Property Geology
The Copper Mountain Project area is underlain by Archaean rocks of the Wyoming Province and overlain in the southern part by Cainozoic sedimentary rocks.
Two phases of pegmatites are recognised, an early granitic pegmatite suite concordant with the schistose fabric which are not known to contain economic mineralisation and younger discordant pegmatite dike suite. This younger discordant suite contains economic minerals including lithium, tantalum and niobium bearing phases.
