Christofschäferite-(Ce) is a rare cerium lanthanum calcium silicate that forms black stubby prismatic crystals or isolated grains. It is a metasomatic reaction product between Mn-rich rock and alkali basalt, found in a volcanic ejectum. It was first described from Wingertsbergwand (Wingertsberg Mt.) of the Laacher See volcano near Mendig, Eifel Mountains, Rhineland-Palatinate (Rheinland-Pfalz), Germany.
Is this christofschäferite-(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 christofschäferite-(ce) with a known reference. Christofschäferite-(Ce) sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Christofschäferite-(Ce) leaves a brown streak.
- 3Read the lusterHold the specimen under a strong light. Christofschäferite-(Ce) typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: stubby prismatic crystals or isolated grains.
Often confused with
Christofschäferite-(Ce) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside christofschäferite-(ce)
Minerals reported to co-occur with christofschäferite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ce,La,Ca)₄Mn(Ti,Fe)₃(Fe,Ti)(Si₂O₇)₂O₈
- Mohs hardness
- 6
- Density
- 4.8 g/cm³
- Colors
- Streak
- Brown
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Stubby Prismatic Crystals or Isolated Grains
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Volcanic Ejecta
Where rockhounds find christofschäferite-(ce)
Classic worldwide localities
- Eifel volcanic field, Germany
Field-hunting tip
Look in volcanic ejecta country, the host setting where christofschäferite-(ce) typically forms. If you start seeing sanidine, augite, magnetite in float, you are in the right ground. Field specimens usually show a stubby prismatic crystals or isolated grains habit, so train your eye for that shape before scanning the outcrop.





