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?
4-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.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: dark gray.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: granular.
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
- 7.258 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As grains in heavy-mineral concentrates derived from drill-core from ultramafic rocks
Where rockhounds find ungavaite
Classic worldwide localities
- Mesamax Northwest Ni-Cu-Co-PGE deposit, in the Cape Smith fold belt of the Ungava region, northern Quebec, Canada
Field-hunting tip
Where it forms: As grains in heavy-mineral concentrates derived from drill-core from ultramafic rocks. If you start seeing chalcopyrite, cobaltite, galena in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.







