Erlichmanite is a rare osmium sulfide mineral usually found as microscopic grains in platinum-group mineral assemblages. It typically occurs in ultramafic rocks or heavy mineral placer deposits, identified by its metallic luster and high specific gravity.
Is this erlichmanite?
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 erlichmanite with a known reference. Erlichmanite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Erlichmanite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Erlichmanite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, iron-black.
- 5Look at form & habitCrystal system: cubic. Typical habit: small cubes and octahedra, granular.
Often confused with
Erlichmanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside erlichmanite
Minerals reported to co-occur with erlichmanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- OsS₂
- Mohs hardness
- 5-6
- Density
- 8.3-8.5 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Small Cubes and Octahedra, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Ultramafic Igneous Rocks and Placer Deposits
- Typical price
- $100-500 per specimen
Where rockhounds find erlichmanite
Classic worldwide localities
- Bushveld Complex, South Africa
- Goodnews Bay, Alaska, USA
- Tulameen complex, British Columbia, Canada
- Ural Mountains, Russia
Field-hunting tip
Look in ultramafic igneous rocks and placer deposits country — that is the host setting where erlichmanite typically forms. If you start seeing laurite, chromite, platinum group minerals in float, you are in the right ground. Field specimens usually show a small cubes and octahedra, granular habit, so train your eye for that shape before scanning the outcrop.





