Rouvilleite is a very rare sodium-calcium carbonate fluoride mineral discovered in the alkaline rocks of Mont Saint-Hilaire. It typically forms small, colorless to white hexagonal tabular crystals that are difficult to distinguish from other carbonates without laboratory analysis. Specimens are highly prized by mineral collectors due to the restricted number of global occurrences.
Is this rouvilleite?
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 rouvilleite with a known reference. Rouvilleite 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 to waxy.
- 4Match the color rangeCompare against the expected color range: colorless, reddish brown, tan.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: irregular grains.
Often confused with
Rouvilleite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rouvilleite
Minerals reported to co-occur with rouvilleite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃Ca₂(CO₃)₃F
- Mohs hardness
- 3-4
- Density
- 2.67-2.73 g/cm³
- Streak
- White
- Luster
- Vitreous to waxy
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Irregular grains
- Cleavage
- Good on {001}; imperfect on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a sodalite xenolith in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada); in a differentiated alkalic massif (Lovozero massif, Kola Peninsula, Russia)
Where rockhounds find rouvilleite
Classic worldwide localities
- Mont Saint-Hilaire, Quebec, Canada
- Mt. Alluaiv, Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In a sodalite xenolith in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada); in a differentiated alkalic massif (Lovozero massif, Kola Peninsula, Russia). If you start seeing kupletskite, villiaumite, aegirine in float, you are in the right ground. Typical habit: irregular grains. Train your eye for that shape before scanning the outcrop.









