Fluorbritholite-(Ce) is a rare silicate mineral belonging to the apatite supergroup, characterized by its cerium-rich composition. It usually occurs as earthy or resinous brown masses in alkaline pegmatites and is often radioactive due to its rare earth element content.
Is this fluorbritholite-(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 fluorbritholite-(ce) with a known reference. Fluorbritholite-(Ce) sits at Mohs 5-5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Fluorbritholite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fluorbritholite-(Ce) typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: brown, reddish-brown, yellow, gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals, massive.
Often confused with
Fluorbritholite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fluorbritholite-(ce)
Minerals reported to co-occur with fluorbritholite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ce,Ca,Y)₅(SiO₄,PO₄)₃F
- Mohs hardness
- 5-5.5
- Density
- 4.5-4.8 g/cm³
- Streak
- White
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks, Syenite Pegmatites
- Typical price
- $20-150 for small specimens
Where rockhounds find fluorbritholite-(ce)
Classic worldwide localities
- Lovozero Massif, Russia
- Khibiny Massif, Russia
- Norra Kärr, Sweden
- Langesundsfjord, Norway
Field-hunting tip
Look in alkaline igneous rocks, syenite pegmatites country — that is the host setting where fluorbritholite-(ce) typically forms. If you start seeing aegirine, nepheline, eudialyte 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.







