Intersilite is an extremely rare silicate mineral found in hyper-alkaline igneous rocks. It is typically identified by its delicate, pearly-white tabular crystals often forming radial aggregates within pegmatite pockets.
Is this intersilite?
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 intersilite with a known reference. Intersilite 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. Intersilite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Intersilite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, tabular aggregates.
Often confused with
Intersilite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside intersilite
Minerals reported to co-occur with intersilite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄MnTiSi₁₀O₂₄(OH)₄·5H₂O
- Mohs hardness
- 3-4
- Density
- 2.1-2.2 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Tabular Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find intersilite
Classic worldwide localities
- Kola Peninsula, Russia
- Mount Saint-Hilaire, Canada
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where intersilite typically forms. If you start seeing aegirine, microcline, nepheline in float, you are in the right ground. Field specimens usually show a platy crystals, tabular aggregates habit, so train your eye for that shape before scanning the outcrop.






