Lepersonnite-(Gd) is a rare uranyl carbonate-silicate mineral found almost exclusively in the Shinkolobwe mine. It is highly prized by collectors for its vibrant yellow color, distinct bladed habit, and intense fluorescence under ultraviolet light.
Is this lepersonnite-(gd)?
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 lepersonnite-(gd) with a known reference. Lepersonnite-(Gd) sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Lepersonnite-(Gd) leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Lepersonnite-(Gd) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular or bladed crystals, radiating clusters.
Often confused with
Lepersonnite-(Gd) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lepersonnite-(gd)
Minerals reported to co-occur with lepersonnite-(gd). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaGd₂(UO₂)₂₄(CO₃)₈(SiO₄)₄(OH)₂₄·48H₂O
- Mohs hardness
- 2-3
- Density
- 4.1 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular or Bladed Crystals, Radiating Clusters
- Cleavage
- None
- Fluorescence
- Bright Yellow-green Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium Deposits
- Typical price
- $100-1000 per specimen depending on size and quality
Where rockhounds find lepersonnite-(gd)
Classic worldwide localities
- Shinkolobwe mine, Democratic Republic of the Congo
Field-hunting tip
Look in oxidized zones of uranium deposits country — that is the host setting where lepersonnite-(gd) typically forms. If you start seeing curite, kasolite, studtite in float, you are in the right ground. Field specimens usually show a acicular or bladed crystals, radiating clusters habit, so train your eye for that shape before scanning the outcrop.




