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 — that is 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.




