U.S. GoldMining Highlights Exploration Potential at the Muddy Creek Mineral System, Including Historic High Grade Rock Grab Samples up to 111.50 g/t Au, Whistler Gold-Copper Project, Alaska
- Strong gold mineralization potential demonstrated by high-grade surface samples up to 111.50 g/t Au
- Large exploration footprint of 6 km x 4 km indicating significant resource potential
- Historic drilling confirmed presence of intrusion-related gold system with broad mineralized intervals
- 100% ownership of the Whistler Project with multiple high-priority exploration targets
- Strategic location just 100 miles west of Anchorage, Alaska
- Limited historical drilling with only 955 metres completed
- Highest-grade areas of the system remain untested by drilling
- No definitive timeline for exploration program commencement
- Current drill results show only low-grade mineralization (0.41-0.44 g/t Au)
Insights
Strong gold surface samples suggest significant potential at Muddy Creek, but lack of systematic drilling means high risk-reward exploration ahead.
The Muddy Creek system represents a classic intrusion-related gold target with impressive surface sampling results. The average gold value of 3.03 g/t Au across 285 historic rock samples is substantially above economic thresholds for bulk-tonnage gold deposits, while high-grade samples reaching 111.50 g/t Au suggest potential for localized high-grade zones. The geological setting within the Estelle Suite monzonitic intrusions is particularly favorable, as these late Cretaceous intrusions host several significant gold deposits in Alaska.
What's particularly intriguing is that despite compelling surface geochemistry over a 6 km × 4 km area, previous drilling was limited to just three holes (955 meters) positioned at the margins of the system. The reported intercepts of 0.43 g/t Au over 38.8m and 0.44 g/t Au over 44.2m confirm mineralization extends to depth but likely missed higher-grade zones suggested by surface sampling. This creates a scenario where the highest-potential portions of the system remain entirely untested.
The company's description of sheeted quartz veins with arsenopyrite, pyrrhotite, and pyrite is consistent with the classic "reduced intrusion-related gold system" model. In such systems, recognizing structural controls and zones of increased vein density is critical. The identification of two principal trends - the 5 km Discovery Creek to Bonanza Zone and the 4 km Contact Zone - provides clear targeting frameworks for follow-up work.
The lack of systematic modern exploration across these zones represents both risk and opportunity. While the high-grade surface samples are encouraging, their narrow nature means bulk grades would likely be lower, and the distribution of mineralization remains poorly understood without more drilling. The company's plans for phased exploration represent a prudent approach to systematically evaluate this potential.
Highlights:
- The Muddy Creek mineral system comprises a large gold surface geochemical footprint over an area of approximately 6 km x 4 km, with an intrusion-related gold geochemical signature. It is located approximately 10 miles southwest of the Whistler deposit and 5 miles northwest of the Island Mountain deposit.
- Historic exploration work completed by previous explorers included reconnaissance rock grab sampling and soil sampling, magnetic geophysical surveying and a small drilling program which tested the margins of the system and confirmed broad low grade gold mineralization.
- Reconnaissance historic rock chip sampling has returned 73 samples which assayed >1 gram per tonne gold ("g/t Au"), including 20 samples which assayed >10 g/t Au, and peak values of 111.50 g/t Au in the 'Upper Phoenix Creek' zone, 69.13 g/t Au in the 'Bonanza' zone and 56.6 g/t Au in the central 'Muddy Creek' zone. The average gold value of 285 historic rock samples collected over the Muddy Creek area is 3.03 g/t Au, attesting to the strong gold endowment of this large system.
- Broadly spaced reconnaissance soil sampling traverses returned 104 samples which assayed >0.10 g/t Au (approximately 10 x background gold values), 56 samples returned >0.50 g/t Au and 14 samples >2.0 g/t Au. Peak gold-in soil values in the central 'Muddy Creek' zone include 5.29 g/t Au, and at 'Discovery Creek' zone up to 2.43 g/t Au.
- Historic drilling targeted the fringes of the mineral system, returning encouraging results and confirming an intrusion related gold system exists at Muddy Creek. However, the highest tenor parts of the system have not been drilled to date.
Tim Smith, Chief Executive Officer of U.S. GoldMining, commented: "In parallel with the Company's recently commenced PEA focused on the existing Whistler Project mineral resources, our technical team has continued to evolve its geological knowledge across the broader Project, and we're excited to have identified significant exploration potential across three large mineral systems identified to date. The numerous historic high grade rock and soil samples collected to date on the Muddy Creek target warrant further systematic exploration, including drilling. The Company is currently planning to develop phased exploration programs to test the highest ranking targets, including at Muddy Creek, which could potentially commence this summer field season. We're excited about this further development in the potential growth of the emerging 'West Susitna Mineral District', located just 100 miles west of
Muddy Creek Mineral System Exploration Targets
The Company's geological analysis of the Whistler Project over the first two highly successful 2023 and 2024 field seasons focused primarily on the Whistler deposit and to a lesser extent on the Whistler Orbit target area. Geologists briefly visited the Muddy Creek target area (see Figure 1), located 10 miles southwest of the Whistler deposit, during the 2024 field season to confirm mineralization style and tenor at two locations: the 'Arsenoknob' showing and the 'Contact Zone'.
Muddy Creek is hosted within a monzonitic intrusive complex, part of the Estelle Suite of intrusions that were emplaced in the late Cretaceous (~65 million years ago). Gold mineralization is of the "Intrusion-Related Gold" class of gold deposits and occurs within narrow sheeted quartz veins that contain minor arsenopyrite, pyrrhotite, pyrite and trace chalcopyrite. Exploration for intrusion related gold deposits generally is focused on areas where the vein/fracture density is highest. Surface sampling to date, comprising rock grab sampling and broad-spaced contour-parallel and ridge-line soil sampling, confirms that the best grades in the monzonite are associated with the highest observed density of veins along the strike extent of a northwest-striking structural corridor, the Discovery Creek to Bonanza zone (see Figure 2).
The average gold value of 285 rocks collected over the Muddy Creek area is 3.03 g/t Au, with a maximum value of 111.50 g/t Au, attesting to the strong gold endowment of this large system. Many of the rock samples collected are of narrow mineralized structures that occur throughout the prospect area, and while they are not representative of the potential bulk grade of the mineral system, their widespread distribution and high tenor broadly confirms a large area of potential bedrock mineralization.
Two principal trends have emerged so far from the surface geochemical data collection, each requiring further detailed mapping and sampling and remaining open along strike (see Figure 2). The Discovery Creek to Bonanza Zone, which trends NW-SE over at least 5 km of strike length, is mapped in monzogranite within the Mt Estelle pluton, with gold associated with sheeted quartz veins typical of a classic intrusion related gold system. The Contact Zone can be traced over at least 4 km, interpreted as a hornfelsed carapace to the Mt Estelle Intrusion. Detailed geological mapping and additional surface geochemical sampling is required to define the geometry of the intrusive phases and, in particular, to identify the upper zones (or 'carapace') of the host pluton, which is a typical position for the highest vein density and highest grading mineralization in intrusion related mineral systems.
In 2011, Kiska Metals Corporation conducted 955 metres of exploration drilling at Muddy Creek, the only holes drilled on this portion of the Project, located on the edges of the Discovery Creek to Bonanza higher-density vein/fracture zone. Two diamond core holes drilled near the Arsenoknob showing returned broad intercepts of low grade mineralization indicative of an intrusion related system, including:
- 0.43 g/t Au over 38.8 m from 262 m depth in hole MC11-001, and
- 0.41 g/t Au over 45.0 m from 159 m depth and 0.44 g/t Au over 44.2 m from 297 m depth in hole MC11-002.
The historic drill intercepts provide encouragement that higher grade mineralization could be discovered elsewhere within the broader Muddy Creek mineral system if zones of higher density veining can be identified. Drill hole MC11-003 near the 'Bonanza Zone' was abandoned prior to reaching target depth.
The highest tenor parts of the Muddy Creek system have not been drilled to date, including the Upper Phoenix Creek zone with rock samples up to 111.50 g/t Au, the 'Bonanza' zone with rock samples up to 69.13 g/t Au, and the central portion of the Muddy Creek zone north of Arsenoknob which contains rocks samples to 56.6 g/t Au and soil samples peaking at 3.65 g/t Au.
The Company is planning to undertake future systematic follow-up exploration at Muddy Creek. Start dates for exploration have not been determined yet.
Data Verification
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,
Rock samples referenced herein consisted of approximately one kilogram of rock collected over a small area surrounding each sampling site collected with a rock hammer. The sampling location was located using a handheld GPS unit and marked in the field with a metallic tag. Descriptive information about the geology of the sample was recorded and aggregated into the project database. Soil samples were collected along traverses as part of multi-kilometre reconnaissance programs, generally at 100 meter spacing. Soil samples were collected from the surface soils (generally the B-horizon) by extracting approximately one kilogram of soil, usually with a hand auger. Each sampling site is located using a GPS unit. Descriptive information such as sample depth and physical attributes were recorded and aggregated into the project database. Typically, field duplicates were collected at a rate of one in every twenty samples.
Historic rock and soil samples were predominantly submitted to Alaska Assay Laboratories for preparation. Pulps were then submitted to ALS-Chemex by the preparation laboratory for assaying. Gold was assayed by fire assay and atomic absorption finish (Au-AA23) on thirty gram sub-samples and for a suite of 33 elements (including copper and silver) by either aqua regia digestion or 3- or 4-acid digest, followed by ICP-AES (method code ME-ICP41) on 0.5 gram sub-samples. Elements exceeding concentration limits of ICP-AES were re-assayed by single element aqua regia digestion and atomic absorption spectrometry (method code element-AA46). The Company's 2024 sampling utilized Bureau Veritas for sample preparation at their lab in
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.
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Forward-Looking Statements
Except for the statements of historical fact contained herein, the information presented in this news release constitutes "forward-looking statements" within the meaning of
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