Bairdite is a very rare lead manganese tellurite mineral discovered at the Otto Mountain locality. It typically occurs as minute, thin tabular yellow crystals within vugs of oxidized ore, often requiring magnification for proper identification.
Is this bairdite?
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 bairdite with a known reference. Bairdite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bairdite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bairdite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Bairdite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bairdite
Minerals reported to co-occur with bairdite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Mn₃TeO₈(OH)₂
- Mohs hardness
- 3.5
- Density
- 4.21 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Tellurium-bearing Ore Veins
- Typical price
- $500-2000 per specimen
Where rockhounds find bairdite
Classic worldwide localities
- Otto Mountain, San Bernardino County, California, USA
Field-hunting tip
Look in oxidized tellurium-bearing ore veins country — that is the host setting where bairdite typically forms. If you start seeing dugganite, quetzalcoatlite, teineite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





