Rémondite-(La) is an exceptionally rare rare-earth element carbonate mineral primarily found in the nepheline syenite pegmatites of Mont Saint-Hilaire. Collectors usually seek it in the form of small, tabular, transparent to translucent crystals associated with other rare alkaline-suite minerals.
Is this rémondite-(la)?
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 rémondite-(la) with a known reference. Rémondite-(La) sits at Mohs ~3, 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.
- 4Match the color rangeCompare against the expected color range: bright orange yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: irregular grains, microscopic crystals, prismatic.
Often confused with
Rémondite-(La) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rémondite-(la)
Minerals reported to co-occur with rémondite-(la). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃(La,Ca,Na)₃(CO₃)₅
- Mohs hardness
- ~3
- Density
- 3.5 g/cm³
- Colors
- Bright orange yellow
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Irregular grains, microscopic crystals, prismatic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of late hydrothermal origin, very rare in a small pegmatite in a differentiated alkalic massif
Where rockhounds find rémondite-(la)
Classic worldwide localities
- Mt. Koashva, Khibiny massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: Of late hydrothermal origin, very rare in a small pegmatite in a differentiated alkalic massif. If you start seeing cancrisilite, microcline, sodalite in float, you are in the right ground. Typical habit: irregular grains, microscopic crystals, prismatic. Train your eye for that shape before scanning the outcrop.







