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, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Goslarite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Goslarite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, blue, green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular or fibrous crusts, efflorescences, 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
- Density
- 1.95-1.97 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular or Fibrous Crusts, Efflorescences, Stalactitic
- Cleavage
- Perfect On {010}
- Rarity
- Common
- Uses
- Collector
- Host rock
- Oxidized Zones of Zinc-rich Hydrothermal Ore Deposits
- Typical price
- $10-60 per specimen
Where rockhounds find goslarite
Classic worldwide localities
- Goslar, Germany
- Chile
- Spain
- United States
- Mexico
Field-hunting tip
Look in oxidized zones of zinc-rich hydrothermal ore deposits country, the host setting where goslarite typically forms. If you start seeing sphalerite, pyrite, melanterite in float, you are in the right ground. Field specimens usually show a acicular or fibrous crusts, efflorescences, stalactitic habit, so train your eye for that shape before scanning the outcrop.






