Clinometaborite is a rare calcium borate mineral known primarily from skarn environments in Japan. It typically occurs as small, clear, tabular monoclinic crystals associated with other calcium-rich minerals in limestone contact zones.
Is this clinometaborite?
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 clinometaborite with a known reference. Clinometaborite 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. Clinometaborite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Clinometaborite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Clinometaborite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside clinometaborite
Minerals reported to co-occur with clinometaborite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaB₃O₄(OH)₃
- Mohs hardness
- 3.5
- Density
- 2.42 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn Deposits
- Typical price
- varies significantly by specimen availability
Where rockhounds find clinometaborite
Classic worldwide localities
- Fuka mine, Okayama Prefecture, Japan
Field-hunting tip
Look in skarn deposits country — that is the host setting where clinometaborite typically forms. If you start seeing calcite, bultfonteinite, tobermorite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.






