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, 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.






