Vismirnovite is an extremely rare zinc-tin hydroxide mineral typically found as small, vibrant yellow octahedral crystals in oxidized ore zones. It is most commonly identified in association with other tin-bearing minerals in hydrothermal environments.
Is this vismirnovite?
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 vismirnovite with a known reference. Vismirnovite sits at Mohs 5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Vismirnovite leaves a yellowish-white streak.
- 3Read the lusterHold the specimen under a strong light. Vismirnovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Vismirnovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside vismirnovite
Minerals reported to co-occur with vismirnovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnSn(OH)₆
- Mohs hardness
- 5.5
- Density
- 4.95 g/cm³
- Colors
- Streak
- Yellowish-white
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Octahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Tin Deposits
- Typical price
- $100-500 per specimen
Where rockhounds find vismirnovite
Classic worldwide localities
- Kazakhstan
Field-hunting tip
Look in oxidized hydrothermal tin deposits country — that is the host setting where vismirnovite typically forms. If you start seeing cassiterite, sphalerite, galena in float, you are in the right ground. Field specimens usually show a octahedral crystals habit, so train your eye for that shape before scanning the outcrop.




