Kihlmanite-(Ce) is an extremely rare cerium-dominant silicate carbonate typically found in alkaline pegmatites of the Kola Peninsula. It occurs as small, delicate platy or tabular crystals and is highly prized by advanced mineralogists for its complex chemistry and scarcity.
Is this kihlmanite-(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 kihlmanite-(ce) with a known reference. Kihlmanite-(Ce) sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kihlmanite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kihlmanite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellowish-brown, brown, yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, tabular aggregates.
Often confused with
Kihlmanite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kihlmanite-(ce)
Minerals reported to co-occur with kihlmanite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ce₂TiO₂(SiO₄)(CO₃)₂·H₂O
- Mohs hardness
- 3.5-4
- Density
- 3.55 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Tabular Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Pegmatites
- Typical price
- $50-300 for micro-specimens
Where rockhounds find kihlmanite-(ce)
Classic worldwide localities
- Khibiny Massif, Kola Peninsula, Russia
- Lovozero Massif, Kola Peninsula, Russia
Field-hunting tip
Look in alkaline pegmatites country — that is the host setting where kihlmanite-(ce) typically forms. If you start seeing aegirine, k-feldspar, nepheline in float, you are in the right ground. Field specimens usually show a platy crystals, tabular aggregates habit, so train your eye for that shape before scanning the outcrop.





