Brumadoite is a rare copper selenite mineral found primarily in the magnesite mines of Bahia, Brazil. It typically appears as small, bright yellow to greenish-yellow tabular crystals or radiating sprays within vugs and fractures. Collectors prize it for its unique chemistry and association with rare selenium-bearing species.
Is this brumadoite?
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 brumadoite with a known reference. Brumadoite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Brumadoite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Brumadoite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, radiating aggregates.
Often confused with
Brumadoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside brumadoite
Minerals reported to co-occur with brumadoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃(SeO₃)₂(OH)₄
- Mohs hardness
- 3
- Density
- 4.8 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Radiating Aggregates
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Magnesite Deposits
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find brumadoite
Classic worldwide localities
- Brumado, Bahia, Brazil
Field-hunting tip
Look in hydrothermal veins in magnesite deposits country, the host setting where brumadoite typically forms. If you start seeing chalcomenite, magnesite, dolomite in float, you are in the right ground. Field specimens usually show a tabular crystals, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.




