Soddyite is a striking secondary uranium mineral characterized by its bright yellow to yellow-orange crystal clusters. It is typically found in the oxidized zones of uranium deposits and is highly prized by collectors for its vibrant fluorescence under ultraviolet light.
Is this soddyite?
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 soddyite with a known reference. Soddyite 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. Soddyite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Soddyite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange, brownish-yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: dipyramidal crystals, granular, massive.
Often confused with
Soddyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside soddyite
Minerals reported to co-occur with soddyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (UO₂)₂SiO₄·2H₂O
- Mohs hardness
- 3.5
- Density
- 4.7-4.8 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Dipyramidal Crystals, Granular, Massive
- Cleavage
- Distinct
- Fluorescence
- Strong Yellow-green Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium Deposits
- Typical price
- $50-500 depending on specimen size and quality
Where rockhounds find soddyite
Classic worldwide localities
- Shinkolobwe, Democratic Republic of the Congo
- Musonoi Mine, Democratic Republic of the Congo
- Arvee Prospect, Australia
Field-hunting tip
Look in oxidized zones of uranium deposits country, the host setting where soddyite typically forms. If you start seeing curite, vandenbrandeite, becquerelite in float, you are in the right ground. Field specimens usually show a dipyramidal crystals, granular, massive habit, so train your eye for that shape before scanning the outcrop.





