near Franklin, Spokane County, Washington, USA |
| Ca(UO2)2(PO4)2-10H2O - Typically occurs as dark green compact groups of fan-like crystals to about 3 cm. |
Ca(UO2)2(PO4)2-6-8H2O - Occurs as yellow-green pseudomorphs caused by dehydration of autunite. Many existing collected autunite specimens exhibit meta-autunite rims due to partial dehydration. |
AUTUNITE with META-AUTUNITE |
AUTUNITE with META-AUTUNITE |