May Lake Property,
Saskatchewan
The May Lake Property encompasses 5,487 ha (13,558 acres) within the northern parts of the LaRonge Greenstone Belt, north-central Saskatchewan. Despite being one of the larger Greenstone Belt’s within Canada, it remains underexplored.

Project Highlights
- LaRonge Greenstone Belt is vastly underexplored
- Historic gold showings
- 2016 boulder samples assayed at 1.15 g/t Au (4.14% Cu) and 1.30 g/t Au (7.51% Cu)
- The region has demonstrated potential for multiple high-grade, gold occurrences and deposits
LaRonge Domain (Gold Deposits)
- LaRonge Greenstone Belt with 160km strike length
- Historic gold grades comparable to other Canadian Greenstone belts
- Good access along all-season Hwy 102
- Limited historic exploration (vastly underexplored)

May Lake Property
- Four mineral claims, 5,487 ha
- Less than 5km from Hwy 102
- The mineralization, encountered by hole DDH MAY-4, consists of disseminated to semi-massive pyrrhotite and pyrite with minor associated chalcopyrite and sphalerite. The mineralization is hosted by a green, variety graphitic, cherty volcanic exhalitive horizon
- Hole DDH MAY-4:
- 6.82 g/t Au, 2.86 g/t Ag and 2.10% Cu over 4.96m
- Hole DDH MAY(NE)-9:
- 4.31 g/t Ag, 0.54% Cu, 0.53% Zn over 6.79m

May Lake Property, Saskatchewan
- Hole DDH MAY-4:
- 6.82 g/t Au, 2.86 g/t Ag and 2.10% Cu over 4.96m
- Hole DDH 9, 10, 35 and 36 with highly anomalous geochemistry, up to 9.72% Cu, 2.35% Zinc, 4.31 g/t Ag
- 2016 Samples
- Rock samples up tp 1.30 g/t Au, 7.51% Cu, 1.25% Zn
- Soil samples up to 23.60 ppb Au, 470 ppm Cu

Summary
- Less than 5km from Hwy 102, access via easily re-activated historic drill roads
- The May Lake Property covers a sulphide-rich VHMS deposit with potential for significant tonnages of Au, Cuand Zn. Anomalous values have been obtained from both historic drilling and sampling.
- Regional exploration data suggests the May Lake Property exhibits several key elements that are fundamental to exhalative VHMS gold mineralization, such as a cherty exhalitehorizon hosting significant sulphides, surrounding felsic-dominated volcanics and two mapped eruptive centres.
- The mineralized zones encountered by historic drillholes consisted of disseminated to semi-massive pyrrhotiteand pyrite with minor associated chalcopyrite and sphalerite.