Lexston Update on Geological Exploration Program on ITZA and 176 Uranium Properties in Nunavut

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VANCOUVER, British Columbia - (NewMediaWire) - October 15, 2024 - Lexston Mining Corporation (the "Company" or "Lexston") (CSE: LEXT) (OTCQB: LEXTF) (Frankfurt: W5G) Lexston Mining Corporation (CSE: LEXT) (OTCQB: LEXTF) (the "Company" or "Lexston") is pleased to provide a project update on the ITZA and 176 Nunavut Uranium properties in Nunavut (the "Project").

Aurora Geoscience geologists completed 7 days of prospecting, mapping and sampling with helicopter access to the Project based out of Baker Lake. The work was completed with two crew, daily field traverses resulted in 75km of prospecting. 5 Areas were prospected and mapped utilizing a RS-125 scintillometer, a total of 113 boulders and 16 outcrops were surveyed. A total of 21 samples were collected and have been submitted to ALS laboratories for Geochemical Analysis these results are still pending. Aurora geologists also provided field-based mapping outlining the extent of Till Veneer and Glaciofluvial deposits which cover >90% of the mapped areas.

Preliminary Results

The recent field reconnaissance program yielded promising results, identifying several key indicators favorable for uranium mineralization. Notably, low-level anomalous readings were detected over a broad area of boulder trains and outcrops using a handheld scintillometer, highlighting potential mineralization zones. Most of the prospective areas (approximately 90-95%) are covered by a thin veneer of glacial till and glaciofluvial deposits, which is consistent with regional patterns and suggests that a potential deposit may be concealed beneath this cover.

Encouraging signs of a broader mineralized system were observed, including strong hematite alteration and with elevated scintillometer readings. These findings, along with historical data, point to the 176-target area as particularly promising, though the central area also shows positive equal signs.

Additionally, historical board spaced geophysics and regional geological mapping have identified significant structural lineaments in the area, intersecting with the unconformity associated with Thelon Basin sandstones. Basement structures known to host uranium-rich hydrothermal convection are present, and the proximity to the unconformity suggests that potential uranium mineralization could be relatively shallow.

Local geophysical anomalies align with the detected low-level uranium anomalism. Given the overlying till veneer, further geophysical investigations are expected to refine our understanding of the structural lineaments and better define the location of the unconformity within the identified anomalous zones.