Cayalsite-(Y) is a rare yttrium-dominant silicate mineral belonging to the gadolinite group. It typically occurs as dark, vitreous, prismatic crystals within rare-earth-enriched pegmatites and requires precise chemical analysis for definitive identification.
Is this cayalsite-(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 cayalsite-(y) with a known reference. Cayalsite-(Y) sits at Mohs 6.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cayalsite-(Y) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cayalsite-(Y) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black, brownish-black, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Cayalsite-(Y) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cayalsite-(y)
Minerals reported to co-occur with cayalsite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Y₂Fe²⁺Be₂Si₂O₁₀
- Mohs hardness
- 6.5
- Density
- 4.6-4.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Syenite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find cayalsite-(y)
Classic worldwide localities
- Tvedalen, Larvik, Norway
- Baveno, Italy
- Mount Malosa, Malawi
Field-hunting tip
Look in syenite pegmatites country — that is the host setting where cayalsite-(y) typically forms. If you start seeing quartz, microcline, zircon in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






