WestKam Reports on Winter Phase at Bonaparte

VANCOUVER, BRITISH COLUMBIA--(Marketwired - Dec 30, 2016) - WestKam Gold Corp. (TSX VENTURE:WKG) (the "Company" or "WestKam") WestKam Gold Corp announced today that the bulk sample program at the Bonaparte Gold Project, managed and conducted by MX Gold Corp. until December 31, 2016, is continuing. MX Gold is incurring a minimum $650,000 in exploration expenditures at Bonaparte by December 31, 2016, to earn a 5% interest in the property (as announced December 28, 2016 and with an effective date of December 16, 2016).

The current position of the decline is at 229.76m, approximately 118.1m from the Bulk Sample target zone. The Bulk Sample target zone encompasses the Grey Jay, Crow, Owl and Nutcracker vein structures which occur over a combined width of approximately 20 metres and are partially located beneath the flooded pits resulting from the 1994 and 2010 bulk sample programs. The structures hosting the aforementioned veins trend near north-south from 023° to 034° azimuth with easterly trending dips from 45° to 55° east. It is estimated that the Bulk Sample zone will be reached in approximately eight weeks once underground operations resume.

Raven Vein

The current face of the underground decline has crosscut the down dip extension of the Raven Vein structure at or before its targeted intersection. The Raven vein structure consists of two widely spaced vein sets. The first quartz vein intersected in the decline trends at 033° dipping 38° to the east. The exposed quartz vein is 0.5m wide hosting 1-2% pyrite. Chlorite, quartz carbonate alteration envelopes are noted on the footwall and hangingwall sides of the vein over widths of 0.3m and 0.5m respectively. The Raven vein proper was intersected a further 7m down the decline to the west. Its orientation varies from 005°-35° to 035°-45°. The bull quartz vein is 0.5m thick hosting disseminated pyrite mineralization from 3%-5%. Chlorite, biotite, pyrite alteration zones are noted on the footwall and hangingwall sides of the vein over widths varying from 0.3m to 1.0m. Elevated pyrite is well noted in both the hanging wall and footwall alteration zones as disseminations and blebs from 20% to 30% pyrite. Approximately 1.5m east on the hanging wall side of the Raven Vein is an interval of strong quartz carbonate and chlorite +/- biotite alteration varying from 0.3m to 0.5m wide hosting 20% to 30% disseminated Pyrite.

The portal entrance was initially developed on the Raven vein during the initial phase of the underground bulk sampling program in December 2009. The Vein was first encountered 12.07m down the decline from the portal entrance which continued in a southerly direction along the decline to a point where the vein changed strike direction to 230° azimuth, after which the decline heading turned to the east. The Raven vein near the portal entrance dips from 40° to 45° east and was traced along strike down the decline over a distance of 41.24m; 23 panel sample results from the vein reported from the original sampling program returned an average grade of 12.6g/t gold over a distance of 38.2m. Individual panel samples from the vein report grades varying from 0.74g/t Au over 0.83m to 69.2g/t Au over 1.26m. The Raven vein varies in width along strike from 0.3m to 1.26m hosting scattered irregular clusters of semi massive sulphides comprising pyrite, pyrrhotite and chalcopyrite.