Shafranovskite is an extremely rare phyllosilicate mineral typically occurring as fragile, golden-yellow hexagonal plates or lamellar aggregates. It is found almost exclusively in the alkaline igneous rocks of the Khibiny Massif in Russia. Collectors prize it for its distinct morphology and association with other rare pegmatite minerals.
Is this shafranovskite?
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 shafranovskite with a known reference. Shafranovskite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: greenish white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow green, yellow orange, olive green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: aggregates, granular.
Often confused with
Shafranovskite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside shafranovskite
Minerals reported to co-occur with shafranovskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃K₂(Mn,Fe,Na)₄[Si₉(O,OH)₂₇](OH)₂(H₂O)n [n ~ 2.33]
- Mohs hardness
- 2-3
- Density
- 2.76-2.78 g/cm³
- Streak
- Greenish white
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Aggregates, granular
- Cleavage
- Well developed on {00*1}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Produced by late-stage crystallization of alkalic nepheline syenite magmas in pegmatites in differentiated alkalic massifs
Where rockhounds find shafranovskite
Classic worldwide localities
- Khibiny Massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: Produced by late-stage crystallization of alkalic nepheline syenite magmas in pegmatites in differentiated alkalic massifs. If you start seeing thermonatrite, natrophosphate, nacaphite in float, you are in the right ground. Typical habit: aggregates, granular. Train your eye for that shape before scanning the outcrop.







