Neskevaaraite-Fe is a very rare member of the labuntsovite group typically found in alkaline pegmatites on the Kola Peninsula. It occurs as small, yellow to brown prismatic crystals and is primarily sought after by advanced systematic mineral collectors.
Is this neskevaaraite-fe?
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 neskevaaraite-fe with a known reference. Neskevaaraite-Fe 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: pale brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic.
Often confused with
Neskevaaraite-Fe vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside neskevaaraite-fe
Minerals reported to co-occur with neskevaaraite-fe. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaK₃Fe(Ti,Nb)₄(Si₄O₁₂)₂(O,OH)₄·6H₂O
- Mohs hardness
- 5
- Density
- 2.88 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent, almost opaque
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In alkaline igneous rocks sometimes intergrown with labuntsovite-Fe or in hydrothermally altered carbonatite veins
Where rockhounds find neskevaaraite-fe
Classic worldwide localities
- Neskevaara Hill, central part of the Vuoriyarvi alkaline complex, Northern Karelia, and the Kirovskii apatite mine, Mount Kukisvumchorr, Khibiny alkaline massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In alkaline igneous rocks sometimes intergrown with labuntsovite-Fe or in hydrothermally altered carbonatite veins. If you start seeing dolomite, calcite, phlogopite in float, you are in the right ground. Typical habit: prismatic. Train your eye for that shape before scanning the outcrop.







