The Bell showing is located about 26 kilometres southeast of Dease Lake.

The showing occurs in an area mapped as Middle Triassic rocks of the Stuhini Group. These include augite porphyry, meta-andesite, metabasalt, volcanic breccia and possibly some sedimentary rock. The southern portion of the property is adjacent to quartz monzonite of the Middle Jurassic Three Sisters Plutonic Suite. Several major north-trending faults are evident in the area.

Magnetite is reported in all the volcanics and in places is accompanied by strong concentrations of disseminated chalcopyrite. Mineralization type is assumed to be copper skarn similar to the Crown showing (104I 046) located 5 kilometres west.

In 1971, Chapparal Mines Ltd. conducted magnetometer and induced polarization surveys, collected soil samples and completed two diamond-drill holes totalling 160 metres. No other work is reported.

In 1989, Equity Silver prospected and sampled the area. This work identified two separate localities, approximately 400 metres apart, of dacite and weakly carbonate-altered andesite. The dacite contained no visible sulphides and has limonite on its weathered surfaces. Epidote, pyrite and malachite are present on fracture surfaces in the altered andesite. Two select grab samples yielded values of 0.232 and 1.299 per cent copper, respectively (Assessment Report 19177).

In 2011, Finsbury Exploration Ltd carried out exploration over the Property as part of a soil and silt sampling program over a much larger 168,983 hectare property area known as the Galaxie property.

In 2012, Quartz Mountain Resources Ltd, on the Galaxie property, conducted systematic soil and IP surveys over eight high-priority grids and two target areas identified by the 2011 stream sediment and soil geochemical results. This work included an IP survey over almost the entirety of title 512878 and the southeastern third of title 604847.