Announcement • Jul 08

Blast Resources Inc. Announces Structural Corridor At Wales Lake Project

Blast Resources Inc. has announced a structural corridor found on the Blast mineral claims. The Company has 3 claim groups on the southwest side of the Athabasca Basin in northern Saskatchewan. Low magnetic susceptibility in regional surveys shows a NE-SW structural corridor that crosses the Blast claims for 9 km. The feature may be caused by alteration and destruction of magnetic minerals. The significance of a structural corridor zone is that it may host concentrations of uranium mineralization in individual or multiple shears or faults to hundreds of metre depths. This structural corridor is a zone of approximately parallel faults or shears in basement rock. The trend extends both NNW (330°) and SSE (150°) of the Blast claims continuous within the Blast claims for a length of 9 km. Width of the zone as indicated by basement conductors (Fission 3) may be 3 km. Info on this target are as a result of the December 2024 airborne magnetic survey done by the Company and historic F3 Uranium field work (public domain). In structural geology, a structural corridor refers to a long, relatively narrow area defined by specific geological structures, such as faults, shears or folds, which can influence the location of geological features and resources. The Athabasca Basin's structural corridors are critical for understanding the sites of uranium mineralization, particularly the relationship to unconformity-related deposits. These corridors, often major fault zones, act as pathways for uranium-bearing fluids and provide geometric traps for ore deposition. The Company is focussed on conductors in basement rock that acted as traps for uranium mineralization. Unconformity-related deposits, uranium mineralization is often associated with the unconformity surface, where older basement rocks are overlain by younger sedimentary rocks. Conductors in the basement rocks can guide fluids from deeper sources to the unconformity, where they can deposit uranium. The Wales Lake project is accessible along the all-weather gravel road provincial highway 955 from La Loche to the past-producing Cluff Lake uranium mine. Highway 955 crosses approximately 1.5km to the east of the project, and access to the west may be on ungazetted bush roads and tracks. The scientific and technical information contained in this news release was prepared and approved by Locke Goldsmith, M.Sc., P.Eng., P. Geo., Arctex Engineering Services and who is a Qualified Person as defined by National Instrument 43-101 - Standards of Disclosure for Mineral Projects. Situated south of Wales Lake and positioned just outside the southwest margin of the Athabasca Basin, the Project is strategically located within the Patterson Lake Corridor which hosts two significant uranium deposits (Triple R Deposit, 2,200,000 @ 1.58 U308 and 0.51 g/t Au & the Arrow Deposit which is the largest source of low-cost uranium globally, delivering up to 30,000,000 pounds of high-grade uranium per year). The deposits represent one of the largest high-grade uranium systems globally, comparable to world-class deposits such as McArthur River, Cigar Lake, and Key Lake.

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