Babefphite is a very rare barium beryllium phosphate mineral found in highly evolved alkaline pegmatites. Collectors look for its small, colorless, or yellowish tabular crystals, which are typically identified through chemical analysis due to their rarity and small size.
Is this babefphite?
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 babefphite with a known reference. Babefphite sits at Mohs 3.5-4, 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 to greasy.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, granular masses.
Often confused with
Babefphite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside babefphite
Minerals reported to co-occur with babefphite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaBe(PO₄)F
- Mohs hardness
- 3.5-4
- Density
- 4.31 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to greasy
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, granular masses
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In eluvium directly above rare-metal skarn deposits associated with alkaline intrusions
Where rockhounds find babefphite
Classic worldwide localities
- Kola Peninsula, Russia
- Norra Kärr, Sweden
Field-hunting tip
Where it forms: In eluvium directly above rare-metal skarn deposits associated with alkaline intrusions. If you start seeing zircon, ilmenorutile, fluorite in float, you are in the right ground. Typical habit: tabular crystals, granular masses. Train your eye for that shape before scanning the outcrop.








