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Hertz Energy Acquires Lake George Antimony Property in New Brunswick

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Vancouver, British Columbia--(Newsfile Corp. - September 16, 2024) - Hertz Energy Inc. (CSE: HZ) (OTCQB: HZLIF) (FSE: QX1) ("Hertz" or the "Company") is pleased to announce the acquisition of the Lake George Antimony Property ("Lake George" or the "Property") located in the Province of New Brunswick. The Property is located in the southwestern part of the province, approximately 30 km southwest of the city of Fredericton.

The Property is comprised of 93 mineral claims within two claim blocks recently staked by the Company for a total area of approximately 2,104.5 hectares. The Property surrounds the past-producing Lake George Antimony Mine ("Lake George Mine") and is considered an exploration-stage Antimony-Gold (Sb-Au) prospect located immediately along strike to the southwest and northeast, as well as downdip to the north of the historical Lake George Mine. The Property benefits from excellent road access, hydroelectric power, and nearby available personnel for field and exploration activities.

The Lake George Mine was formerly the largest antimony producer in North America with a long history of production spanning from 1876 to 1996. The mine closed in 1996 due to falling antimony prices. From 1972 to 1981, 34,417 tonnes of concentrate grading 65% to 66% Sb was produced from the first deposit. Then from 1985 to 1990, approximately 1 Mt grading 4% Sb was extracted from a second deposit (Caron, 1996). The mine also contained molybdenum (Mo), tungsten (W), and Au mineralization. Infrastructure on the Lake George Mine includes 3 shafts, underground development on 10 levels, some remaining surface buildings, and a tailings pond. The deepest level of the mine is approximately 400 m below the surface. The Lake George Sb-Au Mine currently represents one of the Top 3 antimony occurrences in the Province of New Brunswick (Figure 1).

The Lake George Mine includes en-echelon gold-bearing polymetallic and antimony veins with massive stibnite hosted in Ordovician sedimentary and volcanic rocks adjacent to the Lake George granodiorite. Four (4) main antimony veins were developed at the mine, that generally have a shallow dip to the north and vary from 1 to 2 metres in width. The east-trending quartz vein system that has been traced over 1 km in depth and over 2 km along strike length (Procyshyn and Morrissy, 1990). A similar geological context of sedimentary rocks in contact with the intrusion, along with NE trending faults zones possibly responsible for developing the vein structures, is present on Hertz's newly-staked claims (Figure 2).