The Cherry occurrence is located south of Cherry Ridge about 76 kilometres east of Lumby.
The area is underlain by sedimentary and volcanic rocks of the Upper Triassic to Lower Jurassic Nicola Group. These comprise basic lavas and pyroclastics and sedimentary rocks including argillite and some limestones.
A copper occurrence of unknown type is noted on Geological Survey of Canada Open File 637 (#288). No other information is available.