Liandratite is an extremely rare uranium-niobium-tantalum oxide mineral typically found in granitic pegmatites. Collectors should look for small, platy yellow crystals associated with other rare-earth minerals, noting its distinct radioactivity.
Is this liandratite?
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 liandratite with a known reference. Liandratite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: glassy.
- 4Match the color rangeCompare against the expected color range: yellow, brown, brownish yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: encrustations, metamict.
Often found alongside liandratite
Minerals reported to co-occur with liandratite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- UNb₂O₈
- Mohs hardness
- 3.5
- Density
- 7.0 g/cm³
- Streak
- Pale yellow
- Luster
- Glassy
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Encrustations, metamict
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific study
- Host rock
- In a zoned pegmatite in amphibolite-grade gneiss, as an oxidized crust over petscheckite
Where rockhounds find liandratite
Classic worldwide localities
- Antsakoa I pegmatite, Fianavantsoa, near Berere, about 40 km northeast of Tsaratanana, Madagascar
Field-hunting tip
Where it forms: In a zoned pegmatite in amphibolite-grade gneiss, as an oxidized crust over petscheckite. If you start seeing petscheckite, columbite, pyrochlore in float, you are in the right ground. Typical habit: encrustations, metamict. Train your eye for that shape before scanning the outcrop.





