Bayridge Resources Receives Constellation Level 2 Exploration Permit for Drilling

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Vancouver, British Columbia--(Newsfile Corp. - January 29, 2025) - Bayridge Resources Corp. (CSE: BYRG) (OTCQB: BYRRF) (FSE: O0K) ("Bayridge" or the "Company") is pleased to announce that it has received the Level 2 Exploration Permit for drilling at its 11,142 ha Constellation uranium project in Canada's Athabasca Basin region.

The Company is permitted for up to 30 drill sites that can total of up to 10,000 metres of diamond drilling within an 18 month period, that the Company will commence with a Phase 1. In addition, a total of 40-line kilometres of grid line cutting in preparation for ground geophysical surveys have also been permitted. The Company also reports it has received the 2024 Phase I exploration assay results. They will be released as soon as the technical team has reviewed and completed QA/QC procedures in respect of the results.

"The drilling permit is the next milestone in the exploration and development of the Constellation project," commented President and CEO Saf Dhillon. "The receipt of this drill permit puts us right on schedule for a late Q1 early Q2 maiden drill program of which, Phase 1 is already fully funded," he continued.

The Phase I exploration program was successful in highlighting several areas of anomalous spectrometer count-per-second anomalies, several of which were associated with the VTEM (versatile time-domain electromagnetic) conductors identified from the Geotech VTEM survey flown earlier in the summer. A total of 15 spot radiometric anomalies or anomalous zones were identified, largely associated with VTEM conductors or the boundaries of magnetic highs and magnetic lows, areas believed to be prospective for uranium mineralization (as shown in Figure 1).

Figure 1 Constellation Project Spectrometer Anomalies
(Readings in CPS or counts per second)

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The Constellation property has favourable geology for basement-hosted unconformity-style uranium deposits. The regional geology and magnetics have defined structural lineaments trending NNW and ESE, which could represent structural conduits between the Archean granite inlier and graphitic metasediments that have been mapped on the property. These types of structural zones typically function as pathways for hydrothermal activity. Historical NE-trending conductors have also been outlined on the property but are under-explored and un-drilled. Strong EM conductors are proven targets associated with unconformity and basement-hosted uranium mineralization in and around the Athabasca Basin.1