Tamaite is a rare manganese-bearing member of the pumpellyite group, typically occurring as fine fibrous or radiating acicular clusters. It is primarily identified by its characteristic brownish color and its occurrence in metamorphosed manganese deposits.
Is this tamaite?
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 tamaite with a known reference. Tamaite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: colorless, pale yellowish brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: micaceous, platy.
Often found alongside tamaite
Minerals reported to co-occur with tamaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,K,Na)xMn₆(Si,Al)₁₀O₂₄(OH)₄·nH₂O (x = 1-2; n = 7-11)
- Mohs hardness
- 4
- Density
- 2.85 g/cm³
- Colors
- ColorlessPale yellowish brown
- Streak
- White
- Luster
- Vitreous to pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Micaceous, platy
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In veinlets to 1.5 mm in width in a weakly metamorphosed Mn ore deposit
Where rockhounds find tamaite
Classic worldwide localities
- Shiromaru mine, near Okutama, Tama district, ~60 km from Tokyo, Japan
Field-hunting tip
Where it forms: In veinlets to 1.5 mm in width in a weakly metamorphosed Mn ore deposit. If you start seeing celsian, barian orthoclase, aegirine in float, you are in the right ground. Typical habit: micaceous, platy. Train your eye for that shape before scanning the outcrop.




