E2Gold Inc. geologists have discovered mineralized McKinnon-like rocks in outcrops along 2.5 km, east of the McKinnon Zone. Early assay results of up to 2 Au g/t indicates the gold-bearing zone continues eastward beyond the current McKinnon Resource. In the KB claims, geologic mapping and prospecting have identified multiple gossan and sulphide-bearing outcrops tracing for almost 500 m from east to west, still open at either end, ranging from 15 m to 50 m width.

Located 4 km to the west of Goldfields, this represents a potential significant new target at the Hawkins project. Gossan is a product of weathered sulphides and is a common indicator of potential gold or base metal mineralization. The continuity and significant width of the occurrence is a good indication of a large footprint.

Major deposits such as the Borden Lake deposit, for example, was recognized from a single outcrop of gossan. During this year's expanded surface program geologists noted higher concentrations of quartz-carbonate veins, as well as chlorite and limonite, in the western part of the property, where the gossanous shear zones occur. These minerals are suggestive of regional hydrothermal fluid flow, which along with deformation, is an environment favourable to finding gold and base metal deposits.