Zirsilite-(Ce) is a rare cyclosilicate mineral belonging to the eudialyte group, primarily identified in alkaline igneous complexes. It usually forms as small tabular crystals or grains within pegmatitic environments associated with nepheline syenites. Due to its extreme rarity and complex chemistry, it is primarily sought after by advanced systematic mineral collectors.
Is this zirsilite-(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 zirsilite-(ce) with a known reference. Zirsilite-(Ce) sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Zirsilite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Zirsilite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals.
Often confused with
Zirsilite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside zirsilite-(ce)
Minerals reported to co-occur with zirsilite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,K)₃(Ca,Na,Ce)₃(Zr,Ti)Si₈O₂₂(OH,Cl)₂
- Mohs hardness
- 5-6
- Density
- 3.17 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find zirsilite-(ce)
Classic worldwide localities
- Khibiny Massif, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where zirsilite-(ce) typically forms. If you start seeing aegirine, nepheline, microcline in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.






