Watatsumiite is a rare manganese-bearing silicate mineral belonging to the pectolite group. It is typically found in manganese ore deposits as radiating, fibrous, or acicular aggregates with a distinct reddish-yellowish green hue.
Is this watatsumiite?
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 watatsumiite with a known reference. Watatsumiite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white with a greenish tint.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, prismatic.
Often confused with
Watatsumiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside watatsumiite
Minerals reported to co-occur with watatsumiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- LiNa₂KMn₂V₂Si₈O₂₄
- Mohs hardness
- 5.5-6
- Density
- 3.24 g/cm³
- Colors
- Streak
- White with a greenish tint
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Massive, prismatic
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In veinlets in a metamorphosed Mn deposit
Where rockhounds find watatsumiite
Classic worldwide localities
- Tanohata mine, Iwate Prefecture, Japan (type locality)
Field-hunting tip
Where it forms: In veinlets in a metamorphosed Mn deposit. If you start seeing potassicleakeite, quartz, k-feldspar in float, you are in the right ground. Typical habit: massive, prismatic. Train your eye for that shape before scanning the outcrop.





