The B & B quartzite occurrence is situated 5 kilometres east of Remac, west of Creggan Creek near Nelway.
The quarry is reported to be developed in Lower Cambrian quartzite (Exploration in B.C 1978), presumably of the Quartzite Range Formation. However, Geological Survey of Canada Open File 1195 shows the area to be underlain entirely by carbonates of the Middle Cambrian Nelway Formation.
A total of 360 tonnes of quartzite were produced for facing stone, ashlar and flagstone by T. Brown of Salmo in 1978.