Petrovskaite is a very rare silver gold sulfide mineral found in epithermal ore deposits. It typically occurs as microscopic anhedral grains intergrown with other telluride minerals and native gold.
Is this petrovskaite?
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 petrovskaite with a known reference. Petrovskaite 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. Petrovskaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Petrovskaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral grains, interstitial.
Often confused with
Petrovskaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside petrovskaite
Minerals reported to co-occur with petrovskaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- AgAuS
- Mohs hardness
- 2
- Density
- 7.96 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral Grains, Interstitial
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Gold-telluride Deposits
- Typical price
- n/a
Where rockhounds find petrovskaite
Classic worldwide localities
- Petrovsk-Zabaykalsky, Russia
Field-hunting tip
Look in epithermal gold-telluride deposits country — that is the host setting where petrovskaite typically forms. If you start seeing gold, tellurobismuthite, petzite in float, you are in the right ground. Field specimens usually show a anhedral grains, interstitial habit, so train your eye for that shape before scanning the outcrop.






