Swartzite

swartzite

schrockingerite

bayleyite

andersonite

Images

Formula: CaMg(UO2)(CO3)3.12H2O
Hydrated carbonate, uranyl mineral
Crystal System: Monoclinic
Specific gravity: 2.3 measured, 2.32 calculated
Colour: Bright green, yellowish white (dehydrated)
Luminescence: Fluoresces bright green under short wave UV
Solubility: Soluble in water
Very strongly RADIOACTIVE
Environments

Post-mining efflorescences

Localities

At the type locality, the Hillside Mine, Bozarth Mesa, Bagdad, Eureka Mining District, Yavapai County, Arizona, USA, swartzite occurs as post-mining efflorescences on mine walls, as small vivid green clusters on a layer of snow-white gypsum. Swartzite is a secondary mineral in oxidised portions of the polymetallic sulphide deposit, but the source of uranium is undetermined. Associated minerals include gypsum, schröckingerite, andersonite and bayleyite (HOM, Mindat).

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