Asbecasite
4 in the gallery
Asbecasite is a complex silicate mineral in which sodium and calcium occupy the large cation sites, paired with iron in mixed valence states and aluminum in a framework of silicate tetrahedra. The mineral typically forms small to medium crystals and aggregates with a dull to pearly luster, often displaying earthy to reddish-brown hues. It occurs in hydrothermal and pegmatitic environments where alkali-rich fluids interact with aluminous silicates, and it is most notably represented by specimens from Switzerland, among other localities. Asbecasite crystals can be prismatic or granular, and the mineral’s appearance is influenced by iron oxidation states, giving color variation that appeals to collectors seeking color zoning and mineralogical complexity.
- Formula
- Ca3TiAs6Be2Si2O20
- Rarity
- Ultra Rare
- Stability
- Stable
- Collector interest
- Moderate Interest
- Classification notes
- Silicate; calcium titanium beryllium arsenic silicate, Strunz class 9
Key characteristics
- Crystal system
- orthorhombic
- Mohs hardness
- 6
- Specific gravity
- 3.7–3.8
- Luster
- vitreous, adamantine
- Transparency
- transparent, translucent
- Color
- yellow, orange, brown, red
- Streak
- white
- Cleavage
- none
- Fracture
- conchoidal, uneven
- Crystal habit
- prismatic, acicular, granular
- Micro-mount only
Where Asbecasite is found
Top localities
- Wanni glacier - Scherbadung area4 specimens
About Asbecasite
Collectors prize asbecasite for its rarity and the insight it provides into alkaline, aluminous hydrothermal systems. Although not the most common mineral, high-quality specimens exhibit well-formed crystals and aesthetically pleasing aggregates that photograph well and display the subtle interplay of color and luster. Localities such as Swiss occurrences contribute to its appeal, offering material that is sought after by those who specialize in complex silicate minerals and alkali-containing phases, making asbecasite a compelling target for dedicated collectors building a diverse mineral cabinet.