Gatumbaite is a rare phosphate mineral typically found as delicate, radiating clusters of acicular crystals within phosphate-rich pegmatites. It was first identified in the Gatumba pegmatite field of Rwanda and remains a highly sought-after specimen for advanced phosphate mineral collectors.
Is this gatumbaite?
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 gatumbaite with a known reference. Gatumbaite sits at Mohs <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: pearly.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: rosette, scaly, wheat sheaf.
Often confused with
Gatumbaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gatumbaite
Minerals reported to co-occur with gatumbaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₂(PO₄)₂(OH)₂·H₂O
- Mohs hardness
- <5
- Density
- 2.92 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Rosette, scaly, wheat sheaf
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- From the phosphate assemblage in a complex granite pegmatite (Buranga pegmatite, Rwanda; Hålsjöberg, Sweden.); in andesites altered hydrothermally through hydrogen metasomatism (Mt. Perry, Australia)
Where rockhounds find gatumbaite
Classic worldwide localities
- Buranga pegmatite, near Gatumba, Rwanda
- Mt. Perry, 75 km southwest of Bundaberg, Queensland, Australia
- Hålsjöberg, Värmland, Sweden
Field-hunting tip
Where it forms: From the phosphate assemblage in a complex granite pegmatite (Buranga pegmatite, Rwanda; Hålsjöberg, Sweden.); in andesites altered hydrothermally through hydrogen metasomatism (Mt. Perry, Australia). If you start seeing trolleite, scorzalite, apatite in float, you are in the right ground. Typical habit: rosette, scaly, wheat sheaf. Train your eye for that shape before scanning the outcrop.








