Nagashimalite is an extremely rare barium vanadium silicate mineral typically found in metamorphosed manganese deposits in Japan. It usually occurs as small, dark brown to black tabular crystals or granular aggregates, often requiring microscopic examination for positive identification.
Is this nagashimalite?
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 nagashimalite with a known reference. Nagashimalite sits at Mohs ~6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: green.
- 3Read the lusterHold the specimen under a strong light. Luster: submetallic to vitreous.
- 4Match the color rangeCompare against the expected color range: greenish black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: aggregates.
Often confused with
Nagashimalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nagashimalite
Minerals reported to co-occur with nagashimalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba₄(V³⁺,Ti)₄Si₈B₂O₂₇(O,OH)₂Cl
- Mohs hardness
- ~6
- Density
- 4.08 g/cm³
- Colors
- Streak
- Green
- Luster
- Submetallic to vitreous
- Transparency
- Opaque to transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In fissures cutting massive rhodonite ore in a bedded manganese deposit
Where rockhounds find nagashimalite
Classic worldwide localities
- Mogurazawa mine, Kiryu, Gumma Prefecture, Japan
Field-hunting tip
Where it forms: In fissures cutting massive rhodonite ore in a bedded manganese deposit. If you start seeing rhodochrosite, rhodonite, barite in float, you are in the right ground. Typical habit: aggregates. Train your eye for that shape before scanning the outcrop.







