Zincomenite is a very rare zinc selenite mineral typically found as a secondary oxidation product in selenium-rich environments. It usually appears as delicate, colorless to yellowish acicular or needle-like crystals or thin crusts associated with other rare selenide minerals.
Is this zincomenite?
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 zincomenite with a known reference. Zincomenite sits at Mohs 2-3, 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: adamantine.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular crystals, efflorescent crusts.
Often confused with
Zincomenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zincomenite
Minerals reported to co-occur with zincomenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnSeO₃
- Mohs hardness
- 2-3
- Density
- 4.760 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular crystals, efflorescent crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A sublimate around active fumaroles
Where rockhounds find zincomenite
Classic worldwide localities
- First scoria cone, Northern Breakthrough, Great Tolbachik Fissure Eruption, Tolbachik Volcano, Kamchatka, Russia
Field-hunting tip
Where it forms: A sublimate around active fumaroles. If you start seeing sellaite, fluorite, halite in float, you are in the right ground. Typical habit: acicular crystals, efflorescent crusts. Train your eye for that shape before scanning the outcrop.








