Pilawite-(Y) is an exceptionally rare silicate mineral member of the gadolinite group, typically found in pegmatitic environments. Collectors should look for dark, heavy crystals often displaying metamict features due to natural radioactive decay.
Is this pilawite-(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 pilawite-(y) with a known reference. Pilawite-(Y) sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pilawite-(Y) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pilawite-(Y) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black, brownish-black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, massive.
Often confused with
Pilawite-(Y) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pilawite-(y)
Minerals reported to co-occur with pilawite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaY₂Fe²⁺Si₂O₁₀
- Mohs hardness
- 6.5-7
- Density
- 4.5-4.8 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-500 thumbnail
Where rockhounds find pilawite-(y)
Classic worldwide localities
- Poland
- Russia
- Sweden
Field-hunting tip
Look in granite pegmatites country — that is the host setting where pilawite-(y) typically forms. If you start seeing quartz, feldspar, zircon in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive habit, so train your eye for that shape before scanning the outcrop.





