Bityite is a rare lithium-bearing mica species that typically forms as small, pseudohexagonal tabular crystals. It is most commonly found in complex lithium-rich pegmatites and is often associated with other beryllium and lithium minerals.
Is this bityite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch bityite with a known reference. Bityite sits at Mohs 4-4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, pearly on cleavages.
- 4Match the color rangeCompare against the expected color range: brown white, colorless, yellow, pearl white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: encrustations, platy, pseudo hexagonal.
Often confused with
Bityite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bityite
Minerals reported to co-occur with bityite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaLiAl₂(AlBeSi₂)O₁₀(OH)₂
- Mohs hardness
- 4-4.5
- Density
- 3.02-3.05 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, pearly on cleavages
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Encrustations, platy, pseudo hexagonal
- Cleavage
- Perfect micaceous on {001}
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- A late-stage mineral in lithium-bearing pegmatites
Where rockhounds find bityite
2 mapped spotsClassic worldwide localities
- Strickland quarry, Portland, Middlesex Co., Connecticut, and the Harding pegmatite, Dixon, Taos Co., New Mexico, USA
- Maharitra, on Mt. Bity, Madagascar
- Namherere mine, Aukole, Uganda
- Huron claims, 16 km north of Point du Bois, Manitoba, Canada
- Pizzo Marcio, Val Vigezzo, Piedmont, Italy
- Maantienvarsi pegmatite dike, Eräjärvi pegmatite area, Orivesi, Finland
Field-hunting tip
Where it forms: A late-stage mineral in lithium-bearing pegmatites. If you start seeing tourmaline, albite, lepidolite in float, you are in the right ground. Typical habit: encrustations, platy, pseudo hexagonal. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New Mexico. Start trip planning there.








