Arzamastsevite
Chemical formula: K<sub>6</sub>Al<sub>5</sub>Si<sub>6</sub>O<sub>20</sub>(OH)<sub>4</sub>Cl
Arzamastsevite is a very rare silicate mineral, found as small, colorless to white crystals in alkaline massifs.
Properties
- Mohs hardness
- 3
- Luster
- Vitreous
- Streak
- White
- Density
- 2.61
- Cleavage
- Good on {100}
- Fracture
- Uneven
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of arzamastsevite is possible only by advanced analytical methods, such as X-ray diffraction (XRD) and electron microprobe analysis (EMPA). Visual identification in the field or even in a collection is impossible due to the microscopic size of the crystals and their similarity to many other white silicates. ## Distinguishing from similar minerals It can be confused with many other microscopic minerals found in similar environments, such as cancrinite, natrolite, or other zeolites. Certain differentiation requires specialized laboratory equipment. ## Crystal forms Arzamastsevite forms very small, thin, tabular or lath-like crystals, often grouped into small, radial or chaotic aggregates. Crystals rarely exceed 0.3 mm in length and 0.02 mm in thickness.
Geological environment
## Genesis Arzamastsevite forms in the late stages of hydrothermal processes in highly differentiated alkaline massifs. It is found in pegmatites and hydrothermal veins cutting nepheline syenites. ## Mineral associations This mineral coexists with aegirine, sodalite, microcline, nepheline, eudialyte, lorenzenite, lamprophyllite, as well as rarer minerals such as kazakovite, rasvumite, and villiaumite. ## Localities The only confirmed occurrence of arzamastsevite in the world is its type locality - Mount Nyorkpakhk (Niorkpakhk) in the Khibiny Massif on the Kola Peninsula in Russia.
Rarity
Very rare
For collectors
## Quality criteria As a "micromount" type mineral, the collectible value of arzamastsevite primarily depends on the quality of the host specimen and the richness of the mineral association. The most desirable specimens are those on which well-formed, albeit microscopic, aggregates of arzamastsevite crystals are visible, clearly contrasting with the matrix (e.g., dark aegirine). The certainty of identification, confirmed by the discoverer or a laboratory, is also crucial. ## Popular localities The only source of specimens is the Khibiny Massif on the Kola Peninsula in Russia. Specimens from this locality are the only authentic ones on the collector's market.
Care and storage
## Cleaning Specimens with arzamastsevite, usually micromounts, do not require cleaning. If absolutely necessary, compressed air can be used to remove dust. Avoid contact with water and any chemicals. ## What to avoid As a mineral with low hardness, it is very susceptible to mechanical damage. Avoid contact with hard objects, ultrasound, and any cleaning fluids. Protect it from high temperatures and humidity. ## Storage Arzamastsevite specimens should be stored exclusively in specialized micromount boxes that protect them from dust, shocks, and mechanical damage. Display is not recommended due to the small size of the crystals.