Hydroxymanganopyrochlore is a rare member of the pyrochlore group, typically found as small, dark octahedral crystals within alkaline pegmatite complexes. Due to its radioactive nature and scarcity, it is sought primarily by advanced mineral collectors focusing on complex niobate species.
Is this hydroxymanganopyrochlore?
3-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 hydroxymanganopyrochlore with a known reference. Hydroxymanganopyrochlore sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: dark brown, black, with red reflexes.
- 3Look at form & habitCrystal system: cubic. Typical habit: octahedral.
Often confused with
Hydroxymanganopyrochlore vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hydroxymanganopyrochlore
Minerals reported to co-occur with hydroxymanganopyrochlore. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mn,Th,Na,Ca,REE)₂(Nb,Ti)₂O₆(OH)
- Mohs hardness
- 5-5.5
- Density
- 5.398 g/cm³
- Colors
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In small miarolitic cavities in sanidinite as a late pneumatolytic phase
Where rockhounds find hydroxymanganopyrochlore
Classic worldwide localities
- Pumice quarry near Mendig, Laacher See area, Eifel, Rheinland-Pfalz, Germany
Field-hunting tip
Where it forms: In small miarolitic cavities in sanidinite as a late pneumatolytic phase. If you start seeing sanidine, nosean, biotite in float, you are in the right ground. Typical habit: octahedral. Train your eye for that shape before scanning the outcrop.






