Kinoshitalite is a rare barium-rich mica that typically forms as small, platy, micaceous crystals in manganese-rich metamorphic environments. It is highly valued by mineral collectors for its unique chemistry and association with rare manganese minerals. Collectors should look for its characteristic yellowish to brownish color and perfect micaceous cleavage in skarn assemblages.
Is this kinoshitalite?
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 kinoshitalite with a known reference. Kinoshitalite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kinoshitalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kinoshitalite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, orange, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy, micaceous, tabular.
Often confused with
Kinoshitalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kinoshitalite
Minerals reported to co-occur with kinoshitalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ba,K)(Mg,Mn,Al)₃(Al,Si,Fe)₄O₁₀(OH,F)₂
- Mohs hardness
- 2.5-3
- Density
- 3.31 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy, Micaceous, Tabular
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Manganese-rich Skarns
- Typical price
- $20-150 for small specimens
Where rockhounds find kinoshitalite
Classic worldwide localities
- Kyoto Prefecture, Japan
- Långban, Sweden
- Franklin, New Jersey, USA
- Big Creek, California, USA
Field-hunting tip
Look in metamorphic manganese-rich skarns country — that is the host setting where kinoshitalite typically forms. If you start seeing hausmannite, barite, celsian in float, you are in the right ground. Field specimens usually show a platy, micaceous, tabular habit, so train your eye for that shape before scanning the outcrop.






