Parisite-(Ce) is a rare earth fluorocarbonate mineral recognized for its distinctive, often elongated, pseudo-hexagonal bipyramidal crystal habits. It is highly sought after by collectors for its sharp, translucent brown crystals, particularly those originating from the classic emerald-bearing hydrothermal deposits in Colombia.
Is this parisite-(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 parisite-(ce) with a known reference. Parisite-(Ce) sits at Mohs 4.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Parisite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Parisite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: hexagonal bipyramidal crystals, often in tapered or pseudo-hexagonal aggregates.
Often found alongside parisite-(ce)
Minerals reported to co-occur with parisite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCe₂(CO₃)₃F₂
- Mohs hardness
- 4.5
- Density
- 4.42 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Hexagonal Bipyramidal Crystals, Often in Tapered or Pseudo-hexagonal Aggregates
- Cleavage
- Distinct Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Carbonatites, Hydrothermal Veins, And Alkaline Igneous Rocks
- Typical price
- $20-150 thumbnail, $200-800 cabinet specimen
Where rockhounds find parisite-(ce)
Classic worldwide localities
- Muzo, Colombia
- Khibiny Massif, Russia
- Mont Saint-Hilaire, Canada
- Mountain Pass, USA
- Bayun Obo, China
Field-hunting tip
Look in carbonatites, hydrothermal veins, and alkaline igneous rocks country — that is the host setting where parisite-(ce) typically forms. If you start seeing calcite, fluorite, barite in float, you are in the right ground. Field specimens usually show a hexagonal bipyramidal crystals, often in tapered or pseudo-hexagonal aggregates habit, so train your eye for that shape before scanning the outcrop.





