Arsenohopeite is a rare hydrated zinc arsenate found in the oxidized zones of base metal deposits. It typically forms as small, colorless to white tabular crystals that are visually indistinguishable from its phosphate analog, Hopeite, without chemical analysis.
Is this arsenohopeite?
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 arsenohopeite with a known reference. Arsenohopeite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Arsenohopeite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Arsenohopeite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Arsenohopeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arsenohopeite
Minerals reported to co-occur with arsenohopeite. 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
- 3.5
- Density
- 3.31 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zinc Deposits
- Typical price
- $50-500 thumbnail
Where rockhounds find arsenohopeite
Classic worldwide localities
- Broken Hill, Zambia
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized zinc deposits country — that is the host setting where arsenohopeite typically forms. If you start seeing hopeite, smithsonite, hemimorphite 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.




