The HS-19 occurrence is located at an elevation of approximately 2120 metres on the south side of a ridge separating lakes at the head of Walsh and Manchester creeks.

The area is underlain by sedimentary rocks of the middle Creston Formation intruded at their (faulted) contact with Kitchener Formation by diorite sills of the Moyie Intrusions; all these units belong to the mid-Proterozoic Purcell Supergroup.

Locally, thin bedding-parallel quartz veins, up to 2 centimetres wide, host limonite and gold values. The veins trend 020 degrees and dip 38 degrees west.

In 2002, a rock sample (HS-19) assayed 1.83 grams per tonne gold (Assessment Report 27025).

During 2000 through 2002, National Gold Corporation completed programs of geological mapping and silt, soil and rock sampling on the area as the HS and Zinger claims. In 2003, Chapleau Resources conducted an extensive exploration program of surface prospecting, rock and soil sampling and geological mapping on the area as the Zinger property.