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 4.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gagarinite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Gagarinite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, white, yellowish, colorless.
- 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
- 4.5
- Density
- 4.57 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites, Agpaitic Nepheline Syenites
- Typical price
- $50-300 per specimen depending on size and provenance
Where rockhounds find gagarinite-(ce)
Classic worldwide localities
- Lovozero Massif, Russia
- Mont Saint-Hilaire, Canada
- Khibiny Massif, Russia
- Burpala Massif, Russia
Field-hunting tip
Look in alkaline pegmatites, agpaitic nepheline syenites country — that is the host setting where gagarinite-(ce) typically forms. If you start seeing eudialyte, microcline, nepheline in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive habit, so train your eye for that shape before scanning the outcrop.







