Petrovicite is an extremely rare copper mercury lead bismuth selenide mineral first identified in the Predborice uranium deposit. It typically occurs as minute grains in association with other rare selenides and is mainly of interest to advanced micro-mineral collectors.
Is this petrovicite?
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 petrovicite with a known reference. Petrovicite sits at Mohs ~3, 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: strong metallic.
- 4Match the color rangeCompare against the expected color range: gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: microscopic crystals, tabular.
Often confused with
Petrovicite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Petrovicite leaves black, Clausthalite leaves grayish black; luster reads strong metallic on Petrovicite and metallic on Clausthalite.

How to tell apart: Streak differs, so Petrovicite leaves black, Berzelianite leaves shining; luster reads strong metallic on Petrovicite and metallic on Berzelianite.
Often found alongside petrovicite
Minerals reported to co-occur with petrovicite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃HgPbBiSe₅
- Mohs hardness
- ~3
- Density
- 7.707 g/cm³
- Colors
- Streak
- Black
- Luster
- Strong metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Microscopic crystals, tabular
- Cleavage
- Imperfect, parallel to flattening of crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermal dolomite-calcite veins with other selenides
Where rockhounds find petrovicite
Classic worldwide localities
- Petrovice uranium deposit, near Ždǎr, Czech Republic (type locality)
Field-hunting tip
Where it forms: In hydrothermal dolomite-calcite veins with other selenides. If you start seeing berzelianite, eucairite, crookesite in float, you are in the right ground. Typical habit: microscopic crystals, tabular. Train your eye for that shape before scanning the outcrop.





