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: trigonal. 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
- Trigonal
- Crystal habit
- Anhedral Grains, Inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Igneous Rocks
- Typical price
- $100-500 per specimen
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 — that is 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.





