitreous |
| Streak | Pale blue |
| Diaphaneity | Transparent, translucent |
| Specific gravity | 5.3 – 5.5 |
| Optical properties | Biaxial (−) |
| Refractive index | nα = 1.809 nβ = 1.838 nγ = 1.859 |
| Birefringence | δ = 0.050 |
| Pleochroism | X = pale blue; Y = blue; Z = Prussian blue |
| 2V angle | Measured: 80° |
| References | |
Linarite is a somewhat rare, crystalline mineral that is known among mineral collectors for its unusually intense, pure blue color. It is formed by the oxidation of galena and chalcopyrite and other copper sulfides. It is a combined copper lead sulfate hydroxide with formula PbCuSO4(OH)2. Linarite occurs as monoclinic prismatic to tabular crystals and irregular masses. It is easily confused with azurite, but does not react with dilute hydrochloric acid as azurite does. It has a Mohs hardness of 2.5 and a specific gravity of 5.3 – 5.5.
Linarite was first identified in 1822. It is named after the Linares Plateau, Spain. It occurs in association with brochantite, anglesite, caledonite, leadhillite, cerussite, malachite and hemimorphite.
Gallery
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A shallow pocket of crystals of an intense cobalt blue, from Darwin, Darwin District, Inyo County, California, US -
Linarite with malachite, Blanchard Mine, Hansonburg District, Socorro County, New Mexico US (Size: 1.1 × 0.8 × 0.4 cm) -
Linarite with caledonite, from Baker, El Dorado County, California US (Size 5.4 × 5.2 × 3.2 cm) -
Unusual cerussite with a coating ingrained into the surface of microcrystalline malachite and linarite that give it a rich blue-green color
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.
- ^ a b Linarite, Mindat.org, retrieved 11 July 2022
- ^ Barthelmy, David (2014). "Linarite Mineral Data". Webmineral.com. Retrieved 27 June 2022.
- ^ a b Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (2005). "Linarite" (PDF). Handbook of Mineralogy. Mineral Data Publishing. Retrieved 11 July 2022.
