South of Horsefly, the Upper Triassic to Lower Jurassic rocks of the Central Quesnel Belt have been intruded by the Lower Jurassic Takomkane batholith. The Takomkane batholith is of quartz monzonite to granodioritic composition. South of Murphy Lake the batholith is overlain by remnants of the Eocene Kamloops Group sedimentary and volcanic rocks.

The SL showing comprises minor amounts of chalcopyrite within the Takomkane batholith. The overlying Kamloops Group sediments include thin coal seams.

Work History

GWR Resources completed programs of prospecting, geochemical sampling, geological mapping and geophysical surveys on the area during the 1990s through 2013.

During 2018 through 2021, EnGold Mines Ltd. completed programs of prospecting, soil sampling, diamond drilling and a geophysical survey on the area as part of the Lac La Hache property.