Sudburyite is a rare palladium antimonide mineral typically found as tiny metallic grains within massive sulfide deposits. It is most famous for its occurrence in the Sudbury Basin of Canada and is a prized find for advanced mineralogists and collectors of platinum-group element minerals.
Is this sudburyite?
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 sudburyite with a known reference. Sudburyite 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. Sudburyite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sudburyite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: grains.
Often confused with
Sudburyite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Sudburyite leaves white, Stibiopalladinite leaves black.
How to tell apart: Geversite is the harder of the two (Mohs 5.5 vs. 3.5); streak differs — Sudburyite leaves white, Geversite leaves black.
Often found alongside sudburyite
Minerals reported to co-occur with sudburyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdSb
- Mohs hardness
- 3.5
- Density
- 9.5 g/cm³
- Colors
- Streak
- White
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nickel-copper Sulfide Ores
- Typical price
- $50-300 per micro-mount
Where rockhounds find sudburyite
Classic worldwide localities
- Sudbury Basin, Ontario, Canada
- Stillwater Complex, Montana, USA
- Norilsk, Russia
Field-hunting tip
Look in nickel-copper sulfide ores country — that is the host setting where sudburyite typically forms. If you start seeing sperrylite, pentlandite, 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.




