Epistolite is a rare mineral found primarily in alkaline igneous rocks like nepheline syenites. It is typically identified by its distinct micaceous or platy appearance, often forming flexible, pearly lamellae that resemble mica but with different chemical properties.
Is this epistolite?
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 epistolite with a known reference. Epistolite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Epistolite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Epistolite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, gray, pink, yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: lamellar crystals, tabular, micaceous flakes.
Often confused with
Epistolite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside epistolite
Minerals reported to co-occur with epistolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄TiNb₂(Si₂O₇)₂O₂(OH)₂·4H₂O
- Mohs hardness
- 3.5
- Density
- 2.9 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Lamellar Crystals, Tabular, Micaceous Flakes
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites
- Typical price
- $20-150 per specimen depending on size and quality
Where rockhounds find epistolite
Classic worldwide localities
- Kola Peninsula, Russia
- Mont Saint-Hilaire, Canada
Field-hunting tip
Look in nepheline syenite pegmatites country — that is the host setting where epistolite typically forms. If you start seeing aegirine, microcline, nepheline in float, you are in the right ground. Field specimens usually show a lamellar crystals, tabular, micaceous flakes habit, so train your eye for that shape before scanning the outcrop.






