Labuntsovite-Fe is a rare member of the complex labuntsovite group of titanium silicates. It typically forms small, prismatic to tabular crystals in alkaline pegmatites and is most sought after by advanced micromount and systematic collectors.
Is this labuntsovite-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 labuntsovite-fe with a known reference. Labuntsovite-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: orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains.
Often confused with
Labuntsovite-Fe vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside labuntsovite-fe
Minerals reported to co-occur with labuntsovite-fe. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄K₄Fe₂Ti₈O₄(Si₄O₁₂)₄(OH)₄·10-12H₂O
- Mohs hardness
- 5
- Density
- 2.94 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent to transparent
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral grains
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In K-feldspar-natrolite-calcite veinlets in hydrothermally altered urtite
Where rockhounds find labuntsovite-fe
Classic worldwide localities
- Khibiny Massif, Russia
- Lovozero Massif, Russia
- Mont Saint-Hilaire, Canada
Field-hunting tip
Where it forms: In K-feldspar-natrolite-calcite veinlets in hydrothermally altered urtite. If you start seeing pectolite, fluorite, aegirine in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.





