Fergusonite-(Ce) is a rare radioactive rare-earth niobate mineral typically found in granitic pegmatites. It usually forms as small, brownish-black tetragonal prisms that are often metamict due to internal radiation damage. Collectors prize it for its unique chemistry and association with other rare earth minerals.
Is this fergusonite-(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 fergusonite-(ce) with a known reference. Fergusonite-(Ce) sits at Mohs 5.5-6.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Fergusonite-(Ce) leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Fergusonite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, black, yellow, orange.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic crystals.
Often confused with
Fergusonite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fergusonite-(ce)
Minerals reported to co-occur with fergusonite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CeNbO₄
- Mohs hardness
- 5.5-6.5
- Density
- 5.6-5.8 g/cm³
- Streak
- Pale Yellow
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $20-150 per specimen depending on size and quality
Where rockhounds find fergusonite-(ce)
Classic worldwide localities
- Sweden
- Norway
- Canada
- USA
- Russia
Field-hunting tip
Look in granite pegmatites country — that is the host setting where fergusonite-(ce) typically forms. If you start seeing allanite, zircon, monazite 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.






