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, 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.






