Biraite-(Ce) is an extremely rare cerium-iron carbonate-silicate typically found in alkaline rock formations. It usually occurs as small, tabular, yellowish-brown crystals and is primarily a target for advanced systematic mineral collectors due to its limited type locality in the Russian Far East.
Is this biraite-(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 biraite-(ce) with a known reference. Biraite-(Ce) sits at Mohs 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: brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: irregular grains.
Often confused with
Biraite-(Ce) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside biraite-(ce)
Minerals reported to co-occur with biraite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ce₂FeSi₂O₇(CO₃)
- Mohs hardness
- 5
- Density
- 4.76 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Irregular grains
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a vein that cuts fenite fragments in a carbonatite
Where rockhounds find biraite-(ce)
Classic worldwide localities
- Biraia cabonatite dike, 145-150 km east of Bodaibo, Northern Irkutsk district, Siberia, Russia
Field-hunting tip
Where it forms: In a vein that cuts fenite fragments in a carbonatite. If you start seeing cordylite-, aragonite, dolomite in float, you are in the right ground. Typical habit: irregular grains. Train your eye for that shape before scanning the outcrop.






