Zincroselite is a rare arsenate mineral that belongs to the roselite group, often appearing as small, delicate prismatic or acicular crystals. It is typically found in the oxidation zones of arsenic-rich base metal deposits, most notably associated with the Tsumeb mine. Collectors prize it for its unique chemistry and association with secondary zinc minerals.
Is this zincroselite?
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 zincroselite with a known reference. Zincroselite 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. Zincroselite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Zincroselite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to acicular crystals.
Often confused with
Zincroselite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zincroselite
Minerals reported to co-occur with zincroselite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Zn(AsO₄)₂·2H₂O
- Mohs hardness
- 3.5
- Density
- 3.66 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Acicular Crystals
- Cleavage
- Good On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Carbonate Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find zincroselite
Classic worldwide localities
- Tsumeb Mine, Namibia
- Bou Azzer, Morocco
Field-hunting tip
Look in hydrothermal veins in carbonate rocks country, the host setting where zincroselite typically forms. If you start seeing adamite, conichalcite, smithsonite in float, you are in the right ground. Field specimens usually show a prismatic to acicular crystals habit, so train your eye for that shape before scanning the outcrop.





