Pašavaite is a rare palladium lead sulfide discovered in the polymetallic sulfide deposits of the Czech Republic. It typically occurs as minute, metallic grains within sulfide ores, requiring microscopic analysis for positive identification.
Is this pašavaite?
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 pašavaite with a known reference. Pašavaite 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. Pašavaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pašavaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals, massive.
Often confused with
Pašavaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pašavaite
Minerals reported to co-occur with pašavaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₃Pb₂S₂
- Mohs hardness
- 2
- Density
- 6.64 g/cm³
- Colors
- Streak
- White
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Tabular Crystals, Massive
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary-hosted Sulfide Deposits
- Typical price
- $50-300+ depending on specimen quality
Where rockhounds find pašavaite
Classic worldwide localities
- Pašava, Czech Republic
Field-hunting tip
Look in sedimentary-hosted sulfide deposits country — that is the host setting where pašavaite typically forms. If you start seeing chalcopyrite, pyrite, sphalerite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive habit, so train your eye for that shape before scanning the outcrop.





