The BLUEBELL II showing is located approximately 8 kilometres northwest of Peachland.

The showing occurs in quartzite of the Triassic-Jurassic Nicola Group which is underlain by diorite and granodiorite of the Early Jurassic Pennask Batholith.

Workings on the showing include 3 old pits dug in highly oxidized zones exposing greenish and brownish quartzites. In the northernmost pit there is a 4 to 5 centimetre thick shear zone. Grains and masses of pyrite are present in the zone and are sparsely disseminated through the adjacent fractured wallrock. A few grains of galena and sphalerite have been noted in some spots. Minor irregular zones of fracturing and iron oxide staining are locally exposed around the area of the showing.

In 1964, two short holes were drilled by Quinalta Petroleums Ltd. of Calgary. The results of this program are unknown. In 1965, the showing, along with the CAP (082ENW026) showing to the southwest, was examined by Western Resources Consultants Ltd. and an access road constructed. In 1972, Canadian Johns-Manville Company Limited carried out geological mapping, magnetometer surveys and geochemical surveys. They concluded that the mineralized zones, primarily those of the CAP showing to the southwest, were too small and lenticular to be considered economic.