Palladseite is a rare palladium selenide mineral that typically forms as minute grains within hydrothermal PGE-bearing sulfide deposits. Due to its microscopic nature and rarity, it is a highly sought-after species for advanced mineral collectors specializing in platinum-group minerals.
Is this palladseite?
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 palladseite with a known reference. Palladseite sits at Mohs 4.5-5, 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: white.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular.
Often confused with
Palladseite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Palladseite is noticeably harder (Mohs 4.5-5 vs. 3.5); streak differs, so Palladseite leaves black, Potarite leaves silver-white.


How to tell apart: Sperrylite is the harder of the two (Mohs 6-7 vs. 4.5-5).
Often found alongside palladseite
Minerals reported to co-occur with palladseite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₁₇Se₁₅
- Mohs hardness
- 4.5-5
- Density
- 8.30 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- Sparingly in residual concentrates from gold washings (Itabira district, Brazil); in specularite and magnetite (Cauê mine, Itabira district, Brazil)
Where rockhounds find palladseite
Classic worldwide localities
- Minas Gerais, from gold placers in the Itabira district (type locality), and at the Cauê iron mine, Brazil
- Serra Pelada Au–Pd–Pt deposit, Pará, Brazil
Field-hunting tip
Where it forms: Sparingly in residual concentrates from gold washings (Itabira district, Brazil); in specularite and magnetite (Cauê mine, Itabira district, Brazil). If you start seeing arsenopalladinite, isomertieite, atheneite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.



