The Palmer River rises in the Windsor Tablelands area of the Paleozoic Hodgkinson Basin, 110 kilometres northwest of Cairns. It flows west across the Palmerville Fault and Proterozoic Dargalong Metamorphics to the Mitchell River._x000D_
East of the Palmerville Fault, its course lies immediately south of the onlapping Mesozoic Laura Basin conglomerates, sandstones and siltstones._x000D_
Gold occurs in quartz reefs in the Hodgkinson rocks of the Maytown District, in narrow quartz veins in the Dargalong Metamorphics, in the basal conglomerates of the Mesozoic, and more importantly, in alluvial bars within the Palmer River.