Cossaite
Chemical formula: (Mg<sub>0.5</sub>,☐)Al<sub>6</sub>(S<sup>6+</sup>O<sub>4</sub>)<sub>6</sub>(HS<sup>6+</sup>O<sub>4</sub>)F<sub>6</sub>·36H<sub>2</sub>O
Cossaite is an extremely rare, hydrated aluminum sulfate, forming microscopic, colorless crystals with a hexagonal outline.
Properties
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
Diagnostic features
## Identification Identification of cossaite is only possible using advanced analytical methods, such as scanning electron microscopy (SEM) combined with chemical analysis (EDS) and X-ray diffraction (XRD). Visual identification, even under a microscope, is impossible without confirmation of chemical composition and crystal structure. ## Distinguishing from Similar Minerals Cossaite can be confused with other microscopic sulfates found in fumarolic environments, such as alunite, alunogen, or other newly discovered minerals. Differentiation requires specialized chemical analysis to reveal the unique combination of aluminum, sulfur, and fluorine in cossaite's structure. ## Crystal Forms Cossaite forms very small, thin, tabular crystals with a hexagonal outline. They occur as single, scattered crystals on the surface of the host rock.
Geological environment
## Genesis Cossaite is a mineral of volcanic origin, formed by the sublimation of volcanic gases. It crystallizes directly from hot vapors (fumaroles) at temperatures of approximately 200-300°C. It is a product of the reaction of sulfur- and fluorine-rich gases with volcanic rocks. ## Mineral Associations This mineral occurs in association with other sulfates and fluorides typical of fumarolic environments. At the type locality (La Fossa), it was found in association with anhydrite, sassolite, and hematite. ## Localities The only confirmed locality for cossaite in the world is its type locality: the La Fossa crater on Vulcano Island (Aeolian Islands), in the province of Messina, Sicily, Italy.
Rarity
Extremely rare
For collectors
## Quality Criteria As a microscopic mineral, cossaite is not evaluated according to typical collector criteria such as size or color. The value of a specimen lies in its scientific significance and analytical confirmation. The most valuable specimens are fragments of host rock with the largest possible number of well-formed, albeit still microscopic, crystals whose identity has been laboratory-verified.
Care and storage
## Cleaning Due to the extreme rarity and microscopic size of the crystals, cossaite specimens should not be cleaned in a traditional manner. Any attempt at mechanical or chemical cleaning risks irreversible damage to the mineral. Specimens should only be analyzed under laboratory conditions. ## What to Avoid Contact with water, chemicals, and changes in temperature and humidity should be avoided. As a mineral formed in a fumarolic environment, it is likely unstable under standard atmospheric conditions and may undergo dehydration or react with atmospheric moisture. ## Storage Cossaite specimens, typically in the form of host rock fragments with microcrystals, must be stored in specialized, airtight containers (so-called micromount boxes), under stable conditions, away from light, dust, and temperature fluctuations.