Cerromojonite is a rare copper lead bismuth selenide that forms black type I: as grains. It was approved as a distinct mineral species in 2018. It was first described from the El Dragón mine, Province of Antonio Quijarro, Department of Potosí, Bolivia.
Is this cerromojonite?
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 cerromojonite with a known reference. Cerromojonite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cerromojonite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cerromojonite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: type I: as grains.
Often confused with
Cerromojonite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Cerromojonite leaves black, Galena leaves lead-gray.

How to tell apart: Streak differs, so Cerromojonite leaves black, Bournonite leaves steel-gray; luster reads metallic on Cerromojonite and dull on Bournonite.
Often found alongside cerromojonite
Minerals reported to co-occur with cerromojonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuPbBiSe₃
- Mohs hardness
- 2
- Density
- 7.035 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Type I: as Grains
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Tin-silver Veins
Where rockhounds find cerromojonite
Classic worldwide localities
- Cerro Mojón, Potosí, Bolivia
Field-hunting tip
Look in hydrothermal tin-silver veins country, the host setting where cerromojonite typically forms. If you start seeing galena, sphalerite, pyrite in float, you are in the right ground. Field specimens usually show a type i: as grains habit, so train your eye for that shape before scanning the outcrop.



