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 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Davidlloydite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Davidlloydite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, 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
- Density
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Lead-zinc Ore Deposits
- Typical price
- $100-500 thumbnail
Where rockhounds find davidlloydite
Classic worldwide localities
- Tsumeb Mine, Namibia
Field-hunting tip
Look in oxidized hydrothermal lead-zinc ore deposits country — that is the host setting where davidlloydite typically forms. If you start seeing adamite, smithsonite, cornetite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.






