Suzukiite is a rare barium vanadium silicate mineral typically found as small, translucent tabular crystals. It is primarily identified by its distinct yellow color and occurrence in specialized metamorphic manganese-rich environments.
Is this suzukiite?
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 suzukiite with a known reference. Suzukiite sits at Mohs 4-4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: light green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: flakes.
Often confused with
Suzukiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside suzukiite
Minerals reported to co-occur with suzukiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaVSi₂O₇
- Mohs hardness
- 4-4.5
- Density
- 4.0 g/cm³
- Colors
- Streak
- Pale green
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Flakes
- Cleavage
- {010}, perfect; {100} and {001}, distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In massive rhodonite-rhodochrosite ores of a bedded manganese deposit, formed in very weakly metamorphosed Triassic cherts
Where rockhounds find suzukiite
Classic worldwide localities
- Mogurazawa mine, Gumma Prefecture, Japan
Field-hunting tip
Where it forms: In massive rhodonite-rhodochrosite ores of a bedded manganese deposit, formed in very weakly metamorphosed Triassic cherts. If you start seeing quartz, barite, alabandite in float, you are in the right ground. Typical habit: flakes. Train your eye for that shape before scanning the outcrop.







