Omeiite is an extremely rare osmium arsenide found primarily in platinum-group element bearing deposits. It typically occurs as small, metallic grains, often requiring microscopic study for positive identification due to its similarity to other arsenide minerals.
Is this omeiite?
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 omeiite with a known reference. Omeiite sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Omeiite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Omeiite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: tin-white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral to subhedral grains.
Often confused with
Omeiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside omeiite
Minerals reported to co-occur with omeiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- OsAs₂
- Mohs hardness
- 4-5
- Density
- 9.5 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Intrusive Complexes
- Typical price
- $100-500+ for micros and small specimens
Where rockhounds find omeiite
Classic worldwide localities
- Emei Mountain, Sichuan Province, China
- various platinum-group element deposits
Field-hunting tip
Look in ultramafic intrusive complexes country — that is the host setting where omeiite typically forms. If you start seeing platinum, irarsite, chalcopyrite 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.






