Kotulskite is a rare palladium telluride mineral typically found as microscopic inclusions within copper-nickel sulfide ores. It is primarily identified in polished sections through ore microscopy due to its small grain size and metallic, white-to-gray appearance. It is highly valued by mineral collectors specializing in rare platinum-group element minerals.
Is this kotulskite?
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 kotulskite with a known reference. Kotulskite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kotulskite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Kotulskite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, gray, pinkish-white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: anhedral grains, inclusions in other sulfides.
Often confused with
Kotulskite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kotulskite
Minerals reported to co-occur with kotulskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdTe
- Mohs hardness
- 2.5
- Density
- 9.5-9.8 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral Grains, Inclusions in Other Sulfides
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Mafic and Ultramafic Igneous Complexes
- Typical price
- $50-300 per micro-mount or specimen
Where rockhounds find kotulskite
Classic worldwide localities
- Monchegorsk, Kola Peninsula, Russia
- Stillwater Complex, Montana, USA
- Lac des Iles, Ontario, Canada
- Bushveld Complex, South Africa
Field-hunting tip
Look in mafic and ultramafic igneous complexes country — that is the host setting where kotulskite typically forms. If you start seeing chalcopyrite, pentlandite, pyrrhotite in float, you are in the right ground. Field specimens usually show a anhedral grains, inclusions in other sulfides habit, so train your eye for that shape before scanning the outcrop.






