Normandite is a rare silicate mineral belonging to the Wöhlerite group, typically found in alkaline igneous rocks like nepheline syenites. It appears as small, prismatic, yellowish-brown crystals often associated with complex suite of rare-earth and alkali minerals in pegmatite cavities.
Is this normandite?
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 normandite with a known reference. Normandite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Normandite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Normandite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to tabular crystals.
Often confused with
Normandite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside normandite
Minerals reported to co-occur with normandite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa(Mn,Fe)(Ti,Zr,Nb)Si₂O₇(O,OH,F)₂
- Mohs hardness
- 5-6
- Density
- 3.46 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Tabular Crystals
- Cleavage
- Distinct On {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find normandite
Classic worldwide localities
- Mont Saint-Hilaire, Canada
- Khibiny Massif, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in nepheline syenite pegmatites country, the host setting where normandite typically forms. If you start seeing aegirine, microcline, nepheline in float, you are in the right ground. Field specimens usually show a prismatic to tabular crystals habit, so train your eye for that shape before scanning the outcrop.






