Permingeatite is a rare copper antimony selenide typically found in hydrothermal selenide deposits. Collectors usually look for it as dark grey metallic inclusions associated with other copper minerals or uraninite, often identified via polished sections or XRD analysis due to its massive habit.
Is this permingeatite?
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 permingeatite with a known reference. Permingeatite sits at Mohs 4-4.5, 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: pink brown.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: microscopic crystals.
Often confused with
Permingeatite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside permingeatite
Minerals reported to co-occur with permingeatite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃SbSe₄
- Mohs hardness
- 4-4.5
- Density
- 5.82 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A product of epithermal hydrothermal mineralization
Where rockhounds find permingeatite
Classic worldwide localities
- Předbořice uranium deposit, near Krásna Hora, Czech Republic (type locality)
Field-hunting tip
Where it forms: A product of epithermal hydrothermal mineralization. If you start seeing berzelianite, hakite, eskebornite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.








