お知らせ • Mar 18
Zeus North America Mining Corp. announced that it has received CAD 2.5755 million in funding On March 17, 2026, Zeus North America Mining Corp closed the transaction. In connection with the final tranche, the Company has paid finders’ fees in connection with proceeds raised by the Company from investors introduced to the Company by finders consisting
of cash of CAD 29,280 and non-transferable broker warrants. An insider of the Company has subscribed for Units pursuant to the final tranche of the Placement. お知らせ • Jun 21
Zeus North America Mining Corp. announced that it expects to receive CAD 1.5 million in funding Zeus North America Mining Corp. announced a non-brokered private placement to issue 10,000,000 units at an issue price of CAD 0.15 per unit for gross proceeds of CAD 1,500,000 on June 20, 2025. Each unit will comprise one common share and one-half of one common share purchase warrant. Each warrant will entitle the holder to acquire an additional common share at a price of CAD 0.25 per share for a period of two years. Finder’s fees may be payable on all or any portion of the placement, which is subject to regulatory and exchange approval. Completion of the placement is subject to certain conditions including the receipt of all necessary approvals and the acceptance by the Canadian Securities Exchange. お知らせ • Jun 09
Zeus North America Mining Corp., Annual General Meeting, Aug 15, 2025 Zeus North America Mining Corp., Annual General Meeting, Aug 15, 2025. お知らせ • Mar 17
Zeus North America Mining Corp. Announces Rock Grab Sampling Results from the Previously Announced Exploration Program at its Cuddy Mountain Project in Idaho Zeus North America Mining Corp. announced the rock grab sample results from the previously announced exploration program at its Cuddy Mountain Project (the "Project" of "Cuddy Mountain") in Idaho. Cuddy Mountain is located approximately 3 kilometres ("km") to the north of Hercules Metals Corp.'s high-grade "Hercules" coppermoly-silver porphyry discovery announced in October 2023. Highlights of the Rock Grab Sampling Program at Cuddy Mountain: Collected 339 property wide rock grab samples. Of the 339 rock grab samples collected: 35 samples contain 0.1% ("%") copper ("Cu") or more; 16 samples contain greater than 1.1 % Cu, up to and including 3.8% Cu; 26 samples contain 10 g/t molybdenum ("Mo") or more; 5 samples contain more than 40 g/t Mo, with values up to and including 182 g/t Mo (with 0.37g/t Au). The Cuddy Mountain Property is adjacent to Hercules Metals Corp.'s recently discovered Leviathan Copper Porphyry (CAD 167 Million Market Capitalization). The discovery resulted in Barrick injecting CAD 23 million in equity while staking a substantial land position in the district along with Rio Tinto. The Cuddy Mountain Property consists of 101 lode mining claims respectively and cover a cumulative area of approximately 2020 acres. Further historical exploration on Zeus's Cuddy Mountain Project occurred at the Edna May Mine: Mineralized vein with chip samples containing 750 ppm lead ("Pb"), 7.7% zinc ("Zn") and 252 ppm Ag over 4 feet. Underground drilling in 1979 intersected 1.38 oz/t Ag over 7 feet in a breccia zone (Burmeister, 1980). Additional exploration (By Taylor, 1977) at the Rockslide area encountered Malachite-stained outcrops with a grab sample containing 760 ppm Pb, 0.67 % Zn and 36 grams per tonne Silver (Taylor, 1977). All information is derived solely from management of Zeus Mining and otherwise publicly available third-party information which are believed to be reliable, but which have not been independently verified by the Company and as a result are not guaranteed to accuracy and completeness. Zeus's management cautions that past results or discoveries on properties in proximity to Zeus may not necessarily be indicative of the presence of mineralization on the Company's properties. Qualified Person. The scientific and technical information in this news release has been reviewed and approved by Dean Besserer, P.Geo., the President & CEO for the company and Qualified Person as defined in NI 43-101. On behalf of the board of directors. お知らせ • Feb 06
Zeus North America Mining Corp. completed the Spin-Off of Kelso Mining Inc. Zeus North America Mining Corp. entered into a Plan of Arrangement to Spin-Off Kelso Mining Inc. on August 26, 2024. Under the terms of the Arrangement, Zeus' shareholders will be issued one share of Kelso with respect to every 150 shares of Zeus owned on the share distribution record date. Holders of Zeus options and warrants, who exercise their options and/or warrants before the Share Distribution Record Date, will also be entitled to receive one share of Kelso with respect to every 150 shares of Zeus. The Chlore Property will be transferred to Kelso. Upon completion of the Arrangement, Zeus shareholders will ultimately own shares in two public companies: Zeus, which will be focused on its properties in the State of Idaho known as the Cuddy Mountain, Selway and Great Western properties and Kelso, which will focus on the Chlore Property. Completion of the Arrangement is subject to the approval by the shareholders of Zeus by a special resolution at a special meeting, the approval of the Supreme Court of British Columbia and the acceptance of the Arrangement by the Canadian Securities Exchange. As of December 19, 2024, Zeus Shareholders has approved the transaction. As of January 9, 2025, Supreme Court of British Columbia approved the transaction. The scheme was accepted by the Canadian Securities Exchange on January 20, 2025. The share distribution record date has been set at January 29, 2025. Spin off is expected to complete on February 5, 2025. National Securities Administrators Ltd acted as a transfer agent to Zeus North America Mining.
Zeus North America Mining Corp. completed the Spin-Off Kelso Mining Inc. on February 5, 2025. お知らせ • Oct 25
Zeus North America Mining Corp. Provides Cuddy Mountain Exploration Update Zeus North America Mining Corp. announced that Zeus has completed its 2024 exploration program at its Cuddy Mountain Project. The summer programs consisted of property wide mapping, sampling and geophysics including: 799 Soil samples; 339 rock grab samples; mapping and property wide ground magnetics and 3D-DCIP Induced Polarization ("IP") and Resistivity surveys. Results are pending and will be provided in further updates when available. Importantly, the mapped stratigraphy within the Cuddy Mountain Property demonstrates that the same stratigraphic section exists with the Property as that shown on Hercules drill sections which intersected Porphyry mineralization. Highlights from the Mapping: Exposures of the Hercules Rhyolites in the northeast commonly form large outcrop faces. The Rhyolites are more than 100 m thick and may be repeated by faulting. The Rhyolites are often silicified with propylitic alteration. Exposures of the ‘red conglomerate', which is a marker horizon at the unconformity between the Hercules Rhyolites and Seven Devils Volcanics. These are exposed in the northeastern, central, and southwestern parts of the Property. The ‘red conglomerate', overlying the Seven Devils volcanic complex is immature and polymictic with interbedded sand- and siltstone. Outcrops weather red (hematite) to greyish green. Exposures of the Seven Devils Volcanics occur in the southern and central parts of the Property below the basalt cover to the south. Commonly heterogenous volcanic textures, from aphanitic to laminated to phenocrystic to volcanoclastic, at outcrop scale. The rocks are variably fractured to brecciated, bleached, silicified and/or oxidized, with at least two prominent southeast-trending zones of intense alteration and mineralization (blebby and disseminated sulphides; intense manganese oxide and iron staining to fracture-controlled infiltration/replacement), possibly controlled by fault zones. Barite hydrothermal vein mineralization occurs in trenches near the south end of Property. Exposures of younger porphyry intrusions are typically moderately to strongly fractured and locally brecciated including fragments of volcaniclastic rocks. These may form dykes and/or intrusive bodies in the volcanic complex. Locally these intrusions and/or dykes are strongly sulphidic with chalcopyrite. Chalcopyrite, malachite, azurite, and chrysocolla are common in porphyry units around the historical Rockslide copper showing. Mineralized hydrothermal breccias were mapped near the historical Edna May showing. They consisted of intrusive or hydrothermal breccias. Near the Edna May showing the breccias have a black matrix pyrite and peacock sulphides along the margin or porphyry dykes. Fragments of fine grey silicified material locally contain up to 10% sooty sulphides, 1% pyrite and trace bornite and chalcopyrite. Structural complexity exists throughout the Property including numerous mapped folds and faults. Numerous mapped faults contain copper mineralization as malachite and azurite. Alteration styles were notable throughout the Property, including: Chlorite alteration halos around quartz veins; Sericite +/- chlorite +/- pyrite alteration in monzonitic porphyry dykes; and Semi-massive epidote-magnetite +/- pyrite alteration. Intense epidote alteration was observed in many areas of the Seven Devils Volcanics, especially moving towards the southern portion of the valley. 