ALX Resources Corp. Intersects Additional Uranium Mineralization at the Gibbons Creek Uranium Project, Athabasca Basin, Saskatchewan

In This Article:

Vancouver, British Columbia--(Newsfile Corp. - April 25, 2024) - ALX Resources Corp. (TSXV: AL) (FSE: 6LLN) (OTC: ALXEF) ("ALX" or the "Company") is pleased to announce the completion of the 2024 winter drilling program at its 100%-owned Gibbons Creek Uranium Project ("Gibbons Creek", or the "Project") located in the northern Athabasca Basin near the community of Stony Rapids, Saskatchewan. The 2024 drilling program was designed to test for continuity of uranium mineralization first discovered in 1979 by Eldorado Nuclear and by ALX in 2015. Five holes totaling 849.44 metres were completed. Four of the five holes intersected uranium mineralization at or near the unconformity, based upon hand-held scintillometer readings on drill core, downhole gamma probe results, and visual observation of uranium minerals by ALX's geological team. Mineralization found in the 2024 drilling was intersected in two areas located 500 metres apart within a target area that ALX defined in late 2023 by carrying out a high-resolution magnetic survey and a Soil Gas Hydrocarbon ("SGH") survey (see ALX news release dated January 23, 2024).

Hole GC24-04 (180 degree azimuth / -60 degree dip) exhibited the strongest radiometric response of the program where uranium mineralization was intersected over 1.1 metres from 107.17 to 108.27 metres beginning immediately at and below the unconformity at 107.18 metres. The Athabasca formation sandstone immediately above the mineralization was strongly bleached from an unaltered dusky maroon colour to white, indicative of hydrothermal activity in the location of the drill hole. A Mount Sopris 2PGA-1000 downhole gamma probe measured a radioactive peak of 8,662 counts per second ("cps") within the mineralized interval (see photo below), which shows black blebs of uranium mineralization (likely pitchblende) within dark red hematite alteration and closely associated with lesser amounts of yellow limonite alteration.

GC24-04: Close-up of uranium mineralization in core sample - peak radioactivity (8,662 cps) at 107.87 m

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/3046/206777_422b56e4b4e8f89b_001full.jpg

The blebs of uranium mineralization appear to follow both the foliation of the rock and to spread along some of the fine fractures. Zones of strong fracturing and fault breccias, variably strongly hematitic (paleoweathered), argillized or chloritized, were intermittently encountered down to approximately 142.0 metres.