Coskrenite-(Ce) is a rare cerium oxalate mineral found primarily in alkaline igneous environments. It typically forms as delicate, tabular, pale yellow crystals or radiating clusters within vugs or cavities of pegmatite host rocks.
Is this coskrenite-(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 coskrenite-(ce) with a known reference. Coskrenite-(Ce) sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Coskrenite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Coskrenite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, radiating aggregates.
Often confused with
Coskrenite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside coskrenite-(ce)
Minerals reported to co-occur with coskrenite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ce,Nd,La)₂(C₂O₄)₃·10H₂O
- Mohs hardness
- 2-3
- Density
- 2.61 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Radiating Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites, Hydrothermal Cavities
- Typical price
- $50-500 depending on specimen size and rarity
Where rockhounds find coskrenite-(ce)
Classic worldwide localities
- Khibiny Massif, Russia
- Zagi Mountain, Pakistan
Field-hunting tip
Look in alkaline pegmatites, hydrothermal cavities country — that is the host setting where coskrenite-(ce) typically forms. If you start seeing synchysite-(ce), parisite-(ce), quartz in float, you are in the right ground. Field specimens usually show a tabular crystals, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.






