Us Goldmining Highlights Northern Exploration Targets at the Whistler Gold-Copper Project in Alaska

Whistler-Raintree Mineral System Exploration targets

The geological analysis of the WHISTLER company shows considerable potential to build up in Whistler on the first two extremely successful field times of the company in the summer of 2023 and 2024. Our growing database contains knowledge that was put together from holes, the shift of the historical drilling core, surface mapping and sampling as well as geophysical processing and interpretation. So far, over 25 potential individual goals have been identified, and the company works through a systematic review of its geological attributes to evaluate every goal and to develop priorities for future exploration programs.

The Whistler orbit area comprises a wide pool with a low, gently sloping topography between three mountain chains. The flanks and the lower parts of the pelvis are covered with variable thicknesses and gravel deposits. Thicker deposits of Till and gravel, see Figure 1 upper picture, prevents direct superficial mapping and geochemical prospecting techniques and therefore requires remote sensing techniques and/or holes to penetrate the cover sequence in order to test the underlying basic rock for the mineralization potential. One of the most important remote sensing techniques used in the exploration of gold clupper exploration is the magnetic measurement of air in which magnetometers that are attached to solid wing or rotary aircraft fly a grating pattern to map the distribution of the magnetic minerals in the geology of the upper crust. Magnetic surveys are particularly useful to explore the gold-Kupper porphyry systems such as Whistler, since both the intrusive rock of the host and the change associated with the gold-copper mineralization can produce magnetite in sufficient quantities for recognition through remote exploration.

High magnetic concentrations in circular anomalies (if they are viewed in a plan view), which are often referred to as anomalies of bull-eye, can be aligned directly for exploration on site. In recent years, the modeling of 3D underground in version has developed to the point where we can approach the geometry of the magnetic anomalies below the surface. With the well-known whistler deposit as a training data set, the magnetics processing for Whistler Orbit has modeled dozens of high-ranking tubes-like porphyry intra-intricate, which come to the surface Figure 1 lower picture. Our geologists find that a number of magnetic inversion goals have a scaling similar to the Whistler host diority porphyry porphyry, while other smaller porphyry or dike swarms from 'pencil' represent.

The Mammoth The goal is magnetically similar to the whistler deposit, which includes a pipe or plug-shaped interpreted penetration with a diameter similar to the whistler deposit and a “dome” on its base. Mammut is untrocated, but the surface until the sample increased in 2024 resulted in increased gold, copper, silver and other scouts mineral values ​​that were found proximally to the magnetic anomaly, and the morphological analysis of won gold particles shows irregular grains, which indicates potential nearby.

The Large white And Sunbowl Goals are largely interpreted as extensions in the north and south (each) of the Host Porphyr system by Whistler Depositing. Big White represents the northern expansion of the magnetic and induced polarity anomaly of the Whistler deposit (“IP”), which relates to the phyllic change associated with porphyrmineralization (see Figure 1). Sunbowl is located south of Whistler and also represents an anomaly of loading deparse, in which mineralization was excluded by storing whistler by failure or penetration of Porphyr -Post -Mineral -Porphyr.

At Raintree North and EastHistorical bores of magnetic destinations with bull-eye goals crossed increased gold, copper and silver masss, which indicates the correct types of rock and hydrothermal processes that could represent the nearby mineralization in porphyry style. The highlight of the historic Bohrlochs WH11-034, which was drilled in the Raintree north prospectus in 2011, comprised 120.66 meters at 0.73 g/t aueQ (with 0.46 g/t au, 0.16% Cu & 1.68 g/t AG).

Hotfootapprox. 0.75 kilometers south of the deposition of Raintree West includes a large, cable-shaped magnetic feature that resembles the host of the Whistler deposit. A single historical borehole (RG11-032) cut out of calm and phyllic change that indicate porphyry mineralization nearby. Also the Recently announced Drill Discovery (138.0 M at 0.99 g/t Aueq) 500 meters south of the deposition of Raintree West could represent distal veiling from a relatively nearby Porphyr source, for which Hotfoot is a potential candidate.

The company's geological analysis and exploration planning remains. Potential future exploration programs may be carried out in parallel to the previously announced first economic assessment of the company for the project (see press release April 15, 2025. Start data for the exploration have not yet been determined.

Technical information

Tim SmithP.GEO., Chief Executive Officer from US Goldmining, has monitored the preparation of this press release and checked and approved the scientific and technical information contained herein. Mr. Smith is a “qualified person”, as in Canadian National Instrument 43-101 Disclosure standards for mineral projects.

Further information on the project and the mineral resource estimates made here can be found in the summary of the technical report entitled “SK 1300 Technical Report Summary for the Whistler project, South Central Alaska“With a date of the entry into force of September 12, 2024and the technical report entitled “Ni 43-101 2024 updated mineral resource estimate for the Whistler project, South Central Alaska“With a date of the entry into force of September 12, 2024Available under the company's respective profiles at www.sec.gov and www.sedarplus.ca.

About us gold mining Inc.

Us Goldmining Inc. is an exploration and development company that focuses on improving the 100% Whistler Gold-Copper project, which is located northwest of 105 miles (170 kilometers) Anchorage, AlaskaUSA The Whistler project consists of several gold clutch porphyry deposits and exploration goals within a large regional country package that is entirely into the mining of Alaska in the amount of around 53,700 hectares (217.5 square kilometers). The estimate of the Whistler project mineral resources comprises 294 mt at 0.68 g/t aueue for 6.48 MOZ AueQ, plus 198 mt at 0.65 g/t AueQ for 4.16 MOZ AueQ.

Visit www.usgoldmining.us Further information, including high -resolution numbers.

Predicted statements

With the exception of the historical facts contained herein, the information presented in this press release are “future -oriented statements” within the meaning of The United States Bundes-Verwont paper laws and “future-oriented information” in the sense of the applicable Canadian securities laws (together, “future-oriented statements”). These statements contain statements on the expectations of the company in relation to the project, potential exploration goals, future work programs and the project's exploration potential. Words such as “expectations”, “anticipated”, “plans”, estimates “and” intentions “or similar expressions should identify future-oriented statements. Forward-looking statements are based on the current expectations of US gold mining. To Be Materialy Different From Any Future Results, Performance or Achievements Expressed or Implied by such Statements. Labor Disputes and other Risks of the Mining Industry Including, Without Limitation, Those Associated With The Environment, Delays Increased State Approval or Permits, there are other risks that have been examined and developing mineral characteristics and other risk factors in the company's submissions with the US securities and exchange commissioners Beiwww.sec.gov are inherent.

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