Zircosulfate is an extremely rare zirconium sulfate mineral that typically forms as a secondary encrustation or in fumarolic environments. It appears as small, fragile, colorless to white tabular crystals that are highly soluble in water, making it a challenging mineral to collect and store.
Is this zircosulfate?
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 zircosulfate with a known reference. Zircosulfate sits at Mohs 2.5-3, 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: dull.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Zircosulfate vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zircosulfate
Minerals reported to co-occur with zircosulfate. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zr(SO₄)₂·4H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.85 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a cavity in intensely hydrothermally altered nepheline syenite pegmatite, perhaps formed by acid sulfatic solutions attacking eudialyte
Where rockhounds find zircosulfate
Classic worldwide localities
- Korgeredaba alkalic massif, Sangilen Upland, southeastern Tuva, Russia
Field-hunting tip
Where it forms: In a cavity in intensely hydrothermally altered nepheline syenite pegmatite, perhaps formed by acid sulfatic solutions attacking eudialyte. If you start seeing hisingerite, smithsonite, limonite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





