Ferronordite-(Ce) is a rare silicate mineral primarily found in the highly alkaline intrusive complexes of the Kola Peninsula. It typically appears as yellowish-white tabular or prismatic crystals embedded within pegmatitic rocks. Collectors value it as a scarce member of the complex alkaline mineral suite associated with nepheline syenites.
Is this ferronordite-(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 ferronordite-(ce) with a known reference. Ferronordite-(Ce) sits at Mohs 5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ferronordite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ferronordite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellowish-white, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, prismatic crystals.
Often confused with
Ferronordite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferronordite-(ce)
Minerals reported to co-occur with ferronordite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃SrCeFeSi₆O₁₇
- Mohs hardness
- 5.5
- Density
- 3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Syenites and Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find ferronordite-(ce)
Classic worldwide localities
- Lovozero Massif, Russia
- Khibiny Massif, Russia
Field-hunting tip
Look in alkaline syenites and pegmatites country — that is the host setting where ferronordite-(ce) typically forms. If you start seeing aegirine, eudialyte, microcline in float, you are in the right ground. Field specimens usually show a tabular crystals, prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





