Bussyite-(Y) is an exceptionally rare silicate mineral primarily found in agpaitic alkaline igneous rocks. It typically forms small, prismatic to tabular crystals and is highly prized by advanced mineral collectors for its complexity and scarcity.
Is this bussyite-(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 bussyite-(y) with a known reference. Bussyite-(Y) 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to tabular crystals.
Often confused with
Bussyite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bussyite-(y)
Minerals reported to co-occur with bussyite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Y,REE,Ca)₃(Na,Ca)₆MnSi₉Be₅(O,F,OH)₃₄
- Mohs hardness
- ~4
- Density
- 3.11 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to tabular crystals
- Cleavage
- Perfect on {101}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late-stage hydrothermal product in alkaline pegmatite
Where rockhounds find bussyite-(y)
Classic worldwide localities
- Poudrette quarry (level 7), Mont Saint-Hilaire, Rouville County, Quebec, Canada
Field-hunting tip
Where it forms: A late-stage hydrothermal product in alkaline pegmatite. If you start seeing analcime, microcline, sérandite in float, you are in the right ground. Typical habit: prismatic to tabular crystals. Train your eye for that shape before scanning the outcrop.








