The Black Devil occurrence is located on a south facing slope, northeast of McIntyre Creek and approximately 1.7 kilometres northeast of its junction with the Kettle River.

The area is underlain by granite and granodiorite of the Jurassic Nelson Plutonic suite.

Locally, thin quartz veins with sericite-limonite and pyrite are hosted by a fractured and argillic-altered granodiorite.

In 2009, a rock sample (SK09-164) assayed 2.49 grams per tonne gold (Assessment Report 31195).

During 2007 through 2009, Kootenay Gold completed programs of prospecting and geochemical sampling the area immediately north and west as the Devil property.