Vasilseverginite
Chemical formula: Cu²⁺₉O₄(As⁵⁺O₄)₂(S⁶⁺O₄)₂
Vasilseverginite is a very rare copper arsenate-sulfate, forming microscopic, tabular crystals of an intense green color.
Properties
- Mohs hardness
- 3
- Color
- Bright green
- Luster
- Vitreous
- Streak
- Light green
- Density
- 4.409
- Cleavage
- Perfect on {100}
- Fracture
- Irregular/Uneven
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of vasilseverginite is based on its characteristic, intense green color, specific form of microscopic, tabular crystals forming rosette-like aggregates, and its origin. Certain identification requires advanced analytical methods, such as Raman spectroscopy or chemical analysis (EDS). ## Distinguishing from similar minerals It can be confused with other secondary green copper minerals, such as brochantite, linarite, malachite, or euchroite. Differentiation with the naked eye is practically impossible. Vasilseverginite is distinguished by its unique chemical composition (it is both an arsenate and a sulfate) and specific crystal habit, visible under high magnification. ## Crystal forms It forms very small, thin, tabular crystals, often with a hexagonal or rhombic outline. These crystals group into radial or rosette-like aggregates, and also form thin crusts and coatings on the host rock.
Geological environment
## Genesis Vasilseverginite is a fumarolic mineral. It forms as a result of volcanic exhalations, where hot gases rich in copper, arsenic, and sulfur react with volcanic rocks in an oxygen-rich environment. It crystallizes in zones with temperatures around 100-150°C. ## Mineral associations It coexists with other rare fumarolic minerals, such as tenorite, hematite, aphthitalite, langbeinite, anorthite, lammerite, eriostevensite, popovite, urusovite, arsmirandite, and johillerite. ## Localities The only confirmed occurrence of this mineral in the world is its type locality – the Arsenatnaya fumarole field on the second cinder cone of the northern breach of the Great Fissure Eruption of Tolbachik (1975-1976) on Tolbachik volcano, Kamchatka, Russia.
Rarity
Very rare
For collectors
## Quality criteria The quality of vasilseverginite specimens is assessed primarily based on the richness and aesthetics of the crystalline aggregates. Most valued are specimens with clearly formed, rosette-like clusters of an intense, emerald-green color, contrasting with a lighter host rock. Due to the microscopic nature of the mineral, the quality of the photograph taken under a microscope (so-called photomicrography) is crucial. ## Popular localities All known collector specimens come from a single location in the world – Tolbachik volcano in Kamchatka, Russia. Material from this locality is extremely rare and sought after by collectors specializing in systematic minerals and micromounts.
Care and storage
## Cleaning Specimens should only be cleaned with compressed air to remove dust. Due to extreme delicacy and reactivity, any contact with water, chemical solutions, or even a damp cloth should be avoided. ## What to avoid Contact with water and acids, which can damage or dissolve it, must be strictly avoided. The mineral is sensitive to changes in temperature and humidity. It should not be heated or exposed to direct sunlight. ## Storage Vasilseverginite specimens should be stored in airtight, sealed containers (e.g., "micromount boxes") away from dust, moisture, and heat sources. It is best to store them under stable room conditions.