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 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Palladseite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Palladseite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, anhedral grains.
Often confused with
Palladseite vs. its common look-alikes — and how to tell them apart in the field.
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
- 3-4
- Density
- 9.5-10.0 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Platinum-group Element (PGE) Deposits
- Typical price
- $100-500 per micro-mount or small specimen
Where rockhounds find palladseite
Classic worldwide localities
- Harz Mountains, Germany
- Stillwater Complex, USA
- Bushveld Igneous Complex, South Africa
- Norilsk, Russia
Field-hunting tip
Look in hydrothermal platinum-group element (pge) deposits country — that is the host setting where palladseite typically forms. If you start seeing gold, platinum, sperrylite in float, you are in the right ground. Field specimens usually show a massive, anhedral grains habit, so train your eye for that shape before scanning the outcrop.







