Shimazakiite is a rare calcium borate mineral that typically forms in contact metamorphic skarns. It is primarily known from its type locality at the Fuka mine in Japan, where it occurs as small, clear to yellowish crystals associated with other calcium-rich silicates.
Is this shimazakiite?
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 shimazakiite with a known reference. Shimazakiite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Shimazakiite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Shimazakiite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, aggregates.
Often confused with
Shimazakiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside shimazakiite
Minerals reported to co-occur with shimazakiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂B₂O₅
- Mohs hardness
- 3.5
- Density
- 3.16 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn Deposits
- Typical price
- n/a
Where rockhounds find shimazakiite
Classic worldwide localities
- Fuka mine, Okayama Prefecture, Japan
Field-hunting tip
Look in skarn deposits country — that is the host setting where shimazakiite typically forms. If you start seeing fukalite, tilleyite, spurrite in float, you are in the right ground. Field specimens usually show a tabular crystals, aggregates habit, so train your eye for that shape before scanning the outcrop.





