Miessiite is a rare palladium telluride-selenide mineral typically found as microscopic grains within massive sulfide ore bodies. It is primarily identified through electron microprobe analysis due to its minute size and close association with other platinum-group minerals.
Is this miessiite?
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 miessiite with a known reference. Miessiite 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. Miessiite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Miessiite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral to subhedral grains.
Often confused with
Miessiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside miessiite
Minerals reported to co-occur with miessiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₁₁Te₂Se₂
- Mohs hardness
- 2
- Density
- 9.5 g/cm³
- Colors
- Streak
- White
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Mafic-ultramafic Igneous Rocks
- Typical price
- $100-500 for micro-mounts
Where rockhounds find miessiite
Classic worldwide localities
- Miessi, Finland
- Stillwater Complex, USA
Field-hunting tip
Look in mafic-ultramafic igneous rocks country — that is the host setting where miessiite typically forms. If you start seeing chalcopyrite, pentlandite, pyrrhotite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains habit, so train your eye for that shape before scanning the outcrop.




