Ungavaite is a very rare palladium-antimony mineral typically found as microscopic grains within sulfide-rich nickel-copper deposits. It is known primarily from its type locality in the Ungava region of Canada and requires professional analysis for positive identification.
Is this ungavaite?
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 ungavaite with a known reference. Ungavaite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ungavaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Ungavaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Ungavaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ungavaite
Minerals reported to co-occur with ungavaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₄Sb₃
- Mohs hardness
- 3-3.5
- Density
- 9.7 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nickel-copper Sulfide Deposits
- Typical price
- $500-2000+ for rare micro-specimens
Where rockhounds find ungavaite
Classic worldwide localities
- Gordon Lake area, Northwest Territories, Canada
Field-hunting tip
Look in nickel-copper sulfide deposits country — that is the host setting where ungavaite typically forms. If you start seeing pentlandite, chalcopyrite, pyrrhotite 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.




