Abuite is a very rare phosphate mineral first described from the pegmatites of Mount Abu in India. It typically forms colorless to white tabular crystals that are difficult to distinguish from associated phosphate minerals without analytical testing. Collectors generally find it as a micromount specimen due to its extreme scarcity.
Is this abuite?
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 abuite with a known reference. Abuite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Abuite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside abuite
Minerals reported to co-occur with abuite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₂(PO₄)₂F₂
- Mohs hardness
- 3.5
- Density
- 3.214 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals, subparallel aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermally altered, felsic pyroclastic rocks, related to a biotite adamellite intrusion
Where rockhounds find abuite
Classic worldwide localities
- Hinomaru-Nago mine, Kiyo area, Abu, Abu County, Yamaguchi Prefecture, Japan
Field-hunting tip
Where it forms: In hydrothermally altered, felsic pyroclastic rocks, related to a biotite adamellite intrusion. If you start seeing quartz, augelite, apatite in float, you are in the right ground. Typical habit: tabular crystals, subparallel aggregates. Train your eye for that shape before scanning the outcrop.






