Kuzmenkoite-Zn is a rare member of the labuntsovite group typically found in highly evolved alkaline pegmatite environments. It forms small, attractive prismatic crystals, often exhibiting a honey-yellow or brownish-orange color and a vitreous luster.
Is this kuzmenkoite-zn?
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 kuzmenkoite-zn with a known reference. Kuzmenkoite-Zn sits at Mohs 5, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white, grayish white, pale pink, light brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic, pseudomorphous.
Often confused with
Kuzmenkoite-Zn vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kuzmenkoite-zn
Minerals reported to co-occur with kuzmenkoite-zn. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂ZnTi₄(Si₄O₁₂)₂(OH,O)₄·nH₂O
- Mohs hardness
- 5
- Density
- 2.78-2.87 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic, pseudomorphous
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal product in 3 pegmatites
Where rockhounds find kuzmenkoite-zn
Classic worldwide localities
- Mount Kedydverpakhk and Mount Krrnasurt, Lovozero massif, Kola Peninsula, Russia (type locality)
Field-hunting tip
Where it forms: Hydrothermal product in 3 pegmatites. If you start seeing aegirine, microcline, nepheline in float, you are in the right ground. Typical habit: prismatic, pseudomorphous. Train your eye for that shape before scanning the outcrop.






