Bijvoetite-(Y) is an extremely rare secondary uranium carbonate mineral found primarily in the oxidation zones of uranium deposits. Collectors typically look for its distinct yellow platy crystals or crusts, which exhibit notable fluorescence under ultraviolet light.
Is this bijvoetite-(y)?
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 bijvoetite-(y) with a known reference. Bijvoetite-(Y) sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: sulfur yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: microscopic crystals, tabular.
Often confused with
Bijvoetite-(Y) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bijvoetite-(y)
Minerals reported to co-occur with bijvoetite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Y₈(UO₂)₁₆O₈(CO₃)₁₆(OH)₈·39H₂O
- Mohs hardness
- 2
- Density
- 3.9 g/cm³
- Colors
- Sulfur yellow
- Streak
- Light yellow
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Microscopic crystals, tabular
- Cleavage
- On {001}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Very rare, in the lower portion of the oxidation zone developed above uraninite-bearing dolomitic rocks
Where rockhounds find bijvoetite-(y)
Classic worldwide localities
- Shinkolobwe, Katanga Province, Congo (Shaba Province, Zaire)
Field-hunting tip
Where it forms: Very rare, in the lower portion of the oxidation zone developed above uraninite-bearing dolomitic rocks. If you start seeing lepersonnite-, sklodowskite, curite in float, you are in the right ground. Typical habit: microscopic crystals, tabular. Train your eye for that shape before scanning the outcrop.







