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, 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.





