Phosinaite-(Ce) is a rare silicate-phosphate mineral found almost exclusively in the highly alkaline agpaitic pegmatites of the Kola Peninsula. It typically occurs as small prismatic to lath-like crystals that are notable for their strong white fluorescence under short-wave ultraviolet light.
Is this phosinaite-(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 phosinaite-(ce) with a known reference. Phosinaite-(Ce) sits at Mohs 4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Phosinaite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Phosinaite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow, pale pink.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, lath-like aggregates.
Often confused with
Phosinaite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside phosinaite-(ce)
Minerals reported to co-occur with phosinaite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₂Ca₄(Ce,La)₂Ti(Si₂O₇)₂(PO₄)₆F₂
- Mohs hardness
- 4
- Density
- 2.81 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Lath-like Aggregates
- Cleavage
- Perfect
- Fluorescence
- Bright White Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Agpaitic Pegmatites and Alkaline Igneous Complexes
- Typical price
- $50-300 per specimen
Where rockhounds find phosinaite-(ce)
Classic worldwide localities
- Khibiny Massif, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in agpaitic pegmatites and alkaline igneous complexes country — that is the host setting where phosinaite-(ce) typically forms. If you start seeing aegirine, nepheline, eudialyte in float, you are in the right ground. Field specimens usually show a prismatic crystals, lath-like aggregates habit, so train your eye for that shape before scanning the outcrop.






