Gagarinite-(Ce) is a rare sodium-calcium-cerium fluoride mineral that occurs primarily in alkaline pegmatites. It is best identified by its association with unique mineral suites in agpaitic complexes and typically presents as small, pale-colored hexagonal prisms or irregular masses.
Is this gagarinite-(ce)?
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 gagarinite-(ce) with a known reference. Gagarinite-(Ce) 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, pale pink.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals, massive.
Often confused with
Gagarinite-(Ce) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gagarinite-(ce)
Minerals reported to co-occur with gagarinite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCaCeF₆
- Mohs hardness
- 3.5
- Density
- 4.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic crystals, massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a rare-earth-element enriched, peralkaline granitic complex (Strange Lake)
Where rockhounds find gagarinite-(ce)
Classic worldwide localities
- Strange Lake deposit, Quebec-Labrador, Canada
Field-hunting tip
Where it forms: In a rare-earth-element enriched, peralkaline granitic complex (Strange Lake). If you start seeing vlasovite, narsarsukite, willemite in float, you are in the right ground. Typical habit: prismatic crystals, massive. Train your eye for that shape before scanning the outcrop.






