Seidite-(Ce) is an extremely rare silicate mineral characterized by its thin, fragile tabular crystal habit and yellow-to-brown coloration. It is primarily found as an accessory mineral in complex agpaitic alkaline pegmatites, most notably within the Khibiny Massif in Russia. Collectors prize it for its unique chemical structure, though its rarity makes high-quality display specimens difficult to acquire.
Is this seidite-(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 seidite-(ce) with a known reference. Seidite-(Ce) sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Seidite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Seidite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: thin tabular crystals.
Often confused with
Seidite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside seidite-(ce)
Minerals reported to co-occur with seidite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄Ce₂TiSi₈O₂₂·5H₂O
- Mohs hardness
- 3
- Density
- 2.8 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Thin Tabular Crystals
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Agpaitic Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find seidite-(ce)
Classic worldwide localities
- Khibiny Massif, Kola Peninsula, Russia
Field-hunting tip
Look in agpaitic pegmatites country — that is the host setting where seidite-(ce) typically forms. If you start seeing microcline, aegirine, nepheline in float, you are in the right ground. Field specimens usually show a thin tabular crystals habit, so train your eye for that shape before scanning the outcrop.





