Hertz Energy Submits Applications to Acquire Uranium Focused Claims in Namibia

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Vancouver, British Columbia--(Newsfile Corp. - May 3, 2024) - Hertz Energy Inc. (CSE: HZ) (OTCQB: HZLIF) (FSE: QE2) (the "Company") is pleased to announce that is has submitted applications for uranium Exclusive Prospecting Licenses (EPLs) in Namibia.

Namibia is a country of diverse geology and has one of the richest uranium mineral reserves in the world. There are currently two large operating mines, the Husab and Rossing mines, in the Erongo Region and five major exploration projects planned to advance to production in the next few years as the country embraces the green energy transition. Uranium mining in Namibia is of considerable importance to the national economy1. In 2023, Namibia produced the 3rd largest quantity of uranium worldwide at 6,382 tonnes, ranked only behind Kazakhstan and Australia2.

Namibia is a premier operational uranium jurisdiction with a 45-year history of safe uranium production and exportation3. It possesses excellent utilities, transportation, and exportation infrastructure as well as established support for uranium mining from both the Namibian Government and local communities. Namibia enjoys a combination of political stability, security, a strong rule of law and an assertive development agenda. In 2023, mining contributed approximately 12% of Namibia's GDP and employs approximately 16,000 people4.

Hertz Energy Namibia Uranium Project

The application areas cover an area of 9,627.84 hectares located in Central Namibia in the Erongo Region which hosts numerous primary and secondary uranium deposits. Primary economic uranium is hosted mainly in sheeted D-type alaskites which occur both as cross-cutting dykes and as bedding and/or foliation-parallel sills. The sheets can amalgamate to form larger granite plutons or granite stockworks made up of closely spaced dykes and sills. The mineralized alaskites tend to occur at marked stratigraphic levels, often associated with the Khan-R?ssing Formation boundary, or, where the R?ssing Formation is missing, the Khan-Chuos/Arandis Formation boundary. Secondary uranium deposits occur in calcretes in the coastal plain of the Namib Desert. The deposits are associated with ancient river systems that flowed westward from the Great Escarpment during the upper Cretaceous and lower Cenozoic periods. Uranium mineralization is typically located in calcretised fluvial channels which tend to be buried with little or no obvious surface expression to identify them.

Figure 1: Licence applications in the Erongo Uranium Province of Namibia.

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