Galgenbergite-(Ce) is an extremely rare calcium-cerium carbonate mineral first discovered at the Galgenberg locality in Germany. It typically forms small, platy, pseudo-hexagonal crystals that can be confused with other rare-earth minerals like parisite or bastnäsite. Collectors usually acquire it in micro-mounts or small specimens due to its limited global distribution.
Is this galgenbergite-(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 galgenbergite-(ce) with a known reference. Galgenbergite-(Ce) sits at Mohs 4-4.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Galgenbergite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Galgenbergite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, tan.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, pseudo-hexagonal clusters.
Often found alongside galgenbergite-(ce)
Minerals reported to co-occur with galgenbergite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCe₂(CO₃)₄
- Mohs hardness
- 4-4.5
- Density
- 4.15 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Pseudo-hexagonal Clusters
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Metamorphic Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find galgenbergite-(ce)
Classic worldwide localities
- Galgenberg, Saxony, Germany
Field-hunting tip
Look in hydrothermal veins in metamorphic rocks country — that is the host setting where galgenbergite-(ce) typically forms. If you start seeing fluorite, quartz, calcite in float, you are in the right ground. Field specimens usually show a platy crystals, pseudo-hexagonal clusters habit, so train your eye for that shape before scanning the outcrop.




