Isomertieite is a rare palladium antimony arsenide mineral typically found as microscopic inclusions within platinum-group element deposits. It is most often identified through reflected light microscopy or microprobe analysis in polished sections from ultramafic complexes. It is a highly sought-after species for specialist mineral collectors of platinum group minerals.
Is this isomertieite?
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 isomertieite with a known reference. Isomertieite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Isomertieite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Isomertieite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, light yellow, silver-white.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains, inclusions.
Often confused with
Isomertieite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside isomertieite
Minerals reported to co-occur with isomertieite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₁₁Sb₂As₂
- Mohs hardness
- 3.5
- Density
- 9.94 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains, Inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Igneous Rocks
Where rockhounds find isomertieite
Classic worldwide localities
- Stillwater Complex, USA
- Bushveld Complex, South Africa
- Kondyor Massif, Russia
Field-hunting tip
Look in ultramafic igneous rocks country, the host setting where isomertieite typically forms. If you start seeing sperrylite, palladium, chalcopyrite in float, you are in the right ground. Field specimens usually show a anhedral grains, inclusions habit, so train your eye for that shape before scanning the outcrop.





