Numanoite is an extremely rare copper-bearing borosilicate mineral first discovered in Japan. It typically occurs as small tabular crystals within skarn deposits and is highly prized by advanced mineral collectors for its unique chemistry.
Is this numanoite?
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 numanoite with a known reference. Numanoite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white to pale blue-green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, blue green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: inclusions.
Often confused with
Numanoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside numanoite
Minerals reported to co-occur with numanoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄CuB₄O₆(OH)₆(CO₃)₂
- Mohs hardness
- 4.5
- Density
- 2.96 g/cm³
- Colors
- Streak
- White to pale blue-green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Inclusions
- Cleavage
- Perfect, in two directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On the wall of cavities in a vein of nifontovite or in fractures in a crystalline limestone near gehlenite-spurrite skarns
Where rockhounds find numanoite
Classic worldwide localities
- Fuka Mine, Okayama Prefecture, Japan
Field-hunting tip
Where it forms: On the wall of cavities in a vein of nifontovite or in fractures in a crystalline limestone near gehlenite-spurrite skarns. If you start seeing borcarite, nifontovite, bultfonteinite in float, you are in the right ground. Typical habit: inclusions. Train your eye for that shape before scanning the outcrop.






