Terra Clean Energy Corp. Completes First Three Drill Holes on Fraser Lakes

The South Falcon East Project lies 18 km outside the edge of the Athabasca Basin, approximately 50 km east of the Key Lake uranium mill and former mine (Figure 1). The Company entered into an option agreement with Skyharbour Resources Ltd. (“Skyharbour”) in October of 2022 whereby the company can earn up to a 75% interest in the Property.

The Company is currently conducting a 2000-2200 m helicopter supported drill program at the Property. Three diamond drill holes have been completed on the Fraser Lakes B Uranium Deposit, for a total of 802 m. A fourth hole in progress. (Figure 3)

“We are extremely encouraged by the results of the first three drill holes as we continue to see minerlization in each of the first three holes as well as what we believe to be an expansion of the deposit to the North. As stated below, Hole SF063 returned a continuous mineralized zone of pegmatities from 173 meters to 224 meters with some decent grades.” Based on the initial results from Hole SF063 we have decided to reorganize the remaining meters of this program to focus on further defining this new area of interest and chasing clay alteration not yet seen on the property to date, with hopes of finding a high grade unconformity uranium deposit.” said Greg Cameron CEO of the Company.

Hole SF063 was planned to examine an interpreted cross fault offsetting the mineralization and geology on the east end of the Fraser Lakes B Uranium Deposit. This hole was drilled to a depth of 393 meters and intersected multiple structures and a 51 m wide interval of mineralized granitic pegmatites and zones within altered and graphitic pelitic gneiss. Highlights include:

• 0.03% eU over 12.0 m from 173.55 to 185.55 m,

including 0.06% eU3O8 over 0.7 m from 180.35 to 181.05 m

• 0.03% eU over 3.0 m from 213.65 to 216.65 m,

including 0.07% eU3O8 over 0.5 m from 215.95 to 216.45 m

The first structure intersected from 18 m to 47.5m contained zones of intense clay alteration typically found in relation to unconformity uranium deposits. The presence of this alteration is a good indication that hydrothermal fluids suitable for deposition of higher-grade uranium deposits moved through the rocks. The second structure from 306 to 315 m is a brecciated pelitic gneiss situated between two intervals of Archean gneiss. This structure is interpreted to be responsible for the geological offset being targeted. This will assist in updating the target model in this area. The intersections of a clay altered structure and a thick sequence of mineralized pegmatites and pelitic gneiss have expanded the mineralization and improved the…