Black Mammoth Metals Options Callaghan Gold Property in Central Nevada

In This Article:

No.24-12    BMM: TSX-V

VANCOUVER, BC, Aug. 2, 2024 /CNW/ - Black Mammoth Metals Corporation (TSXV: BMM) (OTC: LQRCF) ("Black Mammoth" or the "Company") is pleased to announce that Antelope Creek Gold Corporation ("Antelope Creek"), a wholly owned subsidiary of Black Mammoth, has entered into an option agreement (the "Option Agreement") dated July 17, 2024, with a private vendor (the "Vendor") to earn a 100% interest in the Callaghan gold property (the "Callaghan Property" or the "Property"), located 24 kms NE of Austin, Nevada (see fig.1). The Company has completed a sampling program and due diligence work and has expanded the Callaghan Property through additional staking, completed on July 31, 2024.

The Callaghan Property now consists of 45 Federal lode mining claims (930 acres, 376 hectares) on BLM land and is situated on the eastern flank of the northern Toiyabe Range, Lander County, Nevada. It is located along the 120-kilometer Austin-Tonopah trend of gold occurrences, deposits and mines that include Quito, Round Mountain, and Northumberland, and is considered prospective for Carlin-type gold mineralization. The Company's Quito property is a past-producing mine on this trend.

The Callaghan Property is located within an erosional window (the Callaghan Window) that exposes highly prospective Lower Plate Paleozoic sedimentary rocks, which on the Property have been strongly altered by gold, arsenic, antimony and mercury-bearing hydrothermal fluids. The Callaghan Property contains near-surface gold mineralization in several historic drill holes at the Cottonwood Canyon area, with historic reports estimating approximately 50,000 oz @ 0.5 g/t, hosted in Upper Plate Paleozoic sedimentary rocks.

Black Mammoth has not independently confirmed the historical estimate of mineralization at the Cottonwood Canyon area. Black Mammoth is not treating the historical estimate of mineralization as current mineral resources or as historic resources, and a qualified person has not done sufficient work to classify the historical estimate of mineralization as current mineral resources or as historic resources. A qualified person has not yet determined what work needs to be done to upgrade or verify the historical estimate of mineralization as current mineral resources or as historic resources. The historical estimate of mineralization is relevant for historical completeness but should not be relied on.

Drill Target Areas:

Rast

The Rast area has been the focus of widely spaced, and mostly shallow, historic drilling over an area largely covered by shallow alluvium. Holes intersected strong pathfinder elements and sporadic gold intercepts; however, important geochemical, structural, and stratigraphic data from these holes indicates that the potential of this area remains largely untested. Drilling in the Rast area has demonstrated the presence of anomalous gold in decalcified Lower Plate carbonate host rocks. Shallow trenches expose strongly silicified and clay-altered Orovician-age carbonate rocks (hosts at the Company's nearby Quito property and elsewhere). A 300 meter long, open-ended, easterly trending gold-arsenic-antimony soil anomaly is present to the east of the historic Rast mercury mine. In addition, Lower Plate rocks with intense alteration consistent with Carlin-type gold systems are present at surface approximately 800 meters to the northwest of the historic Rast mine. The Rast area has three target areas where there are anomalous soils at the intersection of Lower Plate carbonate host rocks below the Roberts Mountains Thrust and NW normal faults.