Bindheimite is a lead-antimony oxide typically found as a secondary mineral in the oxidation zones of lead deposits. It is most famous for occurring as yellow to orange earthy masses or as pseudomorphs, retaining the fibrous or acicular shapes of the original minerals it replaced.
Is this bindheimite?
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 bindheimite with a known reference. Bindheimite sits at Mohs 4-4.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bindheimite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Bindheimite typically shows a earthy luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brown, greenish, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, powdery, crusts, or as pseudomorphs after jamesonite and boulangerite.
Often confused with
Bindheimite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bindheimite
Minerals reported to co-occur with bindheimite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Sb₂O₆(O,OH)
- Mohs hardness
- 4-4.5
- Density
- 4.6-5.6 g/cm³
- Streak
- Yellow
- Luster
- Earthy
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Powdery, Crusts, Or as Pseudomorphs After Jamesonite and Boulangerite
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Oxidized Zones of Lead-antimony Bearing Hydrothermal Ore Deposits
- Typical price
- $10-100 depending on specimen size and clarity of pseudomorphs
Where rockhounds find bindheimite
Classic worldwide localities
- Germany
- Czech Republic
- USA
- Australia
- Mexico
Field-hunting tip
Look in oxidized zones of lead-antimony bearing hydrothermal ore deposits country — that is the host setting where bindheimite typically forms. If you start seeing jamesonite, boulangerite, galena in float, you are in the right ground. Field specimens usually show a massive, powdery, crusts, or as pseudomorphs after jamesonite and boulangerite habit, so train your eye for that shape before scanning the outcrop.






