U.S. GoldMining Highlights Northern Exploration Targets at the Whistler Gold-Copper Project, Alaska
- Project encompasses a large 53,700-acre land package with significant exploration potential
- Recent drilling success with 138.0 m at 0.99 g/t AuEq intersection
- Over 25 individual exploration targets identified within the Whistler Orbit area
- Strategic location just 100 miles from Anchorage, Alaska
- Existing deposits make up <1% of total Project area, indicating substantial growth potential
- None.
Insights
U.S. GoldMining's exploration targets at Whistler showcase significant resource expansion potential within a promising porphyry cluster system in Alaska.
The Whistler Gold-Copper Project represents a classic porphyry cluster system spread across a 5 x 5 km area containing multiple intrusions. This geological setting is particularly significant because porphyry deposits are the world's primary copper source and often contain valuable gold and silver, with Whistler representing a gold-rich variant. The company has identified over 25 individual exploration targets within what they call the 'Whistler Orbit,' comprising both mapped and interpreted diorite porphyry stocks and dykes from 3D magnetic modeling.
Recent drilling results validate the exploration potential, with one hole yielding 138.0 meters grading 0.99 g/t gold equivalent (0.89 g/t Au, 0.05% Cu, 17.57 g/t Ag, 0.44% Pb, 0.95% Zn) in a previously undrilled area 500 meters south of the Raintree West deposit. This intercept represents high-grade mineralization by industry standards and demonstrates the potential for additional discoveries within the project area.
The company's technical approach is methodologically sound, utilizing advanced geophysical techniques including magnetic surveying and 3D inversion modeling to identify subsurface targets beneath till and gravel cover. This methodology has identified several promising targets with similar magnetic signatures to the established Whistler deposit, including the undrilled Mammoth target and extensions of known mineralization at Big White and Sunbowl.
Historical drilling at Raintree North has already intercepted 120.66 meters of 0.73 g/t gold equivalent, further supporting the potential for additional economic mineralization within the broader system. What's particularly noteworthy is that the existing gold-copper deposits represent less than 1% of the total 53,700-acre project area, suggesting substantial exploration upside within this emerging West Susitna Mineral District of Alaska.
The company appears to be pursuing a dual-track approach, advancing both economic studies on existing resources while simultaneously developing exploration programs to expand the resource base, potentially supporting a larger mining operation in the future.
Highlights:
- The Whistler - Raintree mineral system, also referred to as the 'Whistler Orbit', comprises a classic 'porphyry cluster' spread over an area of approximately 5 x 5 km, containing multiple mapped and interpreted porphyry intrusions and including the established Whistler and Raintree West mineral resource deposits. Porphyry deposits are the primary source of copper globally and can also contain significant other metals such as gold, silver and molybdenum.1 Whistler represents a gold-rich variant of the porphyry family.
- Over 25 individual exploration targets are identified within the Whistler Orbit area, comprising a mix of mapped diorite porphyry rocks and/or surface geochemical anomalies, and interpreted diorite porphyry stocks and dykes from 3D magnetic modelling.
- The potential for new discoveries within the Whistler Orbit was exemplified by the recently announced drilling results south of Raintree West deposit (see news release dated February 10, 2025) which included 138.0 m at 0.99 g/t AuEq (comprised of 0.89 g/t Au and
0.05% Cu) plus 17.57 g/t Ag,0.44% Pb and0.95% Zn, located 500 meters south of the Raintree West deposit in an area with no previous drilling. - The Company's
100% owned Whistler Project, which lies within the emerging West Susitna Mineral District located just 100 miles west ofAnchorage, Alaska , encompasses a contiguous land package of 53,700 acres of State mining claims. The footprint of the existing gold-copper deposits makes up <1% of the total Project area. - The Company is currently planning for potential future exploration programs to test the highest ranking gold ± copper ± silver targets identified to date and to develop phased exploration programs which could commence this coming summer.
1. | For more information on porphyry deposits visit the USGS website www.usgs.gov Including: "A global database of porphyry copper deposits and prospects", March 4, 2025. |
Tim Smith, Chief Executive Officer of U.S. GoldMining, commented: "The Whistler Gold-Copper Project is located within the West Susitna Mineral District, which contains established gold, copper and silver mineral resources, plus potential for other critical metals such as antimony and tungsten. The Whistler Project, located just 105 miles from
Whistler-Raintree Mineral System Exploration Targets
The Company's geological analysis of Whistler indicates significant potential to build upon the Company's first two highly successful field seasons completed at Whistler during the summer of 2023 and 2024. Our growing database incorporates knowledge compiled from drilling, relogging of historical drill core, surface mapping and sampling, and geophysical processing and interpretation. Over 25 potential individual targets have been identified to date, and the Company is working though a systematic review of their geological attributes to rank each target and to develop priorities for future exploration programs.
The Whistler Orbit area comprises a broad basin with low-lying gently sloping topography located between three mountain ranges. The flanks and lower parts of the basin are covered in variable thickness till and gravel deposits. Thicker deposits of till and gravel, see Figure 1 upper image, prevents direct surficial mapping and geochemical prospecting techniques and thus requires remote sensing techniques and/or drilling to penetrate the cover sequence to test the underlying bedrock for mineralization potential. One of the key remote sensing techniques used in gold-copper exploration is airborne magnetic surveying, where magnetometers attached to fixed-wing or rotary aircraft fly a grid pattern to map the distribution of magnetic minerals in the geology of the upper crust. Magnetic surveys are particularly useful for exploring for gold-copper porphyry -systems like Whistler, because both the host intrusive rock and the alteration associated with gold-copper mineralization can produce magnetite in sufficient quantities for detection by remote sensing.
High magnetite concentrations in circular anomalies (when viewed in plan view), often referred to as 'bulls-eye' anomalies, can be directly targeted for on-ground exploration. Over recent years, 3D subsurface 'inversion' modelling has evolved to the point where we can approximate the geometry of the magnetic anomalies below surface. Using the known Whistler Deposit as a training dataset, the magnetics processing for Whistler Orbit has modelled dozens of high-level pipe-like porphyry intrusives coming close to surface – see Figure 1 lower image. Our geologists note that a number of magnetic inversion targets have similar scale to the Whistler Deposit host diorite-porphyry, while others represent smaller 'pencil' porphyries or dyke swarms.
The Mammoth target is magnetically similar to the Whistler deposit, comprising a pipe- or plug-shaped interpreted intrusion with a similar diameter to the Whistler deposit and a 'cupola' located at its base. Mammoth is undrilled, but surface till sampling in 2024 revealed elevated gold, copper, silver and other pathfinder mineral values located proximal to the magnetic anomaly, and morphological analysis of recovered gold particles indicates irregular shaped grains which suggests a potential nearby source.
The Big White and Sunbowl targets are interpreted broadly to be extensions north and south (respectively) of the Whistler deposit host porphyry system. Big White represents the northern extension of the Whistler deposit's magnetic and Induced Polarity ("IP") chargeability anomaly, which relates to phyllic alteration associated with porphyry mineralization (see Figure 1). Located to the south of Whistler, Sunbowl likewise represents a chargeability anomaly where mineralization may have been offset from the Whistler deposit by faulting or intrusion of post mineral porphyry.
At Raintree North and East, historic drilling of bulls-eye magnetic targets intersected elevated gold, copper and silver assays, indicative of the right rock types and hydrothermal processes that could represent nearby porphyry-style mineralization. The peak intercept from historic drillhole WH11-034, drilled in 2011 at the Raintree North prospect, comprised 120.66 meters at 0.73 g/t AuEq (containing 0.46 g/t Au,
Hotfoot, located approx. 0.75 kilometers south of Raintree West deposit, comprises a large pipe-shaped magnetic feature similar to the host of the Whistler deposit. A single historic drill hole (RG11-032) intersected potassic and phyllic alteration suggestive of porphyry mineralization nearby. Also, the recently announced drill discovery (138.0 m at 0.99 g/t AuEq) located 500 meters south of Raintree West deposit, could represent distal veining from a relatively nearby porphyry source, for which Hotfoot is a potential candidate.
The Company's geological analysis and exploration planning remains ongoing. Potential future exploration programs would be expected to run in parallel with the Company's previously announced initial economic assessment for the Project (see news release 15 April 2025), thereby seeking to develop Whistler's full potential by investigating not only the base case mine development potential of the existing resources, but also to build a pipeline of future potential resources which could feed into a larger potential mining opportunity at the Whistler Project in future. Start dates for exploration have not been determined yet.
Technical Information
Tim Smith, P.Geo., Chief Executive Officer of U.S. GoldMining, has supervised the preparation of this news release and has reviewed and approved the scientific and technical information contained herein. Mr. Smith is a "qualified person" as defined in Canadian National Instrument 43-101 – Standards of Disclosure for Mineral Projects.
For further information regarding the Project and the mineral resource estimates referenced herein, refer to the technical report summary titled "S-K 1300 Technical Report Summary Initial Assessment for the Whistler Project,
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SOURCE U.S. GoldMining Inc.