Cuprocherokeeite
Chemical formula: [Pb<sup>2+</sup><sub>8</sub>Zn<sup>2+</sup><sub>3</sub>Cu<sup>2+</sup>(OH)<sub>16</sub>](S<sup>6+</sup>O<sub>4</sub>)<sub>4</sub>·4H<sub>2</sub>O
Cuprorcherite is an extremely rare, secondary zinc, lead, and copper sulfate mineral, forming microscopic, platy crystals of a blue color.
Properties
- Luster
- Vitreous
- Streak
- Very pale blue
- Cleavage
- Perfect on {0001}
- Fracture
- Brittle
- Transparency
- Transparent
- Crystal system
- Trigonal
Diagnostic features
## Identification Identification of cuprorcherite is possible only through advanced analytical methods, such as Raman spectroscopy, X-ray diffraction (XRD), and chemical analysis (EDS/WDS). Under collecting conditions, identification relies on label analysis and comparison with the appearance of specimens from the type locality. Characteristic features include microscopic, light blue, platy crystals forming rosette-like aggregates. ## Distinguishing from Similar Minerals Cuprorcherite is visually almost identical to cherokeeite, from which it differs by the presence of copper in its structure. It can also be confused with other secondary copper and zinc minerals of blue color, such as ktenasite, serpierite, or linarite. Definitive distinction from these minerals requires specialized laboratory tests. ## Crystal Forms Cuprorcherite crystallizes in the form of very small, thin, platy crystals with a hexagonal or rhombic outline. These crystals often combine into radial or rosette-like aggregates, and also form thin crusts and coatings.
Geological environment
## Genesis Cuprorcherite is a secondary mineral that forms in the oxidation zones (gossans) of polymetallic ore deposits. It originates from the weathering of primary sulfides, such as galena, sphalerite, and chalcopyrite, in the presence of sulfate-rich waters. Its formation is associated with a low pH environment. ## Mineral Associations At the type locality (Cherokee Mine, Georgia, USA), cuprorcherite is associated with anglesite, cherokeeite, linarite, brochantite, hemimorphite, goethite, and quartz. ## Localities The only confirmed and described locality of cuprorcherite occurrence in the world is its discovery site – the Cherokee Mine, located in Lincoln County, Georgia, USA.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of cuprorcherite specimens is primarily assessed based on the richness and aesthetics of the microscopic crystalline aggregates. The most valued specimens are those with clearly formed, rosette-like clusters of intense, blue color, contrasting well with the rock matrix. Crystal size, although always microscopic, is also important – larger and better-formed crystals are more desirable. The presence of associated minerals, which can enhance the visual appeal of the specimen, is also significant. ## Popular Localities The only source of collector specimens is the type locality – the Cherokee Mine in Georgia, USA. Specimens from this location are highly sought after by collectors specializing in rare minerals and microminerals.
Care and storage
## Cleaning Cuprorcherite specimens are extremely delicate and usually microscopic in size. Mechanical or chemical cleaning is not recommended. Any attempts at cleaning may irreversibly destroy the crystalline aggregates. If dust removal is necessary, it can be done very carefully using a photographic air blower, without touching the mineral surface. ## What to Avoid Contact with water, acids, bases, and any solvents must be strictly avoided. The mineral is likely soluble in acids. It should be protected from vibrations, impacts, and abrasion. It should not be heated or exposed to temperature changes. ## Storage Specimens should be stored exclusively in specialized "micromount" boxes, which protect them from mechanical damage and dust. Store in a dry place with stable temperature, away from direct sunlight.