Imayoshiite is an extremely rare calcium aluminum borosilicate mineral known primarily from the Fuka Mine in Japan. It typically occurs as small, colorless, prismatic crystals within skarn environments associated with high-temperature contact metamorphism of limestone.
Is this imayoshiite?
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 imayoshiite with a known reference. Imayoshiite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Imayoshiite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Imayoshiite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Imayoshiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside imayoshiite
Minerals reported to co-occur with imayoshiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Al₂B₆Si₆O₂₄(OH)₈
- Mohs hardness
- 3-4
- Density
- 2.19 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn
- Typical price
- n/a
Where rockhounds find imayoshiite
Classic worldwide localities
- Fuka Mine, Okayama Prefecture, Japan
Field-hunting tip
Look in skarn country — that is the host setting where imayoshiite typically forms. If you start seeing fukalite, spurrite, ettringite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.



