Fedorite is a rare phyllosilicate mineral typically occurring as thin, pearly, micaceous flakes or platy crystals within alkaline rock environments. Collectors often find it associated with other exotic minerals in the pegmatites of the Khibiny or Murun Massifs. Due to its delicate, sheet-like structure and rarity, it is primarily sought after by advanced mineral collectors specializing in rare silicates.
Is this fedorite?
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 fedorite with a known reference. Fedorite sits at Mohs 3-4, 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, satiny, pearly.
- 4Match the color rangeCompare against the expected color range: colorless, light red, pearl white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: pseudo hexagonal, tabular.
Often confused with
Fedorite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fedorite
Minerals reported to co-occur with fedorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KNa₂Ca₂(Si₈O₁₉)(OH,F)₂·H₂O
- Mohs hardness
- 3-4
- Density
- 2.43-2.58 g/cm³
- Streak
- White
- Luster
- Vitreous, satiny, pearly
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Pseudo hexagonal, tabular
- Cleavage
- Perfect micaceous on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In fine veinlets in fenitized sandstone (Turii Peninsula, Russia)
Where rockhounds find fedorite
Classic worldwide localities
- Turii Peninsula, Kola Peninsula, and in the Murun massif, southwest of Olekminsk, Yakutia, Russia
Field-hunting tip
Where it forms: In fine veinlets in fenitized sandstone (Turii Peninsula, Russia). If you start seeing narsarsukite, quartz, apophyllite in float, you are in the right ground. Typical habit: pseudo hexagonal, tabular. Train your eye for that shape before scanning the outcrop.



