Hawkmoon Resources Corp. announced that it has received assay results for the final five drill holes (the “Holes”) from its 2022 10-hole drill program (the “Program”) on the Wilson Gold project (“Wilson” or the “Property”). The Property is situated approximately 15 kilometres east of the town of Lebel-sur-Quévillon, Québec and 170 kilometres northeast of the city of Val-d'Or, Quebec in the Abitibi Greenstone Belt.

164 holes have been drilled on the Property between 1956 and the date of this news release. This drilling has defined three significant mineralized areas on the Property: the Toussaint, Central, and Midrim Zones. Notable pierce points by drill holes are shown in grey circles.

Mineralization at Wilson is present where a volcanic tuff comes into contact with an intrusion. These intrusions are primarily gabbro in composition. The most prospective areas of the Property are along the contacts between volcanic tuffs and intrusions.

The rocks at Wilson dip sub-vertically. The Holes intercepted mineralization typical of Wilson. This mineralization is characterized as a beige to pale grey coloured volcanic tuff which has been strongly foliated, sheared, fractured and altered.

The mineralization is associated with strong silica, sericite and calcite alteration. Ankerite and chlorite alteration are present to a lesser degree. Quartz veins and veinlets are commonly observed in the mineralized zones.

Pyrite is the dominant sulphide mineral.