Canadian Silver Hunter Inc. plans for work at the Company's wholly owned Lac Lachance property located in the Windfall Lake area of Quebec, near the town of Lebel sur Quevillon. The Company now controls a total of 177 mining claims covering just over 9,900 hectares. CSH is planning to conduct exploration programs on several known showings, including stripping and sampling of outcrop, field mapping and inclusion of that data into the existing exploration model, with the goal of drilling the high-value targets based on the existing data and the 2022 season results.

The Lac Lachance north and south block properties occur within the Urban-Barry greenstone belt located in the Northern Volcanic Zone of the Abitibi geological sub-province. The northern portion of the Lac Lachance claims cover electromagnetic anomalies associated with east-west trending fault zones on the northern limit of the Urban-Barry volcanic belt that hosts numerous gold deposits, including the Osisko Mining Inc., Windfall Lake Gold Deposit. The nearby Windfall deposit is classified as a pre-Temiskaming intrusion-associated gold deposit due to: 1) a temporal and spatial association of gold with felsic calc-alkaline QFP (quartz-feldspar porphyry) intrusions; and 2) the main gold event (i.e., vein- and replacement-type mineralization) being interpreted to pre-date known regional scale deformation.

Gold mineralization is structurally controlled and is hosted in: 1) a series of extensional faults and fractures that are concentrated in areas of contrasting competencies, often located proximal to the contacts between pre-mineral QFPs and host volcanic rocks; 2) along boundaries between flat-lying lithologies and steeper structures; and 3) along boundaries of chemical contrast between ultramafic-mafic and felsic rock types. The mineralization style is variable (i.e., vein- to replacement-type) and is largely dependent on host rock composition.