The Belle occurrence is located on the western slopes of Mount Sicker, north of Nugget Creek.

The area is located within the Cowichan uplift and is underlain mainly by andesitic to rhyolitic tuffs of the McLaughlin Ridge Formation, Sicker Group. The local stratigraphy is disrupted by folding, faulting (pre-Triassic as well as Late Cretaceous) and the intrusions of gabbro and diabase sills and dykes that are coeval with the Upper Triassic Karmutsen Formation. The showing lies about 1 kilometre to the north of the Lenora-Tyee volcanogenic massive sulphide deposit (092B 001) and is of related origin.

In 1897, it was reported that two very large veins 6 to 12 metres in width occur about 30 metres apart in dioritic rock. No work was done on them at that time.

In 1980, Serem Limited drilled four diamond drill holes in order to test a package of variably siliceous schists that originated as tuffs and flows and which are similar in nature to the package hosting the Lenora-Tyee deposit. The schists, locally chlorite and sericite altered, appear to form a south dipping panel having a hanging wall and footwall of gabbro. North of the drill holes there is a transition to andesitic rock.

Pyrite and chalcopyrite occur as disseminations or in association with quartz-calcite veins. It is common to see the sulphides concentrated along the schistosity as fine to coarse grains. In drill hole SRM 18 an average grade of 0.37 per cent copper occurs over 4.6 metres (Assessment Report 8264).

In 2010 and 2011, Rock-Con Resources completed a program of prospecting and rock sampling on the Mount Sicker property.