Milotaite is an extremely rare palladium antimony telluride mineral discovered in the Czech Republic. It is typically found as microscopic grains embedded within sulfide-rich hydrothermal ores, making it a highly sought-after species for mineralogical research and advanced collections.
Is this milotaite?
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 milotaite with a known reference. Milotaite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Milotaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Milotaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral to subhedral grains.
Often confused with
Milotaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside milotaite
Minerals reported to co-occur with milotaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PdSbTe
- Mohs hardness
- 3-3.5
- Density
- 6.3-6.5 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Metamorphic Rocks
- Typical price
- $100-500 per specimen
Where rockhounds find milotaite
Classic worldwide localities
- Cerný Důl, Czech Republic
Field-hunting tip
Look in hydrothermal veins in metamorphic rocks country, the host setting where milotaite typically forms. If you start seeing chalcopyrite, galena, sphalerite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains habit, so train your eye for that shape before scanning the outcrop.






