Kyrgyzstanite is a rare sulfate mineral typically found as delicate, pearly-yellow platy crystals or crusts. It is most famously associated with the mercury mines in the Khaydarkan district of Kyrgyzstan, where it forms in oxidized zones.
Is this kyrgyzstanite?
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 kyrgyzstanite with a known reference. Kyrgyzstanite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts.
Often confused with
Kyrgyzstanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kyrgyzstanite
Minerals reported to co-occur with kyrgyzstanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnAl₄SO₄(OH)₁₂·3H₂O
- Mohs hardness
- 2
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Zn-dominant analogue of chalcoalumite
Where rockhounds find kyrgyzstanite
Classic worldwide localities
- Kara-Tangi, Fergana Valley, Osh, Kyrgyzstan (type locality)
Field-hunting tip
Where it forms: Zn-dominant analogue of chalcoalumite. If you start seeing cinnabar, quartz, calcite in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.





