Oxyplumboroméite is a rare mineral of the roméite group, typically occurring as small, well-formed octahedrons within manganese-rich metamorphic environments. It is characterized by its high specific gravity and distinct cubic morphology, usually found in historically significant manganese mines.
Is this oxyplumboroméite?
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 oxyplumboroméite with a known reference. Oxyplumboroméite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: straw-yellow.
- 3Match the color rangeCompare against the expected color range: yellow, brownish yellow.
- 4Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Oxyplumboroméite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oxyplumboroméite
Minerals reported to co-occur with oxyplumboroméite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Sb₂O₆O
- Mohs hardness
- ~5
- Density
- 6.732 g/cm³
- Colors
- Streak
- Straw-yellow
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In fissure veins cutting tephroite skarn
Where rockhounds find oxyplumboroméite
Classic worldwide localities
- Harstigen mine, Pajsberg, Värmland, Sweden
Field-hunting tip
Where it forms: In fissure veins cutting tephroite skarn. If you start seeing calcite, leucophoenicite in float, you are in the right ground. Typical habit: octahedral crystals. Train your eye for that shape before scanning the outcrop.



