Favreauite is an incredibly rare lead-bismuth-copper selenite mineral known almost exclusively from the Poudrette quarry at Mont Saint-Hilaire. It typically forms small, green, translucent tabular crystals or crusts in vugs within alkaline igneous rocks. Collectors prize this species for its intense color and status as a type-locality rarity.
Is this favreauite?
4-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 favreauite with a known reference. Favreauite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: green.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: tabular crystals, crusts, aggregates.
Often confused with
Favreauite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside favreauite
Minerals reported to co-occur with favreauite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbBiCu₆O₄(SeO₃)₄(OH)·H₂O
- Mohs hardness
- ~3
- Density
- 4.851 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Tabular crystals, crusts, aggregates
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral formed by the oxidation of a selenide-bearing hydrothermal vein hosted by sandstones and shales
Where rockhounds find favreauite
Classic worldwide localities
- El Dragón mine, Antonio Quijarro Province, Potosí Department, Bolivia
Field-hunting tip
Where it forms: A secondary mineral formed by the oxidation of a selenide-bearing hydrothermal vein hosted by sandstones and shales. If you start seeing ahlfeldite, allophane, calcite in float, you are in the right ground. Typical habit: tabular crystals, crusts, aggregates. Train your eye for that shape before scanning the outcrop.








