Tarbuttite is a rare zinc phosphate mineral typically found in the oxidation zones of ore deposits. It is highly prized by collectors for its sharp, distinctively shaped prismatic crystals, which are most famously associated with the Broken Hill mine in Zambia.
Is this tarbuttite?
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 tarbuttite with a known reference. Tarbuttite 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, pearly on cleavages.
- 4Match the color rangeCompare against the expected color range: colorless, brown, green, white, light yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: prismatic, striated, wheat sheaf.
Often confused with
Tarbuttite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tarbuttite
Minerals reported to co-occur with tarbuttite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₂(PO₄)(OH)
- Mohs hardness
- 3.5-4
- Density
- 4.19 g/cm³
- Streak
- White
- Luster
- Vitreous, pearly on cleavages
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Prismatic, striated, wheat sheaf
- Cleavage
- On {001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An uncommon secondary mineral in the oxidized zone of zinc-bearing deposits
Where rockhounds find tarbuttite
Classic worldwide localities
- Kabwe (Broken Hill), Zambia
- Lueca vanadium mines, Angola
- Kef Semmah mine, near Sétif, Algeria
- Reaphook Hill, near Blinman, Flinders Ranges, South Australia
- Broken Hill, New South Wales, Australia
- Hudson Bay mine, Salmo, British Columbia, Canada
Field-hunting tip
Where it forms: An uncommon secondary mineral in the oxidized zone of zinc-bearing deposits. If you start seeing hopeite, hemimorphite, smithsonite in float, you are in the right ground. Typical habit: prismatic, striated, wheat sheaf. Train your eye for that shape before scanning the outcrop.






