Iimoriite-(Y) is a rare yttrium-bearing silicate-carbonate mineral first discovered in the Iimori mine in Japan. It typically occurs as massive, granular aggregates in granitic pegmatites and is often associated with other rare-earth minerals like xenotime and fergusonite.
Is this iimoriite-(y)?
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 iimoriite-(y) with a known reference. Iimoriite-(Y) sits at Mohs 5-5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Iimoriite-(Y) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Iimoriite-(Y) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellowish-white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: granular, massive, rarely distinct crystals.
Often confused with
Iimoriite-(Y) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside iimoriite-(y)
Minerals reported to co-occur with iimoriite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Y₂(SiO₄)(CO₃)
- Mohs hardness
- 5-5.5
- Density
- 4.25-4.35 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Granular, Massive, Rarely Distinct Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-300 per specimen depending on size and provenance
Where rockhounds find iimoriite-(y)
Classic worldwide localities
- Iimori mine, Fukushima Prefecture, Japan
- Kola Peninsula, Russia
- Strange Lake, Quebec, Canada
Field-hunting tip
Look in granite pegmatites country — that is the host setting where iimoriite-(y) typically forms. If you start seeing xenotime, fergusonite, allanite in float, you are in the right ground. Field specimens usually show a granular, massive, rarely distinct crystals habit, so train your eye for that shape before scanning the outcrop.




