Spiridonovite is an extremely rare platinum telluride mineral typically found as microscopic inclusions within platinum-group element deposits. It is known primarily from layered ultramafic complexes where it forms during the late stages of magmatic crystallization.
Is this spiridonovite?
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 spiridonovite with a known reference. Spiridonovite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Spiridonovite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Spiridonovite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: grains.
Often confused with
Spiridonovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside spiridonovite
Minerals reported to co-occur with spiridonovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PtTe₃
- Mohs hardness
- 3.5
- Density
- 9.18 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Ultramafic Igneous Rocks
- Typical price
- $100-500 micro-mount
Where rockhounds find spiridonovite
Classic worldwide localities
- Konder Massif, Russia
- Norilsk, Russia
Field-hunting tip
Look in ultramafic igneous rocks country, the host setting where spiridonovite typically forms. If you start seeing platinum, sperrylite, chalcopyrite in float, you are in the right ground. Field specimens usually show a grains habit, so train your eye for that shape before scanning the outcrop.





