Braitschite-(Ce) is a very rare hydrated calcium cerium borate mineral typically found in marine evaporite deposits. It usually occurs as small, delicate platy crystals or granular masses embedded within potash or halite beds. Collectors generally look for it in specialized research-grade collections focusing on rare borate mineralogy.
Is this braitschite-(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 braitschite-(ce) with a known reference. Braitschite-(Ce) sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Braitschite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Braitschite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, yellow, colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, granular aggregates.
Often confused with
Braitschite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside braitschite-(ce)
Minerals reported to co-occur with braitschite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Na)₇(Ce,La)₂Ti(B₈O₃₀)(OH)₂·10H₂O
- Mohs hardness
- 3
- Density
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Platy Crystals, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Evaporite Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find braitschite-(ce)
Classic worldwide localities
- Paradox Member of the Hermosa Formation, Utah, USA
- Potash deposits of the Paradox Basin, USA
Field-hunting tip
Look in evaporite deposits country — that is the host setting where braitschite-(ce) typically forms. If you start seeing halite, sylvite, anhydrite in float, you are in the right ground. Field specimens usually show a platy crystals, granular aggregates habit, so train your eye for that shape before scanning the outcrop.






