Boromuscovite is a rare boron-rich member of the mica group, structurally analogous to muscovite. It typically appears as colorless to pale-colored platy crystals or foliated aggregates, usually found in complex pegmatitic or metamorphic environments where boron enrichment occurs.
Is this boromuscovite?
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 boromuscovite with a known reference. Boromuscovite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Boromuscovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Boromuscovite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy, foliated, micaceous masses.
Often confused with
Boromuscovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside boromuscovite
Minerals reported to co-occur with boromuscovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KAl₂(AlSi₃O₁₀)(OH)₂
- Mohs hardness
- 2.5-3
- Density
- 2.8-2.9 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy, Foliated, Micaceous Masses
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphic Rocks, Pegmatites
- Typical price
- $20-100 per specimen
Where rockhounds find boromuscovite
Classic worldwide localities
- Sarany deposit, Russia
- Finland
- Brazil
Field-hunting tip
Look in metamorphic rocks, pegmatites country — that is the host setting where boromuscovite typically forms. If you start seeing quartz, feldspar, tourmaline in float, you are in the right ground. Field specimens usually show a platy, foliated, micaceous masses habit, so train your eye for that shape before scanning the outcrop.






