Majakite is an extremely rare palladium-nickel arsenide mineral found primarily in copper-nickel sulfide deposits associated with layered igneous complexes. It typically occurs as tiny, metallic inclusions within other ore minerals, making identification difficult without microscopic analysis or electron microprobe study.
Is this majakite?
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 majakite with a known reference. Majakite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: microscopic crystals.
Often confused with
Majakite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside majakite
Minerals reported to co-occur with majakite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdNiAs
- Mohs hardness
- ~5
- Density
- 9.33 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- As intergrowths with other platinum-group minerals in chalcopyrite and talnakhite ores (Majak mine, Russia); in sulfide mineralization in a strongly metamorphosed layered intrusive (Konttijärvi intrusion, Finland)
Where rockhounds find majakite
Classic worldwide localities
- Majak mine, Talnakh area, Noril’sk region, western Siberia (type locality), Russia
- Found at the Chiney layered intrusion, western Aldan shield, Siberia, Russia
- Nizhni Tagil, Ural Mountains, Russia
- Vostok deposit, Lukkulaisvaara layered intrusion, Karelia, Russia
- Konttijärvi intrusion, northern Finland
- Lubin and Polkovice copper mines, near Legnica, Zechstein copper district, Lower Silesia, Poland
Field-hunting tip
Where it forms: As intergrowths with other platinum-group minerals in chalcopyrite and talnakhite ores (Majak mine, Russia); in sulfide mineralization in a strongly metamorphosed layered intrusive (Konttijärvi intrusion, Finland). If you start seeing chalcopyrite, talnakhite, polarite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.







