PANTHER MINERALS COMPLETES INITIAL SITE VISIT ON THE HUBER HEIGHTS URANIUM PROPERTY, ELKO COUNTY, NEVADA

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VANCOUVER, BC, Aug. 15, 2024 /CNW/ - Panther Minerals Inc. ("Panther Minerals" or the "Company") (CSE: PURR) (OTC: GLIOF) (FWB: 2BC) reports that the initial site visit has been completed on the Huber Heights Uranium property (the "Property"), located in northern Elko County, Nevada. The Property comprises 35 unpatented mineral claims (700 acres, 283 ha), located near the village of Mountain City. As reported previously (Press Release July 9th, 2024) the Property covers known uranium prospects and showings that were discovered in the 1950s, including the Autunite and October Group prospects, and the Huber Hills Granite Ridge Prospect.

Panther Minerals Inc. Logo (CNW Group/Panther Minerals Inc.)
Panther Minerals Inc. Logo (CNW Group/Panther Minerals Inc.)

The Property lies within the Mountain City Mining District, centred approximately 110 kilometres north of Elko, Nevada. As previously disclosed, the first mining activities were based on gold and silver discoveries in the late 1860s, but more recently the district was known for copper production from the Mountain City Copper Mine. Uranium was discovered in the area in 1954, with limited production between 1958 and 1963.

To date, activities by contract geologists retained by the Company have comprised geologically mapping, prospecting visually and with a spectrometer, and soil and rock sampling. Field examinations have largely corroborated the historical literature (previously reported) of two types of uranium mineralization. One type of uranium mineralization occurs along vertical fractures and/or shear zones in quartz monzonite (Autunite and October prospects) associated with intense alteration. The other type of uranium mineralization is related to the contact zone between the underlying Cretaceous quartz monzonite and the overlying Tertiary volcanic sediments. Numerous areas of historic trenching were observed and several apparent adits, which are now collapsed and inaccessible. Both types of uranium mineralization tend to weather recessively due to associated alteration, and outcrop exposure is limited. Soil geochemistry, followed by geophysical surveys will be utilized to define initial drill targets.

Scattered autunite (a secondary uranium mineral) has been observed on fractures in the granite, with some localized-on NNW-trending faults. Occasionally autunite mineralization (autunite is a radioactive secondary mineral resulting from the oxidation of uranium minerals associated with hydrothermal alteration) has been observed on fractures in granite, with some potentially localized along NNW trending faults. The granite is hydrothermally altered with propylitic and sericitic alteration observed locally. Company geologists are returning to the Property this month to continue additional soil and rock geochemistry, and spectrometer surveying.