Lemmleinite-K is a rare mineral belonging to the labuntsovite group, typically found as small, colorless prismatic crystals. It is primarily identified within the alkaline pegmatites of the Khibiny Massif in Russia, often associated with microcline and aegirine.
Is this lemmleinite-k?
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 lemmleinite-k with a known reference. Lemmleinite-K 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.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, pseudo orthorhombic.
Often confused with
Lemmleinite-K vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lemmleinite-k
Minerals reported to co-occur with lemmleinite-k. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄K₈Ti₈(Si₄O₁₂)₄(O,OH)₈·8H₂O
- Mohs hardness
- 5
- Density
- 2.80 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, pseudo orthorhombic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In ultra-agpaitic pegmatites in apatite-nepheline in an alkaline massif
Where rockhounds find lemmleinite-k
Classic worldwide localities
- Mount Koashva, Khibina alkaline massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In ultra-agpaitic pegmatites in apatite-nepheline in an alkaline massif. If you start seeing sodalite, natrolite, aegirine in float, you are in the right ground. Typical habit: fibrous, pseudo orthorhombic. Train your eye for that shape before scanning the outcrop.








