Aleksandrovite is an extremely rare phyllosilicate mineral discovered in the Sakha Republic of Russia. It typically occurs as small tabular crystals within contact-metamorphosed limestone xenoliths. Due to its scarcity, it is almost exclusively found in advanced research collections.
Is this aleksandrovite?
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 aleksandrovite with a known reference. Aleksandrovite sits at Mohs 4-4.5, 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, pearly on cleavage surfaces.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Aleksandrovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside aleksandrovite
Minerals reported to co-occur with aleksandrovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KCa₇Sn₂Li₃Si₁₂O₃₆F₂
- Mohs hardness
- 4-4.5
- Density
- 3.05 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, pearly on cleavage surfaces
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a zoned microcline-calcite vein with aegirine-hedenbergite, quartz, and albite in a glacial moraine boulder
Where rockhounds find aleksandrovite
Classic worldwide localities
- Darai-Pioz glacier, at the junction of the Turkestan, Zeravshan, and Alay Mountain Ranges, Tajikistan
Field-hunting tip
Where it forms: In a zoned microcline-calcite vein with aegirine-hedenbergite, quartz, and albite in a glacial moraine boulder. If you start seeing miserite, baratovite, katayamalite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.








