Baratovite is a very rare phyllosilicate mineral primarily known from the alkaline pegmatites of the Dara-i-Pioz massif. It typically forms thin, white to pale pink platy or lamellar crystals that display a distinct pearly luster.
Is this baratovite?
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 baratovite with a known reference. Baratovite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Baratovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Baratovite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, lamellar aggregates.
Often confused with
Baratovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside baratovite
Minerals reported to co-occur with baratovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KLi₃Ca₇Ti₂Si₁₂O₃₆F₂
- Mohs hardness
- 5-6
- Density
- 2.86 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Lamellar Aggregates
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-500 depending on specimen quality
Where rockhounds find baratovite
Classic worldwide localities
- Dara-i-Pioz Glacier, Tajikistan
Field-hunting tip
Look in alkaline pegmatites country, the host setting where baratovite typically forms. If you start seeing aegirine, fluorite, quartz in float, you are in the right ground. Field specimens usually show a platy crystals, lamellar aggregates habit, so train your eye for that shape before scanning the outcrop.






