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, 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.






