Bayleyite sample from the Ambrosia Lake area, Grants District, New Mexico (size: 4.6 x 2.4 x 1.6 cm)
|Crystal class||Prismatic (2/m)
(same H-M symbol)
|Unit cell||a = 26.65 Å, b = 15.31 Å,
c = 6.53 Å; β = 93.07°; Z = 4
|Crystal habit||Clusters of prismatic crystals, crusts|
|Mohs scale hardness||2 - 2.5|
|Optical properties||Biaxial (-)|
|Refractive index||nα = 1.453 - 1.455 nβ = 1.490 - 1.492 nγ = 1.498 - 1.502|
|Birefringence||δ = 0.045 - 0.047|
|Pleochroism||Visible: X = Pinkish, Y = Light yellow, Z = Light yellow|
|2V angle||Measured: 30°|
|Ultraviolet fluorescence||Weak; yellow-green to pale greenish under LW and SW|
Bayleyite is an uranium carbonate mineral with the chemical formula: Mg2(UO2)(CO3)3·18(H2O). It is a secondary mineral which contains magnesium, uranium and carbon. It is a bright yellow color. Its crystal habit is acicular but is more commonly found as crusts on uranium bearing ores. It has a Mohs hardness of about 2-2.5.
It was first described in 1948 for an occurrence in the Hillside mine, north of Bagdad, Yavapai County, Arizona and named for mineralogist William Shirley Bayley (1861–1943) of the University of Illinois. It occurs as an efflorescence or coating on other secondary minerals and often is deposited on mine walls and workings. It occurs with schrockingerite, andersonite, swartzite and gypsum in the Hillside mine; with schrockingerite and gypsum in the Hideout mine in Utah; and with tyuyamunite, uranophane, liebigite and carnotite in the Powder River Basin in Wyoming.
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