The Site 812 occurrence is located on a ridge to the north of Hardscrabble Creek, approximately 2.7 kilometres west of the Skeena River.

The area is underlain by a sequence of volcanic and sedimentary rocks that have been mapped as Early Jurassic Hazelton Group or more recently as Early Jurassic Kitselas volcanics. The Kitselas volcanics are predominantly of felsic composition. These have been intruded by granites, granodiorites and diorites of the Eocene Carpenter Creek pluton.

Locally, a zone of quartz veins with fracture filling chalcopyrite-magnetite-pyrite mineralization and malachite alteration are hosted in greenstones.

In 2010, three rock samples (2922, 2923 and 2934) yielded values ranging from 0.044 to 2.740 grams per tonne gold, 58.0 to 58.8 grams per tonne silver and greater than 1.0 per cent copper (Assessment Report 32186).

In 2002, the Carlson group of mineral claims was staked by G.W. Kurz. During 2003 through 2014, various programs of bedrock prospecting, rock chip sampling, geological mapping, a ground self-potential geophysical survey and geochemical soil and silt sampling were completed.