Bazhenovite is a rare calcium-sulfur-bearing mineral known primarily from the Bazhenovskoye asbestos deposit in Russia. It typically forms thin, yellowish, platy or lamellar crystals within the cavities of altered serpentinite rocks.
Is this bazhenovite?
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 bazhenovite with a known reference. Bazhenovite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bazhenovite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Bazhenovite typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: lamellar to platy crystals.
Often confused with
Bazhenovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bazhenovite
Minerals reported to co-occur with bazhenovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₈S₅(S₂O₃)(OH)₁₂·20H₂O
- Mohs hardness
- 2
- Density
- 2.47 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Lamellar to Platy Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Serpentinite and Altered Skarn Environments
- Typical price
- $50-500 depending on specimen quality
Where rockhounds find bazhenovite
Classic worldwide localities
- Bazhenovskoye deposit, Ural Mountains, Russia
Field-hunting tip
Look in serpentinite and altered skarn environments country, the host setting where bazhenovite typically forms. If you start seeing ettringite, calcites, hydrocalumite in float, you are in the right ground. Field specimens usually show a lamellar to platy crystals habit, so train your eye for that shape before scanning the outcrop.



