Kuzmenkoite-Mn is a rare member of the labuntsovite group found primarily in alkaline pegmatites. It typically occurs as small, yellow to brown prismatic crystals often forming radial sprays on matrix.
Is this kuzmenkoite-mn?
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-mn with a known reference. Kuzmenkoite-Mn 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: yellow, dark orange, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic.
Often confused with
Kuzmenkoite-Mn vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kuzmenkoite-mn
Minerals reported to co-occur with kuzmenkoite-mn. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂MnTi₄(Si₄O₁₂)₂(OH)₄·5-6H₂O
- Mohs hardness
- 5
- Density
- 2.67 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic
- Cleavage
- Imperfect cleavages in several unspecified directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late hydrothermal phase in minute cavities in albitized murmanite-bearing lujavrites
Where rockhounds find kuzmenkoite-mn
Classic worldwide localities
- Mt. Flora (north ridge of Mt. Selsurt), northern Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: A late hydrothermal phase in minute cavities in albitized murmanite-bearing lujavrites. If you start seeing natrolite, labuntsovite, calciohilairite in float, you are in the right ground. Typical habit: prismatic. Train your eye for that shape before scanning the outcrop.







