Britholite-(Ce) is a rare earth-bearing silicate mineral belonging to the apatite supergroup. It is primarily identified by its characteristic brown color and association with rare alkaline igneous complexes, often requiring testing to distinguish from standard apatite.
Is this britholite-(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 britholite-(ce) with a known reference. Britholite-(Ce) sits at Mohs 5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Britholite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Britholite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, tan, reddish-brown, yellowish-brown.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals, massive, granular.
Often confused with
Britholite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.


How to tell apart: Streak differs — Britholite-(Ce) leaves white, Allanite leaves gray; luster reads vitreous on Britholite-(Ce) and submetallic on Allanite.

How to tell apart: Luster reads vitreous on Britholite-(Ce) and resinous on Monazite.
Often found alongside britholite-(ce)
Minerals reported to co-occur with britholite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ce,Ca,Th)₅(SiO₄,PO₄)₃(OH,F)
- Mohs hardness
- 5.5
- Density
- 4.3-4.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals, Massive, Granular
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks, Pegmatites
- Typical price
- $20-150 thumbnail to small cabinet specimen
Where rockhounds find britholite-(ce)
Classic worldwide localities
- Kola Peninsula, Russia
- Ilimaussaq Complex, Greenland
- Magnet Cove, USA
- Norra Kärr, Sweden
Field-hunting tip
Look in alkaline igneous rocks, pegmatites country — that is the host setting where britholite-(ce) typically forms. If you start seeing aegirine, nepheline, microcline in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.




