Stergiouite
Chemical formula: CaZn<sup>2+</sup><sub>2</sub>(As<sup>5+</sup>O<sub>4</sub>)<sub>2</sub>·4H<sub>2</sub>O
Stergiouite is a hydrated calcium zinc arsenate, forming colorless, platy crystals with a pearly luster, found in the Lavrion mines in Greece.
Properties
- Mohs hardness
- 2
- Luster
- Pearly, Vitreous
- Streak
- White
- Density
- 3.43
- Cleavage
- Perfect on {010}
- Fracture
- Micaceous
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Stergiouite is recognized by its unique appearance: it forms colorless, very thin, platy crystals with a strong pearly luster, often gathered into small, rosette-like aggregates. Key factors are its occurrence locality (Hilarion mine in Lavrion) and its association with other rare arsenates. ## Differentiation from similar minerals It can be confused with other microscopic, colorless secondary minerals, such as gypsum or talc, due to similar luster and low hardness. However, the unique crystal habit (thin plates in rosettes), flexibility, and specific geochemical environment (oxidized zone of a polymetallic deposit rich in arsenic) allow for its differentiation. Final identification requires advanced analytical methods, such as Raman spectroscopy or chemical analysis (EDS). ## Crystal forms The crystals are thin-platy, with a bladed or lamellar habit, dominated by the {010} face. They typically form rosette-like, fan-shaped, or spherulitic aggregates up to 0.4 mm in diameter.
Geological environment
## Genesis Stergiouite is a secondary mineral that forms in the oxidation zone (gossan) of polymetallic (Zn-Pb-Ag) deposits. It crystallizes in voids within arsenic-rich rocks as a result of low-temperature hydrothermal processes. ## Mineral associations This mineral occurs in association with other, often rare, secondary minerals. In its type locality (Hilarion mine), it was found in association with annabergite, gypsum, quartz, sericite, sphalerite, galena, pyrite, and goethite. ## Localities The only confirmed occurrence of stergiouite in the world is its type locality: Hilarion Mine (shaft no. 3), Kamariza, in the Lavrion district, Attica region, Greece.
Rarity
Extremely rare
For collectors
## Quality criteria The quality of stergiouite specimens is primarily assessed based on the richness and aesthetics of the crystal aggregates. Samples with well-formed, distinct rosettes or spherulites that contrast with the rock matrix are most highly valued. The size of the aggregates (though always microscopic) and the absence of damage also influence value. The clarity and transparency of individual crystals within the aggregate are an additional asset. ## Popular localities The only source of stergiouite specimens is the Hilarion mine in Lavrion, Greece. Specimens from this locality are highly sought after by collectors specializing in systematic minerals and rare micromounted minerals.
Care and storage
## Cleaning Stergiouite specimens should be handled with utmost care. Due to the microscopic size and fragility of the crystals, mechanical cleaning is not recommended. If absolutely necessary, compressed air can be used from a safe distance to remove loose dust particles. Avoid contact with water and any chemicals. ## What to avoid The mineral is very soft (hardness 2), so any physical contact that could scratch or damage it should be avoided. It must be protected from moisture, acids, and other chemical agents. As an arsenate, mineral dust is toxic – avoid inhaling it and wash hands after any contact. ## Storage Stergiouite should be stored exclusively in specialized micromount boxes, which protect it from dust, moisture, and mechanical damage. Display should only be done under a microscope.