Rodgers Cove is situated on the eastern edge of the Dunnage Zone within the Exploits Subzone, an area that forms the Central Newfoundland Gold Belt. The Property straddles both the JBP Fault and the Appleton Fault, which are associated with hydrothermal epigenetic gold veining at high-grade discoveries in the Exploits Subzone. In line with these discoveries is the presence of altered granodiorite-hosted mineralization linked to quartz veining and abundant arsenopyrite.

The property has seen limited exploration conducted historically and has never been drilled. Soil geochemistry, trenching, and limited channel sampling have identified multiple anomalies:

• Target #1: 800 × 600m soil anomaly with up to 758 ppb Au, trench results up to 115.6 g/t Au over 1m.
• Target #2: 400 × 500m anomaly with soils between 50–300 ppb Au, historic showings up to 14.56 g/t Au and 440 g/t Ag.
• Target #3: 100 × 450m anomaly with soils up to 1.78 g/t Au.
• Target #4: Multiple high-grade gold showings, including Rodgers Cove (7.55 g/t Au), Kypher (11.93 g/t Au), and Long Pond (7.16 g/t Au).

*Sorrento has not verified historic work