Kalungaite is a very rare palladium arsenic selenide mineral primarily found in hydrothermal deposits. It is typically identified as tiny, metallic, opaque grains associated with other sulfides and sulfosalts.
Is this kalungaite?
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 kalungaite with a known reference. Kalungaite sits at Mohs 4-5, 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: lead gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Kalungaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kalungaite
Minerals reported to co-occur with kalungaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdAsSe
- Mohs hardness
- 4-5
- Density
- 7.59 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a hydrothermal gold deposit in quartz-muscovite-rich zones of a mylonite cutting peraluminous granite
Where rockhounds find kalungaite
Classic worldwide localities
- Buraco do Ouro gold mine, Cavalcante town, Goiás State, central Brazil
Field-hunting tip
Where it forms: In a hydrothermal gold deposit in quartz-muscovite-rich zones of a mylonite cutting peraluminous granite. If you start seeing gold, bohdanowicszite, guanajuatite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.







