Skaergaardite is a rare palladium-copper intermetallic mineral that typically occurs as microscopic inclusions within other metallic minerals. It is primarily recognized as a significant component of platinum-group element mineralization in layered igneous complexes.
Is this skaergaardite?
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 skaergaardite with a known reference. Skaergaardite 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. Skaergaardite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Skaergaardite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: cubic. Typical habit: microscopic grains.
Often confused with
Skaergaardite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside skaergaardite
Minerals reported to co-occur with skaergaardite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdCu
- Mohs hardness
- 3.5
- Density
- 9.9 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microscopic Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Mafic Igneous Layered Intrusions
Where rockhounds find skaergaardite
Classic worldwide localities
- Skaergaard intrusion, Greenland
- Stillwater Complex, USA
- Bushveld Complex, South Africa
Field-hunting tip
Look in mafic igneous layered intrusions country, the host setting where skaergaardite typically forms. If you start seeing magnetite, ilmenite, bornite in float, you are in the right ground. Field specimens usually show a microscopic grains habit, so train your eye for that shape before scanning the outcrop.




