Mellizinkalite

Chemical formula: K₃Zn²⁺₂Cl₇

Mellizinkalite is a very rare potassium zinc halide, forming tiny, colorless crystals in volcanic fumaroles.

## Characteristics Mellizinkalite is a potassium zinc halide, occurring as very small, colorless, tabular or lath-like crystals, which usually do not exceed 0.2 mm. These crystals form aggregates and coatings. Due to their size and mode of occurrence, visual features are difficult to observe without specialized equipment, such as an electron microscope. ## Physical Properties Mellizinkalite crystals exhibit a vitreous luster. They are transparent and colorless. Hardness and density have not been precisely measured due to the small size of the samples. ## History and Name The mineral was approved by the IMA in 2011. Its name comes from the Greek words μέλλω (mello - "future" or "coming") and "zink" (zinc), referring to the fact that the existence of a synthetic analogue K₃Zn₂Cl₇ was known before its natural occurrence was discovered. The discovery was made on material from the 1906 and 1944 eruptions of Mount Vesuvius in Italy.

Properties

Color
Yellow-brown to reddish brown
Luster
Vitreous
Streak
White
Density
2.46
Cleavage
Perfect on {0001}
Fracture
Irregular/Uneven
Transparency
Transparent
Crystal system
Triclinic

Diagnostic features

## Identification Identification of mellizinkalite is impossible without advanced laboratory techniques, such as X-ray diffraction (XRD) and chemical analysis using an electron microprobe (EDS/WDS). In collecting or field conditions, identification is unfeasible. A characteristic feature is its occurrence in the specific environment of volcanic fumaroles. ## Differentiation from Similar Minerals It can be confused with other fine-crystalline, colorless halides found in the same environment, such as salammoniac (NH₄Cl) or halite (NaCl). Differentiation requires specialized analysis of chemical composition and crystal structure. ## Crystal Forms It forms very small, thin, tabular crystals with a hexagonal outline, often elongated and lath-like. It occurs as single, dispersed crystals or small, loose aggregates.

Geological environment

## Genesis Mellizinkalite is a mineral of volcanic origin. It forms by direct sublimation from volcanic gases (exhalations) in the environment of active fumaroles. It crystallizes at high temperatures from gases rich in chlorine, potassium, and zinc. ## Mineral Associations It co-occurs with other fumarolic minerals, such as salammoniac, halite, sylvite, cotunnite, as well as various metal chlorides, e.g., zinc and copper. ## Localities The only confirmed locality of mellizinkalite in the world is the Vesuvius-Somma volcanic complex in Campania, Italy. It has been identified in exhalative products associated with historical eruptions.

Rarity

Extremely rare

For collectors

## Quality Criteria As a "micromount" type mineral, the collector's value of a specimen primarily depends on the confirmation of its identity by a reputable laboratory. Samples with well-formed, though still microscopic, crystals that are rich in mellizinkalite and embedded on a stable matrix are most highly valued. Precise documentation of the locality and analysis is crucial. ## Popular Localities The only source of specimens is the fumaroles on Mount Vesuvius in Italy. Material from this location is highly prized by collectors specializing in systematic minerals and "micromounts."

Care and storage

## Cleaning Due to its extreme rarity, small crystal size, and water solubility, mellizinkalite specimens should not be cleaned in any way. Any attempt at cleaning risks irreversible destruction of the mineral. ## What to Avoid Contact with water, water vapor, and all chemicals must be absolutely avoided, as the mineral is hygroscopic and easily soluble. It must be protected from atmospheric moisture, temperature changes, and any shocks or vibrations. ## Storage Mellizinkalite specimens must be stored in specialized, airtight containers (so-called micromount boxes) under controlled, very low humidity conditions. Storage in a dry place, away from light and heat sources, is absolutely crucial for preserving the sample.

External references

Sources

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