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 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, dulling with dehydration.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow, yellowish white.
- 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
- 2-2.5
- Density
- 2.05 g/cm³
- Streak
- White
- Luster
- Vitreous, dulling with dehydration
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, drusy crusts, efflorescent coatings
- Cleavage
- None
- Fluorescence
- Yellow under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As a coating or efflorescence with other secondary uranium minerals, which may be post-mining, typically in sediment-hosted uranium-bearing deposits
Where rockhounds find bayleyite
Classic worldwide localities
- Hillside mine, about 5.5 km north of Bagdad, Eureka district, Yavapai Co., and in the Cole shaft, Bisbee, Cochise Co., Arizona, USA
- Ambrosia Lake, Grants district, McKinley Co., New Mexico, USA
- Hideout No. 1 (Tiger) mine, Deer Flats, White Canyon district, on the Coral claim, Elk Ridge, at the Mi Vida mine, San Juan Co., and from the Delta Group mine, San Rafael Swell, Emery Co., Utah, USA
- Garfield and Rifle mines, north of Rifle, Garfield Co., from the J.J. mine, Montrose Co., and Schwartzwalder mine, Jefferson Co., Colorado, USA
- Rabbit Lake uranium mine, Saskatchewan, Canada
- Azegour, Morocco
Field-hunting tip
Where it forms: As a coating or efflorescence with other secondary uranium minerals, which may be post-mining, typically in sediment-hosted uranium-bearing deposits. If you start seeing schröckingerite, andersonite, swartzite in float, you are in the right ground. Typical habit: prismatic crystals, drusy crusts, efflorescent coatings. Train your eye for that shape before scanning the outcrop.






