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. Tarbuttite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tarbuttite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish, greenish.
- 5Look at form & habitCrystal system: triclinic. Typical habit: prismatic crystals, globular aggregates, radiating groups.
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
- 4.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Prismatic Crystals, Globular Aggregates, Radiating Groups
- Cleavage
- Perfect On {101}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Zinc-lead Deposits
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find tarbuttite
Classic worldwide localities
- Broken Hill, Zambia
- Namibia
- Democratic Republic of the Congo
Field-hunting tip
Look in oxidized zones of zinc-lead deposits country — that is the host setting where tarbuttite typically forms. If you start seeing hopeite, descloizite, smithsonite in float, you are in the right ground. Field specimens usually show a prismatic crystals, globular aggregates, radiating groups habit, so train your eye for that shape before scanning the outcrop.





