Hertz Energy Provides Corporate Update and Announces Option Grants

In This Article:

Vancouver, British Columbia--(Newsfile Corp. - August 30, 2024) - Hertz Energy Inc. (CSE: HZ) (OTCQB: HZLIF) (FSE: QE2) (the "Company" or "Hertz") is pleased to provide the following corporate updates.

SNAKE AND AC/DC LITHIUM PROJECTS, JAMES BAY REGION, QUEBEC:

Field activities at the Company's Snake Lithium Project were conducted between June 17 to June 26th, 2024, targeting pegmatitic dykes, known mineral occurrences, and areas with the potential for spodumene mineralization. Access to the project site was facilitated by an AS350BA+ helicopter provided and piloted by Panorama Helicopters, complemented by extensive ground hiking. The exploration team completed nineteen traverses across prospective zones within the project boundaries, documenting a total of 389 observations and collecting 95 samples-77 for lithium and 18 for gold.

The most commonly encountered geological unit was migmatite, derived from paragneiss with granitic and pegmatitic leucosome. All pegmatitic rocks, quartz veins and sulphide-bearing lithologies encountered during the 2024 exploration phase were sampled. No lithium and/or gold-associated minerals were documented throughout the traverses. Data interpretation is still ongoing, and no anomalies have been observed at this time.

Field activities at the Company's AC/DC Lithium Project commenced after the Snake field program and ended on July 28, 2024. A total of 171 observations points and 81 samples were collected along several traverses with assay results still pending and data interpretation still ongoing.

HERTZ ENERGY NAMIBIA URANIUM PROJECT:

Hertz Energy has submitted applications EPL-10185 and EPL-10186 for Exclusive Prospecting Licenses (EPLs) in Namibia. See News Release May 3, 2024.The Company anticipates receiving these licenses in the next few months and will provide clarity as more information is provided.

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-Rössing Formation boundary, or, where the Rössing 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.