Ilmajokite-(Ce) is a rare hydrated sodium-cerium-titanium silicate belonging to the eudialyte group. It occurs as microscopic, yellowish-brown anhedral grains found within alkaline pegmatite environments in Finland.
Is this ilmajokite-(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 ilmajokite-(ce) with a known reference. Ilmajokite-(Ce) sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ilmajokite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ilmajokite-(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: anhedral grains.
Often confused with
Ilmajokite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ilmajokite-(ce)
Minerals reported to co-occur with ilmajokite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ce,Ba)₄(Ti,Nb)Si₄O₁₃(OH,F)₂·nH₂O
- Mohs hardness
- 5
- Density
- 2.8 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- n/a
Where rockhounds find ilmajokite-(ce)
Classic worldwide localities
- Ilmajoki, Finland
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where ilmajokite-(ce) typically forms. If you start seeing arfvedsonite, albite, aegirine in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.





