Ustarasite is a rare lead bismuth sulfide mineral typically found in complex hydrothermal deposits. It is best identified through laboratory analysis as it visually resembles several other lead-bismuth sulfosalts, typically appearing as massive metallic gray aggregates.
Is this ustarasite?
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 ustarasite with a known reference. Ustarasite 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. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray, silver gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic.
Often confused with
Ustarasite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ustarasite
Minerals reported to co-occur with ustarasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb(Bi,Sb)₆S₁₀
- Mohs hardness
- 2.5
- Density
- 6.8 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic
- Cleavage
- One perfect; another present
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In quartz-bismuthinite veins (Ustarasai deposit, Uzbekistan)
Where rockhounds find ustarasite
Classic worldwide localities
- Ustarasai bismuth deposit, near Brichmulla, Pskem Mountains, southern Tien-Shan, northeastern Uzbekistan (type locality)
- Pangushan tungsten deposit, Huang sha district, Jiangxi Province, China
Field-hunting tip
Where it forms: In quartz-bismuthinite veins (Ustarasai deposit, Uzbekistan). If you start seeing bismuthinite, kobellite, bismuthian jamesonite in float, you are in the right ground. Typical habit: prismatic. Train your eye for that shape before scanning the outcrop.





