Lucky Strike is located within the western Abitibi Greenstone Belt whose rocks have undergone a complex sequence of deformation events ranging from early folding and faulting to ductile shearing resulting in the development of two long 250-350 km ,  east-west trending, steeply dipping crustal deformation corridors also known as “breaks”. These are known as  the  Destor-Porcupine Deformation Zone  and the Larder Lake-Cadillac Deformation Zone (LLDCZ), which lies approximately 5 kms to the south of the southern-most boundary of the Lucky Strike Project. These two deep-seated crustal breaks are responsible for the major gold camps that stretch across much of Ontario and Quebec.

Two regional structures, the Misema-Mist Lake Fault, and the Mulven-Kinabik Lake Fault transect the Lucky Strike Project in an east-northeast orientation. The Misema-Mist Lake Fault and the Mulven-Kinabik Lake Fault are speculated to be the continuation of the Kirkland Lake Main Break which hosts seven historic gold mines of the Kirkland Lake Gold Camp approximately 16km to the west-southwest of the western-most boundary of the Project. Past gold production in the Kirkland-Larder Lake area has exceeded 50 million ounces. The Kirkland Lake Main Break itself is considered a splay structure off the LLDCZ. The Lucky Strike Project hosts ~19km of strike length of the Mulven-Kinabik Lake Fault and ~10km of strike length of the Misema-Mist Lake Fault and considered prime targets for future exploration efforts on the Project.

The Project area is underlain by a succession of Archean volcanic and volcaniclastic rocks of the Blake River assemblages and later intrusives and dikes:

• 70% - Upper Blake River: 2701- 2696 Ma; Felsic to intermediate metavolcanic calc-alkaline basaltic, dacitic, and andesitic flows, tuffs, and breccias with some areas underlain by bimodal tholeiitic basalt and rhyolite. Mostly covering the north and east of the Project.

• 20% - Lower Blake River: 2704-2701 Ma, Tholeiitic mafic to intermediate metavolcanics with lesser amounts felsic volcanic rocks and turbiditic sedimentary rocks. Basaltic and andesitic flows, tuffs, breccias, chert, iron formation, minor metasedimentary and intrusive rocks and related migmatites. Mostly covering the southwest portion of the Project.

• 5% - Mafic and Ultramafic Intrusives; Gabbro, anorthosite, and ultramafic intrusive rocks. Mostly contained within the Upper Blake River assemblage or at the contact with the Lower Blake River.

• 4% - Timiskaming: 2676-2670 Ma; Syenite Intrusives +/- Porphyry: Diorite-Monzodiorite-Granodiorite Suite (saturated to oversaturated). Diorite, quartz diorite, minor tonalite, monzonite, granodiorite, syenite, mafic syenite and hypabyssal equivalents.

• <1% - Matachewan Mafic Dikes (2454 Ma) and Sudbury Diabase Dikes (1235-1238 Ma): Youngest rocks exposed on the property striking north-northwest utilizing major structural contact boundaries and faults.

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Gold mineralization occurs in several localities throughout the Project. Gold can occur in veins within intrusive rocks proximal to the major faults and/or deformation zones. This type of mineralization is commonly associated with Cu-Pb-Zn and can occur in several closely spaced veins (Walsh and Norwood). Gold can also occur in intensely deformed rocks (shear zones) within structural “breaks” up to tens of metres thick (Labyrinth) and associated with strong iron-carbonate, sericite, quartz and pyrite.

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Known Areas of Interest on the property include: