Davidlloydite is an extremely rare zinc arsenate mineral that occurs as small, delicate tabular crystals. It is primarily found in the Tsumeb Mine in Namibia, typically associated with other secondary arsenic and zinc minerals in the oxidation zone of ore deposits.
Is this davidlloydite?
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 davidlloydite with a known reference. Davidlloydite sits at Mohs 3-4, 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 to opalescent.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Davidlloydite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside davidlloydite
Minerals reported to co-occur with davidlloydite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₃(AsO₄)₂·4H₂O
- Mohs hardness
- 3-4
- Density
- 3.661 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to opalescent
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals
- Cleavage
- Distinct on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Secondary in the oxidation zone of a Cu-Pb-Zn mineral deposit
Where rockhounds find davidlloydite
Classic worldwide localities
- Tsumeb mine, Otjikoto (Oshikoto) region, Namibia
Field-hunting tip
Where it forms: Secondary in the oxidation zone of a Cu-Pb-Zn mineral deposit. If you start seeing calcioandyrobertsite, stranskiite, geminite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





