Tsilaisite
Chemical formula: NaMn²⁺₃Al₆(Si₆O₁₈)(BO₃)₃(OH)₃OH
Tsilaisite is a manganese-rich tourmaline characterized by its yellow, yellowish-green, or black color, valued by collectors for its rarity and intense hue.
Properties
- Mohs hardness
- 7
- Color
- Greenish yellow
- Luster
- Vitreous
- Streak
- White
- Density
- 0
- Cleavage
- None
- Fracture
- Sub-Conchoidal
- Transparency
- Transparent to translucent
- Crystal system
- Trigonal
Diagnostic features
## Identification Key diagnostic features of tsilaisite include its characteristic yellow to yellowish-green color, prismatic crystal habit with typical tourmaline vertical striations on the faces, and high hardness (7 on the Mohs scale). Strong pleochroism is also an important indicator. ## Distinguishing from Similar Minerals Yellow tsilaisite can be confused with other yellow minerals such as beryl (heliodor), citrine, or some varieties of apatite. However, it is distinguished by its higher hardness than apatite, characteristic triangular cross-section of the crystal (in contrast to hexagonal in beryl), and lack of cleavage. Distinguishing it from other tourmalines, such as elbaite or dravite, requires advanced chemical analysis to confirm the dominance of manganese. ## Crystal Forms Tsilaisite forms columnar, prismatic crystals, often with rounded, triangular faces in cross-section. Characteristic vertical striations are almost always visible on the prism faces. It also occurs as radial aggregates, acicular forms, or as granular masses embedded in rock.
Geological environment
## Genesis Tsilaisite, like other lithium tourmalines, crystallizes in granitic pegmatites, especially in their complex zones rich in lithium, boron, and manganese. It forms during the late stages of magma crystallization under hydrothermal conditions. ## Mineral Associations This mineral often co-occurs with other minerals typical of pegmatites, such as quartz, albite (especially cleavelandite), microcline, lepidolite, spodumene, beryl, and other tourmaline varieties (elbaite, schorl). ## Localities The most important and historical locality, which is the type locality, is in Madagascar in the Tsilaizina Mountain region. Specimens have also been found in pegmatites in Zambia, Mozambique, and in small quantities in Brazil (Minas Gerais) and Italy (Elba).
Rarity
Rare
For collectors
## Quality Criteria The most highly prized tsilaisite specimens are those that form well-developed, transparent crystals with an intense, pure, canary-yellow color. Crystal size and luster are also important. Specimens on rock matrix, especially in association with other pegmatite minerals (e.g., albite), are more desirable than single, isolated crystals. ## Popular Localities Collectors most seek specimens from the type locality in Madagascar, which are considered classic. High-quality crystals also come from Zambia, which often feature a beautiful greenish-yellow color.
Care and storage
## Cleaning Tsilaisite specimens can be safely cleaned with lukewarm water and a mild soap, using a soft brush. After washing, they should be thoroughly rinsed, preferably with distilled water, and left to air dry completely or gently blotted with a soft cloth. ## What to Avoid Avoid contact of the mineral with strong chemicals, acids, and bases, which can damage its surface. Cleaning in ultrasonic cleaners or steam cleaners is not recommended. Tsilaisite is sensitive to sudden temperature changes, which can cause internal fractures. ## Storage Tsilaisite crystals, especially those on delicate rock matrix, should be stored in separate boxes or display cases to prevent scratching by other, harder minerals. It is advisable to protect them from prolonged exposure to direct sunlight, which theoretically may affect color intensity.