Bellidoite is a rare copper selenide mineral typically found as microscopic grains or anhedral masses within hydrothermal selenide deposits. It is best identified by its high density and metallic luster, usually requiring X-ray diffraction or electron microprobe analysis for positive field identification due to its similarity to other selenide minerals.
Is this bellidoite?
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 bellidoite with a known reference. Bellidoite 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. Bellidoite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Bellidoite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: microscopic grains, anhedral masses.
Often confused with
Bellidoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bellidoite
Minerals reported to co-occur with bellidoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂Se
- Mohs hardness
- 2.5
- Density
- 8.85 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Microscopic Grains, Anhedral Masses
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find bellidoite
Classic worldwide localities
- Bellido mine, Argentina
- Siekierki, Poland
- Predborice, Czech Republic
Field-hunting tip
Look in hydrothermal veins country, the host setting where bellidoite typically forms. If you start seeing berzelianite, umangite, clausthalite in float, you are in the right ground. Field specimens usually show a microscopic grains, anhedral masses habit, so train your eye for that shape before scanning the outcrop.




