Cherokeeite
Chemical formula: [Pb<sup>2+</sup><sub>2</sub>Zn<sup>2+</sup>(OH)<sub>4</sub>](S<sup>6+</sup>O<sub>4</sub>)·H<sub>2</sub>O
Cherokeeite is a very rare, secondary zinc and lead sulfate mineral, forming microscopic, colorless crystals.
Properties
- Luster
- Vitreous
- Streak
- White
- Density
- 4.96
- Cleavage
- Perfect on {010}
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of cherokeeite is impossible without specialized equipment. It requires the use of a scanning electron microscope (SEM) to observe crystal morphology and energy-dispersive X-ray spectroscopy (EDS) or other analytical methods to confirm chemical composition. Visually, in field conditions or in a collection, it is impossible to distinguish from other microscopic secondary minerals. ## Distinguishing from Similar Minerals It can be confused with many other secondary lead and zinc sulfates and carbonates, such as cerussite, anglesite, or hydrozincite, which often form similar, fine coatings. Certain differentiation requires advanced laboratory analyses. ## Crystal Forms It forms elongated, bladed, or thin, tabular crystals. They usually occur as rosette-like, radial, or haphazardly arranged aggregates on the rock surface.
Geological environment
## Genesis Cherokeeite is a secondary mineral, forming in the oxidation zone of zinc and lead ore deposits. It forms as a result of weathering and alteration of primary sulfide minerals, such as sphalerite and galena, under low temperature and pressure conditions, in the presence of water. ## Mineral Associations At the type locality, it co-occurs with other secondary minerals, such as anglesite, cerussite, sphalerite, galena, as well as newly discovered minerals from the same locality: kansasite and downsite. ## Localities The only confirmed occurrence of cherokeeite in the world is the Cherokee Mine in Cherokee County, Kansas, USA.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a cherokeeite specimen is assessed primarily based on the richness and aesthetics of the microcrystal aggregates visible under a microscope. The most valued specimens are those where crystals form distinct, well-formed, rosette-like clusters, contrasting with the matrix. Association with other rare minerals from this locality is also important. ## Popular Localities The only source of specimens is the type locality – the Cherokee Mine in Kansas, USA. Specimens from this location are highly sought after by collectors specializing in rare minerals and so-called "micromounts."
Care and storage
## Cleaning Due to the extreme fragility and microscopic size of the crystals, no mechanical or chemical cleaning is recommended. Specimens should be treated as inviolable. ## What to Avoid Avoid any contact with chemicals, water, and ultrasound. Vibrations, shocks, and temperature changes can damage or destroy delicate crystals. Do not expose the specimen to direct sunlight. ## Storage Cherokeeite specimens should be stored exclusively in stable, sealed containers (so-called "micromount boxes") to protect them from dust, moisture, and mechanical damage. It is best to store them in a dry place with a constant temperature.