Françoisite-(Nd) is a very rare secondary uranium mineral typically found in the oxidized zones of uranium-rich ore bodies. It usually occurs as small, yellow, platy crystals or thin crusts, often associated with other uranium-bearing minerals.
Is this françoisite-(nd)?
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 françoisite-(nd) with a known reference. Françoisite-(Nd) sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Françoisite-(Nd) leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Françoisite-(Nd) typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Françoisite-(Nd) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside françoisite-(nd)
Minerals reported to co-occur with françoisite-(nd). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Nd,Sm,Gd)(UO₂)₃(PO₄)₂(OH)₃·8H₂O
- Mohs hardness
- 3
- Density
- 4.45 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Dull
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts, Radial Aggregates
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find françoisite-(nd)
Classic worldwide localities
- Masupa-Kabwe, Democratic Republic of the Congo
- Lodève, France
Field-hunting tip
Look in oxidized zones of uranium deposits country — that is the host setting where françoisite-(nd) typically forms. If you start seeing uraninite, parsonsite, torbernite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.




