Alsakharovite-Zn is a very rare mineral belonging to the complex labuntsovite group of titanosilicates. It typically occurs as small, yellowish-brown prismatic crystals within alkaline pegmatites, primarily documented in the Kola Peninsula of Russia.
Is this alsakharovite-zn?
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 alsakharovite-zn with a known reference. Alsakharovite-Zn 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: white, pale brown, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic, tabular.
Often confused with
Alsakharovite-Zn vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside alsakharovite-zn
Minerals reported to co-occur with alsakharovite-zn. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaSrKZn(Ti,Nb)₄(Si₄O₁₂)₂O₄·7H₂O
- Mohs hardness
- 5
- Density
- 2.90 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic, tabular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In cavities in eudialyte-aegirine-feldspar pegmatite in an alkaline massif
Where rockhounds find alsakharovite-zn
Classic worldwide localities
- Mt. Lepkhe-Nelm, Lovozero alkaline massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In cavities in eudialyte-aegirine-feldspar pegmatite in an alkaline massif. If you start seeing lamprophyllite, natrolite, halloysite in float, you are in the right ground. Typical habit: prismatic, tabular. Train your eye for that shape before scanning the outcrop.







