Oxyplumbopyrochlore is a rare lead-rich member of the pyrochlore supergroup typically found as small, octahedral crystals. It is primarily recognized by mineralogists for its high density and association with complex manganese-rich metamorphic environments.
Is this oxyplumbopyrochlore?
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 oxyplumbopyrochlore with a known reference. Oxyplumbopyrochlore sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellowish-white.
- 3Read the lusterHold the specimen under a strong light. Luster: resinous.
- 4Match the color rangeCompare against the expected color range: yellow, brown, reddish-brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Oxyplumbopyrochlore vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oxyplumbopyrochlore
Minerals reported to co-occur with oxyplumbopyrochlore. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Nb₂O₆O
- Mohs hardness
- 5-5.5
- Density
- 6.0-6.5 g/cm³
- Colors
- Streak
- Yellowish-white
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- metamorphic manganese deposits
Where rockhounds find oxyplumbopyrochlore
Classic worldwide localities
- Kola Peninsula, Russia
- Långban, Sweden
Field-hunting tip
Where it forms: metamorphic manganese deposits. If you start seeing hausmannite, baryte, calcite in float, you are in the right ground. Typical habit: octahedral crystals. Train your eye for that shape before scanning the outcrop.





