Miassite is a very rare rhodium sulfide mineral first discovered in the Ural Mountains. It is typically found as microscopic inclusions within platinum group mineral assemblages in ultramafic rocks, making it a highly sought-after specimen for advanced mineral collectors.
Is this miassite?
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 miassite with a known reference. Miassite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Miassite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Miassite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Miassite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside miassite
Minerals reported to co-occur with miassite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Rh₁₇S₁₅
- Mohs hardness
- 3.5-4
- Density
- 9.35 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Igneous Rocks
- Typical price
- $100-500 for micro-mounts
Where rockhounds find miassite
Classic worldwide localities
- Miass, Ural Mountains, Russia
- Konder Massif, Russia
- Stillwater Complex, USA
Field-hunting tip
Look in ultramafic igneous rocks country — that is the host setting where miassite typically forms. If you start seeing platinum group minerals, chromite, magnetite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.





