Shkatulkalite is a rare member of the labuntsovite group typically found as thin, tabular, yellowish-brown crystals. It occurs primarily in the hyperalkaline pegmatites of the Lovozero Massif in Russia. It is best identified by its association with other complex titanium-silicate minerals in alkaline complexes.
Is this shkatulkalite?
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 shkatulkalite with a known reference. Shkatulkalite sits at Mohs 4-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Shkatulkalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Shkatulkalite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, yellowish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, platy aggregates.
Often confused with
Shkatulkalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside shkatulkalite
Minerals reported to co-occur with shkatulkalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₀Nb₂TiSi₄O₁₄(OH,F)₄·nH₂O
- Mohs hardness
- 4-5
- Density
- 2.81 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Platy Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hyperalkaline Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find shkatulkalite
Classic worldwide localities
- Mount Alluaiv, Lovozero Massif, Kola Peninsula, Russia
Field-hunting tip
Look in hyperalkaline pegmatites country, the host setting where shkatulkalite typically forms. If you start seeing microcline, aegirine, eudialyte in float, you are in the right ground. Field specimens usually show a tabular crystals, platy aggregates habit, so train your eye for that shape before scanning the outcrop.






