Black Mammoth Metals Leases Coal Canyon Gold Property, NV

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Black Mammoth Metals Corporation logo (CNW Group/Black Mammoth Metals Corp)
Black Mammoth Metals Corporation logo (CNW Group/Black Mammoth Metals Corp)

BMM: TSX-V

VANCOUVER, BC, April 15, 2025 /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 a lease with option to purchase agreement (the "Lease Agreement") signed on April 14, 2025, with private vendors (the "Vendor") to earn a 100% interest in the Coal Canyon gold property ("Coal Canyon" or the "Property"), situated in Pershing County, Nevada, in the West Humboldt Range and on the Oreana Trend, approximately 14 km west of the Rochester gold and silver deposit (see Figure 1) and 2 km south of the Willard Mine which was a heap-leach operation in the 1990's. The Property consists of 43 federal lode claims (approximately 359 hectares, 888 acres) administered by the Bureau of Land Management ("BLM").

Highlights:

  • Road cut sampling up to: 46m @ 0.76 g/t Au (oxide). (see Figure 2)

  • An extensive soils grid shows strong silver and molybdenum values surrounding the gold zone.

  • Existing drill permit with BLM needs change of operator.

  • Drill roads and pads constructed.

Geology:
The geology consists of Jurassic and Triassic sedimentary rocks intruded by Jurassic gabbro and Tertiary rhyolite. The main lithologic units on the property are part of the Auld Lang Syne Group which is a very thick sequence of peletic and sandy strata with interbeds and lenses of limestone and dolomite.

The Property hosts intrusive-related, sediment-hosted precious metal mineralization discovered by previous drilling and roadcut sampling. Channel sampling from these roadcut exposures documented wide zones of gold mineralization with associated high arsenic values. Outcrops of intrusive rocks and sill-like bodies of felsic to granodioritic composition and the associated alteration have a northwest strike and extend over a minimum strike length of 1750m and average approximately 120m in width. There are also east-west trending altered and mineralized zones up to 450m wide. Mineralization is primarily fracture-hosted, and is accompanied by oxidized, gossan zones, quartz veins and stringers. There are large outcrops of gossan-bearing material enriched in copper, molybdenum, and zinc, with pervasive silicification and massive sulfide (see Figure 2). The gossan zones have been intersected in drill holes but the sulfide potential is still unexplored.

Black Mammoth looks forward to commencing a complex on-site evaluation of this high prospective property with diverse discovery potential.


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