Company: LINMF
Filing Date: 2025-08-01
Form Type: 20-F
Source: 0001176256-25-000065
Chunk: 29

Company: Linear Minerals Corp
Filing Date: 2025-08-01
Form: 20-F
Item: Item 4
Chunk 29
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 description and location

The Kokanee Creek Gold Property consists of 3 claims covering approximately 1,000 hectares area in Nelson Mining Division in British Columbia, Canada. It is located 18 km to the east of Nelson on NTS map 082F055. The property is part of a very active mining area with several historical and current gold, silver and base metals deposits located in the region. Nelson is a historical mining town dating back to the discovery of Toad Mountain Silver deposit in 1886.
Ownership

The Company acquired a 100% interest in the Kokanee Creek Property in 2022 by completing an aggregate of $45,500 in option payments and 1,388,158 in common share issuances.

The Property is subject to a 2.0% NSR royalty of which the Company will have the option to reduce the NSR by 1.0% by paying $1,000,000.

During the year ended March 2025, the Company wrote-off all deferred costs to date as the company does not plan to do further work on the property.

20

<{self.tag} alt="{self.alt}" src="{self.src}">Property Location Map

Geology

Geologically the property area is underlain by Slocan Group basal slates and phyllites with lesser fine-grained quartzite and limestone beds are overlain by well-bedded, arenaceous quartzite argillites with local impure quartzite and limestone. The top of the argillite section is marked by tuffaceous lava beds, likely related to early Rossland Group volcanism. Jurassic Nelson intrusives consist of porphyritic granite, granodiorite, diorite, quartz diorite, monzonite and hornblende syenite. Several smaller alkaline plugs belong to the Tertiary (Eocene) Coryell Batholith.

The claim area is underlain by a metasedimentary roof pendant remnant within the Middle Jurassic Nelson Batholith. The roof pendant is predominantly composed of argillic siltstone (siltite) and biotite schist mixed with Nelson paragneiss. Siltstones are exposed along the Lower Kokanee Creek Road and the Upper Busk Creek Road. Large rusty quartz veins intrude host sedimentary rocks. Some of the veins contain muscovite and form minor stockworks. Sulphide mineralization on the property includes coarse-grained euhedral galena, coarse-grained euhedral pyrite cubes and