Bertossaite is a very rare phosphate mineral belonging to the amblygonite group, typically found in highly fractionated pegmatites. It usually forms small bladed or granular clusters and is prized by advanced collectors of rare phosphate species due to its extremely limited global occurrence.
Is this bertossaite?
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 bertossaite with a known reference. Bertossaite sits at Mohs 6, 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: light pink.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: bladed crystals, granular masses.
Often confused with
Bertossaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bertossaite
Minerals reported to co-occur with bertossaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Li₂CaAl₄(PO₄)₄(OH)₄
- Mohs hardness
- 6
- Density
- 3.10 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Bladed crystals, granular masses
- Cleavage
- On {100}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Thought to be formed during a late calcium-rich phase of mineralization in a lithium-bearing granite pegmatite
Where rockhounds find bertossaite
Classic worldwide localities
- Buranga pegmatite, near Gatumba, Rwanda
Field-hunting tip
Where it forms: Thought to be formed during a late calcium-rich phase of mineralization in a lithium-bearing granite pegmatite. If you start seeing amblygonite, lazulite-scorzalite, augelite in float, you are in the right ground. Typical habit: bladed crystals, granular masses. Train your eye for that shape before scanning the outcrop.







