Khibinskite is a rare potassium zirconium silicate discovered in the alkaline massifs of the Kola Peninsula. It typically occurs as small, tabular crystals within nepheline syenites and is highly prized by mineralogists specializing in rare alkaline minerals.
Is this khibinskite?
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 khibinskite with a known reference. Khibinskite sits at Mohs 4.5-5.5, 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: dull or greasy.
- 4Match the color rangeCompare against the expected color range: colorless, white, light yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: inclusions, stellate.
Often confused with
Khibinskite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside khibinskite
Minerals reported to co-occur with khibinskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂ZrSi₂O₇
- Mohs hardness
- 4.5-5.5
- Density
- 3.40 g/cm³
- Streak
- White
- Luster
- Dull or greasy
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Inclusions, stellate
- Cleavage
- Perfect on {001}; perfect on {100}; perfect on {111}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In aegirine-rich metasomatic rocks in a differentiated alkalic massif
Where rockhounds find khibinskite
Classic worldwide localities
- Khibiny massif, in the Hackmann Valley, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In aegirine-rich metasomatic rocks in a differentiated alkalic massif. If you start seeing eudialyte, zircon in float, you are in the right ground. Typical habit: inclusions, stellate. Train your eye for that shape before scanning the outcrop.



