Voronkovite is a very rare silicate mineral found in the highly alkaline rocks of the Lovozero Massif in Russia. It typically occurs as small, pseudo-hexagonal tabular crystals associated with other rare-earth and zirconium-bearing minerals in pegmatitic veins.
Is this voronkovite?
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 voronkovite with a known reference. Voronkovite 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: light brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: subhedral crystals.
Often confused with
Voronkovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside voronkovite
Minerals reported to co-occur with voronkovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₅(Na,Ca,Ce)₃(Mn,Ca)₃Fe₃Zr₃Si₂₆O₇₂(OH,O)₄Cl·H₂O
- Mohs hardness
- 5
- Density
- 2.97 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Subhedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a lenticular zoned pegmatite hosted by poikilitic nepheline-sodalite syenite in the middle part of a differentiated alkaline complex
Where rockhounds find voronkovite
Classic worldwide localities
- Shkatulka hyperalkaline pegmatite, Mt. Alluaiv, Lovozero alkaline massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In a lenticular zoned pegmatite hosted by poikilitic nepheline-sodalite syenite in the middle part of a differentiated alkaline complex. If you start seeing microcline, sodalite, nepheline in float, you are in the right ground. Typical habit: subhedral crystals. Train your eye for that shape before scanning the outcrop.







