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 — that is 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.






