Bergenite
A variety of Minerals

What is Bergenite?
Bergenite is a rare uranyl phosphate of the more specific phosphuranylite group. The phosphuranylite-type sheet in bergenite is a new isomer of the group, with the uranyl phosphate tetrahedra varying in an up-up-down, same-same-opposite (uuduudSSOSSO) orientation. All bergenite samples have been found in old mine dump sites. Uranyl minerals are a large constituent of uranium deposits. The phosphuranylites are one of the two major groups of the uranyl series, and are the most extensive of the uranium minerals. Uranyl phosphates include 45 different minerals, at least 16 of which belong to the phosphuranylite type topology, including dumontite, vanmeersscheite, upalite, and the most characteristic, phosphuranylite. As explained by Frost et al., the uranyl phosphates display diverse chemical and structural features, which often exhibit the geochemical conditions present during formation.
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Bergenite Localities Map
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Key Characteristics
Characteristics of Bergenite
Bergenite forms as a dark yellow crust with well-developed, small thin needle-like crystals. An original description of bergenite is the orthorhombic symmetry and a density greater than 4.1 g/cm.
Quick Facts
Physical Properties
- Color
- Yellow
- Density
- 4.82 g/cm³
Chemical Properties
- Chemical Formula
- Ca2Ba4(UO2)9(PO4)6O6 · 16H2O
- Elements
- Ba, Ca, H, O, P, U

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