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 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Atokite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Atokite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 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
- 3.5-4
- 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
- Ultramafic Igneous Rocks
- Typical price
- $50-300 per micro-mount
Where rockhounds find atokite
Classic worldwide localities
- Bushveld Igneous Complex, South Africa
- Stillwater Complex, USA
- Norilsk, Russia
Field-hunting tip
Look in ultramafic igneous rocks country — that is the host setting where atokite typically forms. If you start seeing sperrylite, cooperite, braggite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.






