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 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Shafranovskite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Shafranovskite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, golden yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: lamellar crystals, tabular hexagonal plates.
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
- (K,Na,Ca)₃(Mn,Fe)₄Si₅O₁₅(OH)·2H₂O
- Mohs hardness
- 2
- Density
- 2.36 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Lamellar Crystals, Tabular Hexagonal Plates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find shafranovskite
Classic worldwide localities
- Khibiny Massif, Kola Peninsula, Russia
Field-hunting tip
Look in nepheline syenite pegmatites country — that is the host setting where shafranovskite typically forms. If you start seeing aegirine, eudialyte, kalsilite in float, you are in the right ground. Field specimens usually show a lamellar crystals, tabular hexagonal plates habit, so train your eye for that shape before scanning the outcrop.





