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, 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, white.
- 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
- Density
- 3.75 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to acicular crystals
- Cleavage
- {010}, good to perfect; {001}, traces
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in an oxidized zone of a dolostone-hosted hydrothermal polymetallic ore deposit
Where rockhounds find zincroselite
Classic worldwide localities
- Tsumeb, Namibia
Field-hunting tip
Where it forms: A rare secondary mineral in an oxidized zone of a dolostone-hosted hydrothermal polymetallic ore deposit. If you start seeing tsumcorite, stranskiite, leiteite in float, you are in the right ground. Typical habit: prismatic to acicular crystals. Train your eye for that shape before scanning the outcrop.







