Wülfingite is a rare zinc hydroxide mineral that typically forms as delicate, needle-like crystals or crusts in oxidized zinc deposits. It is best identified by its association with secondary zinc minerals like smithsonite and its distinct orthorhombic crystal form, often requiring microscopic examination for positive identification.
Is this wülfingite?
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 wülfingite with a known reference. Wülfingite 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: waxy.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: pseudo octohedral.
Often confused with
Wülfingite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wülfingite
Minerals reported to co-occur with wülfingite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn(OH)₂
- Mohs hardness
- 3
- Density
- 3.05 g/cm³
- Streak
- White
- Luster
- Waxy
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Pseudo octohedral
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral formed by weathering of zinc-bearing slag (Richelsdorf, Germany)
Where rockhounds find wülfingite
Classic worldwide localities
- Milltown, near Ashover, Derbyshite, England (type locality)
Field-hunting tip
Where it forms: A rare secondary mineral formed by weathering of zinc-bearing slag (Richelsdorf, Germany). If you start seeing simonkolleite, hydrocerussite, diaboleite in float, you are in the right ground. Typical habit: pseudo octohedral. Train your eye for that shape before scanning the outcrop.








