Honzaite is a rare nickel arsenite that forms irregular to hemispherical aggregates. It is associated with arsenolite and zeunerite. It was first described from Jáchymov, Czech Republic.
Is this honzaite?
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 honzaite with a known reference. Honzaite 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: pale pink.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: pale pink, sometimes with purplish, violet tints.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: irregular to hemispherical aggregates.
Often confused with
Honzaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside honzaite
Minerals reported to co-occur with honzaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ni₂[AsO₃(OH)]₂(H₂O)₅
- Mohs hardness
- ~3
- Density
- 2.993 g/cm³
- Colors
- Streak
- Pale pink
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Irregular to hemispherical aggregates
- Cleavage
- Good on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral formed by weathering of nickelskutterudite and tennantite, under strongly acidic conditions, in a Ag+As+Co+Ni+Bi and U vein-type hydrothermal mineral deposit
Where rockhounds find honzaite
Classic worldwide localities
- Jáchymov, Czech Republic
Field-hunting tip
Where it forms: A secondary mineral formed by weathering of nickelskutterudite and tennantite, under strongly acidic conditions, in a Ag+As+Co+Ni+Bi and U vein-type hydrothermal mineral deposit. If you start seeing arsenolite, zeunerite, ni-rich burgessite in float, you are in the right ground. Typical habit: irregular to hemispherical aggregates. Train your eye for that shape before scanning the outcrop.




