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 — that is 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.





