Goslarite is a hydrated zinc sulfate that typically forms as a secondary efflorescence in mines where zinc-rich sulfide ores have oxidized. It is highly unstable in dry air and will rapidly dehydrate into a white powder, so collectors must keep specimens in airtight, humidity-controlled containers to maintain their crystal structure.
Is this goslarite?
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 goslarite with a known reference. Goslarite sits at Mohs 2-2.5, 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, silky if fibrous.
- 4Match the color rangeCompare against the expected color range: colorless, blue, brown, green, green blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular, massive, stalactitic.
Often confused with
Goslarite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside goslarite
Minerals reported to co-occur with goslarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnSO₄·7H₂O
- Mohs hardness
- 2-2.5
- Density
- 1.98 g/cm³
- Streak
- White
- Luster
- Vitreous, silky if fibrous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular, massive, stalactitic
- Cleavage
- On {010}, perfect
- Rarity
- Common
- Uses
- Collector
- Host rock
- A secondary mineral in oxidized portions of zinc sulfide deposits, particularly as coatings on walls of mine passages
Where rockhounds find goslarite
Classic worldwide localities
- Bisbee, Cochise Co., Arizona, USA
- Central district, Grant Co., New Mexico, USA
- Island Mountain, Trinity Co., California, USA
- Butte, Silver Bow Co., Montana, USA
- Rammelsberg mine, near Goslar, Harz Mountains, and at Freiberg and Altenberg, Saxony, Germany
- Baňská Stiavnica (Schemnitz), Slovakia
Field-hunting tip
Where it forms: A secondary mineral in oxidized portions of zinc sulfide deposits, particularly as coatings on walls of mine passages. If you start seeing epsomite, melanterite, pickeringite in float, you are in the right ground. Typical habit: acicular, massive, stalactitic. Train your eye for that shape before scanning the outcrop.






