Kashinite is an extremely rare iridium sulfide mineral typically found as microscopic grains in alluvial platinum deposits. Because of its rarity and size, it is strictly a professional research or advanced private collector species that requires micro-analysis for positive identification.
Is this kashinite?
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 kashinite with a known reference. Kashinite sits at Mohs 7.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray, black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral grains.
Often confused with
Kashinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kashinite
Minerals reported to co-occur with kashinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ir₂S₃
- Mohs hardness
- 7.5
- Density
- 9.1 g/cm³
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In placer deposits derived from ultramafic rocks
Where rockhounds find kashinite
Classic worldwide localities
- Goodnews Bay, Alaska, USA
- Aleksandrov Log platinum deposit, Mt. Solov’eva, Nizhni Tagil massif, Ural Mountains (type locality), Russia
- Ray-Iz ophiolite complex, Polar Ural Mountains, Russia
- Vaimka River placers, Aluchinskii massif, and the Baimka placers, Aluchin horst, Chukota region, Far Eastern Region, Russia
- Chromwerk, Kraubath ultramafic massif, Styria, Austria
Field-hunting tip
Where it forms: In placer deposits derived from ultramafic rocks. If you start seeing iridosmine, platinum, osmiridium in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.





