Rameauite is a hydrated complex uranyl oxide mineral with formula K<sub>2</sub>Ca(UO<sub>2</sub>)<sub>6</sub>(OH)<sub>16</sub>÷H<sub>2</sub>O or K<sub>2</sub>CaU<sup>6+</sup><sub>6</sub>O<sub>20</sub>÷9H<sub>2</sub>O.
Rameauite has four observed forms which are {010}, {100}, {001} and {110}. The angles between these faces are {100}^{001} = 58ð40' and {010}^{110} = 49ð 50'. The crystals are always twinned on {100} and they are flattened parallel to {010}, and elongated parallel to {001}. The mineral rameauite is an example of a monoclinic mineral and appears pseudo-hexagonal. I has unit cell dimensions of: a= 13.97, b= 14.26, c= 14.22 with ò = 121.02ð.
It was first described in 1972 for an occurrence in the Margnac Mine, Compreignac, Haute-Vienne, Limousin, France and named after Jacques Rameau (1926âÂÂ1960), French prospector at the "Commissariat àl'Energie Atomique", who discovered the deposit where the mineral occurs. In addition to the type locality in France it has been reported from the Orphan Mine on the south rim of the Grand Canyon in Arizona and on Rhyolite Ridge, Esmeralda County, Nevada.