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, 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.







