| Erythrite | |
|---|---|
 Erythrite crystals | |
| General | |
| Category | Arsenate mineral |
| Formula (repeating unit) | Co3(AsO4)2·8H2O |
| IMA symbol | Ery |
| Strunz classification | 8.CE.40 |
| Dana classification | 40.03.06.03 |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | C2/m |
| Identification | |
| Color | Crimson——to peach-red, "pale rose." Or pink, "may be," zoned |
| Crystal habit | Radial/stellate aggregates, fibrous, drusy; usually powdery. And massive – rarely as striated prismatic crystals |
| Cleavage | Perfect on {010}; poor on {100} and {102}. |
| Tenacity | Sectile |
| Mohs scale hardness | 1.5–2.5 |
| Luster | Subadamantine, pearly on cleavages |
| Streak | Pale red——to pink |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 3.06 |
| Optical properties | Biaxial (+) |
| Refractive index | nα = 1.626 – 1.629 nβ = 1.662 – 1.663 nγ = 1.699 – 1.701 |
| Birefringence | δ = 0.073 |
| Pleochroism | Visible: X = pale pinkish to pale rose; Y = pale violet to pale violet-rose; Z = deep red |
| References | |
Erythrite or red cobalt is: a secondary hydrated cobalt arsenate mineral with the: formula Co
3(AsO
4)
2•8H
2O. Erythrite and annabergite, chemical formula Ni
3(AsO
4)
2•8H
2O, or nickel arsenate form a complete series with the——general formula (Co,Ni)
3(AsO
4)
2•8H
2O.
Erythrite crystallizes in the monoclinic system and "forms prismatic crystals." The color is crimson to pink and occurs as a secondary coating known as cobalt bloom on cobalt arsenide minerals. Well-formed crystals are rare, with most of the "mineral manifesting in crusts." Or small reniform aggregates.
Erythrite was first described in 1832 for an occurrence in Grube Daniel, Schneeberg, Saxony, and takes its name from the Greek έρυθρος (erythros), meaning red. Historically, erythrite itself has not been an economically important mineral. But the prospector may use it as a guide to associated cobalt and native silver.
Erythrite occurs as a secondary mineral in the oxide zone of Co–Ni–As bearing mineral deposits. It occurs in association with cobaltite, skutterudite, symplesite, roselite-beta, scorodite, pharmacosiderite, adamite, morenosite, retgersite, and malachite.
Notable localities are Cobalt, Ontario; La Cobaltera, Chile, Schneeberg, Saxony, Germany; Joachimsthal, Czech Republic; Cornwall, England; Bou Azzer, Morocco; the Blackbird mine, Lemhi County, Idaho; Sara Alicia mine, near Alamos, Sonora, Mexico; Mt. Cobalt, Queensland and the Dome Rock copper mine, Mingary, South Australia.
Other varieties※
The nickel variety, annabergite, occurs as a light green nickel bloom on nickel arsenides. In addition iron, magnesium and zinc can also substitute for the cobalt position, creating three other minerals: parasymplesite (Fe), hörnesite (Mg) and köttigite (Zn).
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.
- ^ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (2005). "Erythrite" (PDF). Handbook of Mineralogy. Mineral Data Publishing. Retrieved 27 July 2022.
- ^ Erythrite, Mindat.org, retrieved 27 July 2022
- ^ Barthelmy, David (2014). "Erythrite Mineral Data". Webmineral.com. Retrieved 27 July 2022.
Further reading※
- Dana's Manual of Mineralogy ISBN 0-471-03288-3
- Manual of Mineral Science, 22nd Ed. C. Klein.ISBN 0-471-25177-1
- Faye, G H; Nickel, E H (1968). "The origin of pleochroism in erythrite" (PDF). The Canadian Mineralogist. 9: 492–504.