Souzalite is a rare phosphate mineral often found as fibrous, blue-green aggregates within granite pegmatites. It is best identified by its association with other rare phosphate minerals and its distinct acicular habit, which makes it a sought-after species for mineral collectors specializing in pegmatite suites.
Is this souzalite?
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 souzalite with a known reference. Souzalite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue green, dark green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: crystalline, massive.
Often confused with
Souzalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside souzalite
Minerals reported to co-occur with souzalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₃Al₄(PO₄)₄(OH)₆·2H₂O
- Mohs hardness
- 5.5-6
- Density
- 3.087 g/cm³
- Colors
- Streak
- Pale green
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Crystalline, massive
- Cleavage
- On {001}, good; a second ⊥ {001}, poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare hydrothermal alteration product of scorzalite in complex zoned granite pegmatites, in sedimentary phosphate nodules, and in a high-pressure kyanite deposit
Where rockhounds find souzalite
Classic worldwide localities
- Bell Pit, Newry, Oxford Co., Maine, USA
- Corrego Frio pegmatite mine, Divino das Laranjeiras, near Linópolis, Minas Gerais, Brazil
- Rapid Creek, Yukon Territory, Canada
Field-hunting tip
Where it forms: A rare hydrothermal alteration product of scorzalite in complex zoned granite pegmatites, in sedimentary phosphate nodules, and in a high-pressure kyanite deposit. If you start seeing scorzalite in float, you are in the right ground. Typical habit: crystalline, massive. Train your eye for that shape before scanning the outcrop.



