Bussyite-(Ce) is a rare beryllium-silicate mineral found within alkaline igneous environments, specifically agpaitic pegmatites. It typically occurs as small yellowish-brown tabular crystals and is prized almost exclusively by advanced systematic mineral collectors due to its extreme rarity.
Is this bussyite-(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 bussyite-(ce) with a known reference. Bussyite-(Ce) sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bussyite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bussyite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-brown, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Bussyite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bussyite-(ce)
Minerals reported to co-occur with bussyite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄Ce₂REE(Be₂Si₂O₈)(SiO₄)F₂
- Mohs hardness
- 5-6
- Density
- 3.32 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Agpaitic Pegmatites
- Typical price
- $100-500 per specimen
Where rockhounds find bussyite-(ce)
Classic worldwide localities
- Kola Peninsula, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in agpaitic pegmatites country — that is the host setting where bussyite-(ce) typically forms. If you start seeing microcline, aegirine, nepheline in float, you are in the right ground. Field specimens usually show a tabular crystals, subparallel aggregates habit, so train your eye for that shape before scanning the outcrop.






