Warikahnite is a rare secondary zinc arsenate mineral typically found as delicate, pale yellow bladed crystals. It is most famous from the Tsumeb Mine in Namibia where it forms in oxidized zones of ore deposits. Collectors should handle specimens with care due to their fragile nature and arsenic content.
Is this warikahnite?
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 warikahnite with a known reference. Warikahnite sits at Mohs ~2, 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: colorless, honey yellow, light yellow, orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: acicular, radial.
Often confused with
Warikahnite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside warikahnite
Minerals reported to co-occur with warikahnite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₃(AsO₄)₂·2H₂O
- Mohs hardness
- ~2
- Density
- 4.24 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Acicular, radial
- Cleavage
- On {001}, perfect; on {100}, {010}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral formed by alteration of tennantite in an oxidized zone in a dolostone-hosted hydrothermal polymetallic ore deposit
Where rockhounds find warikahnite
Classic worldwide localities
- Tsumeb, Namibia
Field-hunting tip
Where it forms: A rare secondary mineral formed by alteration of tennantite in an oxidized zone in a dolostone-hosted hydrothermal polymetallic ore deposit. If you start seeing tennantite, claudetite, ludlockite in float, you are in the right ground. Typical habit: acicular, radial. Train your eye for that shape before scanning the outcrop.







