Taneyamalite is a rare manganese-bearing silicate mineral belonging to the ardennite group. It typically occurs as small, delicate, radiating fibrous aggregates within manganese-rich metamorphic environments and is highly sought after by systematic mineral collectors.
Is this taneyamalite?
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 taneyamalite with a known reference. Taneyamalite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light yellow, brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: greenish yellow, grayish yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: acicular, flakes.
Often found alongside taneyamalite
Minerals reported to co-occur with taneyamalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)Mn₁₂(Si,Al)₁₂(O,OH)₄₄
- Mohs hardness
- 5-6
- Density
- 3.30 g/cm³
- Streak
- Light yellow, brown
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Acicular, flakes
- Cleavage
- Perfect to good on (010), fair on (100)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In cracks in ferruginous chert, mafic rocks, and limestone subjected to blueschist facies metamorphism (Taneyama mine, Japan)
Where rockhounds find taneyamalite
Classic worldwide localities
- Ward Creek, near Cazadero, and along the Russian River, Sonoma Co., and Pacheco Pass, Santa Clara Co., California, USA
- Taneyama mine, Kumamoto Prefecture, and the Iwaizawa mine, near Agano, Saitama Prefecture, Japan
- Brezovia, Yugoslavia
Field-hunting tip
Where it forms: In cracks in ferruginous chert, mafic rocks, and limestone subjected to blueschist facies metamorphism (Taneyama mine, Japan). If you start seeing quartz, hematite, chamosite in float, you are in the right ground. Typical habit: acicular, flakes. Train your eye for that shape before scanning the outcrop.






