Zavaritskite is a rare bismuth oxyfluoride mineral typically found as small, pearly, platy crystals or coatings in oxidized bismuth-bearing deposits. It is most easily identified by its association with secondary bismuth minerals in pegmatite environments or hydrothermal zones.
Is this zavaritskite?
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 zavaritskite with a known reference. Zavaritskite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Zavaritskite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Zavaritskite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, white, gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: platy crystals, granular aggregates.
Often confused with
Zavaritskite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside zavaritskite
Minerals reported to co-occur with zavaritskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BiOF
- Mohs hardness
- 2-3
- Density
- 6.6 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Platy Crystals, Granular Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites, Hydrothermal Veins
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find zavaritskite
Classic worldwide localities
- Sherlovaya Gora, Russia
- Mount Malosa, Malawi
- Sahatany Pegmatite Field, Madagascar
Field-hunting tip
Look in granite pegmatites, hydrothermal veins country — that is the host setting where zavaritskite typically forms. If you start seeing bismutite, fluorite, topaz in float, you are in the right ground. Field specimens usually show a platy crystals, granular aggregates habit, so train your eye for that shape before scanning the outcrop.







