Nyholmite is a rare zinc-copper arsenate mineral discovered in the Broken Hill mining district. It typically appears as small, white to colorless bladed crystals or clusters formed within the oxidized zones of ore deposits.
Is this nyholmite?
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 nyholmite with a known reference. Nyholmite sits at Mohs 3-3.5, 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 crystals, white in aggregates.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed crystals, aggregates.
Often confused with
Nyholmite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nyholmite
Minerals reported to co-occur with nyholmite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cd₃Zn₂(AsO₃OH)₂(AsO₄)₂·4H₂O
- Mohs hardness
- 3-3.5
- Density
- 4.42 g/cm³
- Colors
- Colorless crystalsWhite in aggregates
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed crystals, aggregates
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late-stage secondary mineral in the weathering zone of a Cd-Zn arsenate deposit
Where rockhounds find nyholmite
Classic worldwide localities
- Block 14 Opencut, Broken Hill, New South Wales, Australia
Field-hunting tip
Where it forms: A late-stage secondary mineral in the weathering zone of a Cd-Zn arsenate deposit. If you start seeing goldquarryite, lavendulan-sampleite, scorodite-strengite in float, you are in the right ground. Typical habit: bladed crystals, aggregates. Train your eye for that shape before scanning the outcrop.




