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, 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.







