Bortnikovite is an extremely rare palladium-copper alloy first discovered in the Konder Massif of Russia. It typically occurs as minute, irregular grains embedded within platinum-group element (PGE) mineral assemblages found in ultramafic rocks.
Is this bortnikovite?
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 bortnikovite with a known reference. Bortnikovite sits at Mohs 4.5-5, 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: steel white.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: granular.
Often confused with
Bortnikovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bortnikovite
Minerals reported to co-occur with bortnikovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pd₄Cu₃Zn
- Mohs hardness
- 4.5-5
- Density
- 11.16 g/cm³
- Colors
- Steel white
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Granular
- Cleavage
- None observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As rims on isoferroplatinum grains in alluvial placer sediment derived from a concentrically zoned, alkaline ultramafic massif
Where rockhounds find bortnikovite
Classic worldwide localities
- Konder River PGM placer deposit, Ayan-Maya district, Khabarovsk region, Russia
Field-hunting tip
Where it forms: As rims on isoferroplatinum grains in alluvial placer sediment derived from a concentrically zoned, alkaline ultramafic massif. If you start seeing isoferroplatinum, titanite, perovskite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.






