Boyleite is a rare secondary zinc sulfate mineral typically found as white crusts or efflorescences in the oxidized zones of zinc-rich sulfide deposits. It is structurally related to the Gunningite group and is highly water-soluble, making it a challenge for collectors to preserve in humid environments. It is most commonly identified by its occurrence as a late-stage weathering product in mines.
Is this boyleite?
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 boyleite with a known reference. Boyleite sits at Mohs ~2, 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 to dull.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crusts, efflorescences, granular.
Often confused with
Boyleite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside boyleite
Minerals reported to co-occur with boyleite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnSO₄·4H₂O
- Mohs hardness
- ~2
- Density
- 2.41 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to dull
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Crusts, efflorescences, granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare alteration product of sphalerite in a hydrothermal Pb–Zn vein (Kropbach quarry, Germany)
Where rockhounds find boyleite
Classic worldwide localities
- Kropbach quarry, Münstertal, Black Forest, Germany
- Les Vallettes, Valais, Switzerland
- Keno Hill, Yukon Territory, Canada
Field-hunting tip
Where it forms: A rare alteration product of sphalerite in a hydrothermal Pb–Zn vein (Kropbach quarry, Germany). If you start seeing gypsum, gunningite, sphalerite in float, you are in the right ground. Typical habit: crusts, efflorescences, granular. Train your eye for that shape before scanning the outcrop.








