Laurite is a rare ruthenium sulfide mineral typically found as small, metallic black crystals within platinum group element (PGE) deposits. Collectors often find it as inclusions in chromite or alluvial placer deposits derived from ultramafic rocks. Due to its extreme rarity and high ruthenium content, it is highly prized by advanced mineralogists.
Is this laurite?
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 laurite with a known reference. Laurite sits at Mohs 7-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Laurite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Laurite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: iron-black, grayish-black.
- 5Look at form & habitCrystal system: cubic. Typical habit: small octahedra, pyritohedra, and cubic crystals.
Often confused with
Laurite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside laurite
Minerals reported to co-occur with laurite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- RuS₂
- Mohs hardness
- 7-7.5
- Density
- 6.42 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Small Octahedra, Pyritohedra, And Cubic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Ultramafic Igneous Rocks and Alluvial Deposits
- Typical price
- $100-500+ for high-quality micro-crystals
Where rockhounds find laurite
Classic worldwide localities
- Borneo (Malaysia)
- Bushveld Complex (South Africa)
- Urals (Russia)
- Ethiopia
Field-hunting tip
Look in ultramafic igneous rocks and alluvial deposits country — that is the host setting where laurite typically forms. If you start seeing platinum, osmium, chromite in float, you are in the right ground. Field specimens usually show a small octahedra, pyritohedra, and cubic crystals habit, so train your eye for that shape before scanning the outcrop.





