Babkinite is an extremely rare lead-bismuth sulfoselenide-telluride mineral known primarily from epithermal gold-telluride deposits. It is usually found as microscopic inclusions or intergrowths with other lead minerals and tellurides, making it difficult for collectors to acquire as a macro specimen.
Is this babkinite?
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 babkinite with a known reference. Babkinite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Babkinite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Babkinite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, tin-white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral grains, interstitial masses.
Often confused with
Babkinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside babkinite
Minerals reported to co-occur with babkinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Bi₂S₃Se₂Te
- Mohs hardness
- 2.5
- Density
- 8.06 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral Grains, Interstitial Masses
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Gold Deposits
Where rockhounds find babkinite
Classic worldwide localities
- Kochbulak deposit, Uzbekistan
Field-hunting tip
Look in epithermal gold deposits country, the host setting where babkinite typically forms. If you start seeing galena, gold, chalcopyrite in float, you are in the right ground. Field specimens usually show a anhedral grains, interstitial masses habit, so train your eye for that shape before scanning the outcrop.




