Atokite is a rare palladium-tin alloy typically found as minute grains within platinum-group mineral deposits. It is most commonly identified through microscopic analysis of polished sections in ore bodies, particularly within layered igneous complexes.
Is this atokite?
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 atokite with a known reference. Atokite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Atokite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside atokite
Minerals reported to co-occur with atokite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₃Sn
- Mohs hardness
- 5
- Density
- 14.9 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As very sparse grains in concentrates of ore (Merensky Reef, South Africa)
Where rockhounds find atokite
Classic worldwide localities
- Atok (type locality) and Rustenburg mines, on the Merensky Reef, Bushveld complex, Transvaal, South Africa
- Oktyabr mine, Talnakh area, Noril’sk region, western Siberia, Russia
Field-hunting tip
Where it forms: As very sparse grains in concentrates of ore (Merensky Reef, South Africa). If you start seeing unspecified platinum tellurides, keithconnite, palladoarsenide in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.

