Agrinierite is a rare, vibrant orange uranyl oxide mineral that typically forms as a secondary mineral in the oxidized zones of uranium deposits. Collectors should look for its distinctive platy, orange crystals that often occur as thin crusts on uranium-bearing host rocks.
Is this agrinierite?
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 agrinierite with a known reference. Agrinierite 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. Streak: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: resinous to greasy.
- 4Match the color rangeCompare against the expected color range: orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: lamellar, pseudo hexagonal.
Often confused with
Agrinierite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside agrinierite
Minerals reported to co-occur with agrinierite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Ca[(UO₂)₃O₃(OH)₂]₂·5H₂O
- Mohs hardness
- 3
- Density
- 5.7 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Resinous to greasy
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Lamellar, pseudo hexagonal
- Cleavage
- {001}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidation zone of a uranium deposit
Where rockhounds find agrinierite
Classic worldwide localities
- Margnac mine, Compreignac, Haute-Vienne, France
Field-hunting tip
Where it forms: In the oxidation zone of a uranium deposit. If you start seeing uranophane, gummite in float, you are in the right ground. Typical habit: lamellar, pseudo hexagonal. Train your eye for that shape before scanning the outcrop.



