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 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Labuntsovite-Fe leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Labuntsovite-Fe typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: orange, brown, yellow, red.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to tabular crystals.
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
- K₂Ti₄(Si₄O₁₂)(O,OH)₄·5H₂O
- Mohs hardness
- 5-6
- Density
- 2.8-2.9 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Tabular Crystals
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites
- Typical price
- $20-150 per specimen
Where rockhounds find labuntsovite-fe
Classic worldwide localities
- Khibiny Massif, Russia
- Lovozero Massif, Russia
- Mont Saint-Hilaire, Canada
Field-hunting tip
Look in nepheline syenite pegmatites country — that is the host setting where labuntsovite-fe typically forms. If you start seeing aegirine, microcline, eudialyte in float, you are in the right ground. Field specimens usually show a prismatic to tabular crystals habit, so train your eye for that shape before scanning the outcrop.






