Schlemaite is an extremely rare copper-lead selenide mineral named after its type locality in the Schlema-Hartenstein district. It is typically found as small, lead-gray metallic grains associated with other selenium-bearing minerals in hydrothermal uranium veins. Collectors generally prize it as a rare species of interest for advanced mineralogical suites.
Is this schlemaite?
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 schlemaite with a known reference. Schlemaite 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. Schlemaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Schlemaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains.
Often confused with
Schlemaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside schlemaite
Minerals reported to co-occur with schlemaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,□)₆(Pb,Bi)Se₄
- Mohs hardness
- 2.5
- Density
- 8.8 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Uranium-bearing Deposits
- Typical price
- $50-300+ for micro-specimens
Where rockhounds find schlemaite
Classic worldwide localities
- Schlema-Hartenstein district, Saxony, Germany
- Příbram, Czech Republic
Field-hunting tip
Look in hydrothermal veins in uranium-bearing deposits country — that is the host setting where schlemaite typically forms. If you start seeing clausthalite, berzelianite, uraninite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.




