LIDSTONE GOLD PROJECT

Located ~240km northwest of Geraldton, ON
Within the English River Basin proximal to the southern contact of the Uchi Domain of the Superior geological province
Network of logging roads allows the property access from the west via a truck and from the east via a truck and on foot (approx. 1.5km)
16,238 ha of mining claims, 100% owned, no royalties
Completed 2 field exploration geochemical programs
Quartz vein assays returned 2.34g/t Au (Feb 3, 2026) and 0.272 g/t Au (Mar. 2025)
Easy access due to extensive network of logging roads
Exploration to follow up on gold mineralization prospectivity in the 2026 field season

Lidstone is located on the boundary of the metasedimentary dominated English River Basin with the greenstone and plutonic complexes of the Uchi Domain
Lithologies consist of metasedimentary units, migmatized supracrustal rocks, mafic to intermediate greenstone belt of basaltic/andesitic flows, tuffs and breccias
Massive to foliated late stage tonalite – granodiorite – monzodiorite suites occur on the northern sections

The prospect area consist of coincident magnetic abrupt highs and lows and zones of high electromagnetic (EM) conductance
Multiple areas of interest suggests historical work overlooked a significant exploration opportunity in the prospect area
The area shows shear strike that extends north-west through the central part of the prospect with the magnetic high defining the mafic and tonalite units which show high potential magnetic / iron signatures that can be part of a catalyst for Ni-Cu-PGE deposition
Magnetic data in combination with lithology from historical drilling demonstrates potential scale and prospectivity for a near surface mineralization

In the 2024 field exploration on the project showed potential for gold mineralization with a sample from a quartz vein returning 0.272 g/t Au
The surrounding geology was further investigated for potential economic gold mineralization in the fall of 2025
The 2025 sampling campaign was conducted over ten days in November 2025. A total of 229 samples were collected, representing 102 quartz veins, 112 metavolcanic-metasedimentary rocks, 7 granitic rocks, and 8 mafic-ultramafic intrusive rocks
Extensive sampling was carried out along the margins of an interpreted granite-greenstone belt contact which is strongly delineated in the regional magnetic survey
Out of 225 samples twelve samples assayed returned anomalous gold between 0.01-0.05 g/t Au and one sample (F570631) returned 2.34 g/t Au