Bayleyite is a rare secondary uranium carbonate typically found as a result of mine water evaporation in arid environments. It is most easily identified by its bright yellow-orange color and intense green fluorescence under ultraviolet light. Due to its high water content, it is sensitive to atmospheric conditions and should be stored in a controlled environment to prevent dehydration.
Is this bayleyite?
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 bayleyite with a known reference. Bayleyite 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. Bayleyite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bayleyite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, drusy crusts, efflorescent coatings.
Often confused with
Bayleyite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bayleyite
Minerals reported to co-occur with bayleyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂(UO₂)(CO₃)₃·18H₂O
- Mohs hardness
- 2.5
- Density
- 2.16 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Drusy Crusts, Efflorescent Coatings
- Cleavage
- Perfect
- Fluorescence
- Bright Green Under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium-bearing Hydrothermal Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find bayleyite
Classic worldwide localities
- Hillside Mine, Arizona, USA
- Jáchymov, Czech Republic
- Schneeberg, Germany
Field-hunting tip
Look in oxidized zones of uranium-bearing hydrothermal deposits country — that is the host setting where bayleyite typically forms. If you start seeing gypsum, andersonite, schröckingerite in float, you are in the right ground. Field specimens usually show a prismatic crystals, drusy crusts, efflorescent coatings habit, so train your eye for that shape before scanning the outcrop.




