Lavoisierite
Chemical formula: Mn²⁺₈[Al₁₀(Mn³⁺Mg)][Si₁₁P]O₄₄(OH)₁₂
Lavoisierite is a very rare silicate mineral, discovered in Spain, with a complex chemical composition containing manganese, aluminum, and phosphorus.
Properties
- Color
- Yellow-orange
- Luster
- Vitreous
- Streak
- White
- Density
- 3.576
- Cleavage
- Perfect on {0001}
- Transparency
- Translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Identification of lavoisierite is impossible without advanced laboratory techniques, such as Raman spectroscopy, electron microprobe (EDS/WDS), and X-ray diffraction (XRD). In collector conditions, identification relies on a label from a confirmed locality. Visually, only orange-brown, microscopic, rosette-like aggregates on the matrix rock can be observed. ## Distinguishing from Similar Minerals Due to its unique chemical composition and structure, there are no minerals with which it could be directly confused after chemical analysis. Visually, it may resemble other microscopic silicates of similar color and habit, but certain differentiation is only possible through analytical methods. ## Crystal Forms Lavoisierite forms very small, thin, platy crystals with a hexagonal outline. These crystals combine into characteristic rosette-like or spherulitic (spherical) aggregates.
Geological environment
## Genesis Lavoisierite forms as a result of hydrothermal or low-grade metamorphic processes acting on manganese-rich sedimentary rocks. At its type locality (Fuente del Moro mine in Spain), it occurs in veins cutting radiolarites (siliceous rocks) mineralized with manganese oxides. ## Mineral Associations This mineral co-occurs with other manganese minerals and silicates. At the discovery site, it was found in association with quartz, alleghanyite, piemontite, rhodonite, tephroite, bementite, ganophyllite, aegirine, and manganese oxides. ## Localities The only confirmed occurrence of lavoisierite in the world is its type locality: Fuente del Moro mine, near Viñuela, in the province of Malaga, Andalusia (Spain).
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a lavoisierite specimen primarily depends on the abundance and visibility of microscopic aggregates on the matrix rock. The most prized samples are those where rosette-like clusters are numerous, well-formed, and contrast with the substrate. The size of the aggregates, although always microscopic, is also important – larger spherulites are more desirable. Analytical confirmation of the mineral's identity is crucial for its value. ## Popular Localities The only source of lavoisierite specimens is the Fuente del Moro mine in Spain, which is its type locality.
Care and storage
## Cleaning Lavoisierite specimens are extremely delicate and small, usually occurring as coatings on the matrix rock. Mechanical or chemical cleaning is not recommended. If necessary, compressed air (from a safe distance) can be used to remove dust. ## What to Avoid Avoid contact with any chemicals, acids, and detergents. Do not subject it to ultrasonic cleaning. Protect from high temperatures and sudden temperature changes. Due to its microscopic nature, avoid any touching or abrading of the specimen's surface. ## Storage Specimens should be stored in stable conditions, in sealed "micromount" containers, to protect them from dust, moisture, and mechanical damage. There are no special requirements regarding light exposure.