Rutherfordine is a secondary uranium mineral often found as an alteration product of uraninite in the oxidation zones of uranium-bearing deposits. It typically forms delicate, yellow, needle-like or bladed crystals, though it is more frequently encountered as earthy, powdery coatings on host rocks.
Is this rutherfordine?
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 rutherfordine with a known reference. Rutherfordine sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rutherfordine leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Rutherfordine typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular, bladed, or earthy crusts.
Often confused with
Rutherfordine vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rutherfordine
Minerals reported to co-occur with rutherfordine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- UO₂(CO₃)
- Mohs hardness
- 2.5
- Density
- 4.82 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular, Bladed, Or Earthy Crusts
- Cleavage
- Perfect in One Direction
- Fluorescence
- Bright Yellow-green Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium Deposits
- Typical price
- $50-500 thumbnail to small cabinet specimens
Where rockhounds find rutherfordine
Classic worldwide localities
- Democratic Republic of the Congo
- Czech Republic
- USA (Wyoming)
- Germany
- France
Field-hunting tip
Look in oxidized zones of uranium deposits country, the host setting where rutherfordine typically forms. If you start seeing uraninite, becquerelite, curite in float, you are in the right ground. Field specimens usually show a acicular, bladed, or earthy crusts habit, so train your eye for that shape before scanning the outcrop.





