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 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Boyleite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Boyleite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 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
- (Zn,Mg)SO₄·4H₂O
- Mohs hardness
- 2.5
- Density
- 3.17 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Crusts, Efflorescences, Granular
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Ore Deposits
- Typical price
- $20-100 for small specimens
Where rockhounds find boyleite
Classic worldwide localities
- Tsumeb, Namibia
- Sterling Hill, New Jersey, USA
- Galena, Kansas, USA
Field-hunting tip
Look in oxidized hydrothermal ore deposits country — that is the host setting where boyleite typically forms. If you start seeing smithsonite, sphalerite, anglesite in float, you are in the right ground. Field specimens usually show a crusts, efflorescences, granular habit, so train your eye for that shape before scanning the outcrop.






