Exhibit 99.1
U.S.
GoldMining Expands Pipeline of High-Priority Targets With 2026 Surface Exploration Program at its Whistler Gold-Copper Project, Alaska
Anchorage,
Alaska – September 28, 2026 – U.S. GoldMining Inc. (NASDAQ: USGO) (“U.S. GoldMining” or the “Company”)
announces the completion of a surface exploration program (the “Program”) at its 100% owned Whistler Gold-Copper Project
in Alaska (“Whistler” or the “Project”). Alongside the recently completed 7,493 meters of diamond core drilling
across 10 targets within the Whistler Orbit (see news release dated September 22, 2026), the Company executed an extensive surface exploration
campaign across the broader property. The Program, including identification and sampling of new outcrop zones of gold-copper porphyry-style
mineralization, supports a systematic evaluation of district-scale mineral systems to build and expand a pipeline of high-priority drill
targets aimed at discovering new gold-copper resources.
Highlights:
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Expands
the District-Scale Target Pipeline: Prospecting, geological mapping, and rock chip sampling were completed with the aim of adding
prospects to the existing robust pipeline of exploration targets across the Whistler Project. Field observations indicate potential
extensions to the known gold-copper porphyry mineral systems at Whistler-Raintree (the ‘Whistler Orbit’) and Island Mountain,
while further defining target areas within the emerging Muddy Creek intrusion-related gold system. |
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Whistler
Orbit Footprint Expanded: Geologists identified and sampled new outcrop zones of gold-copper porphyry-style mineralization featuring
porphyritic intrusions, phyllic and potassic alteration, and diagnostic quartz-sulfide veining, associated with historical elevated
gold and copper rock grab samples. |
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Island
Mountain Anomalies Extended: Reconnaissance mapping over zones of historical elevated gold and copper rock grab samples indicates
targets to support potential resource expansion to the northwest of the existing drill-delineated mineral resource, in addition to
identification of untested geochemical and geophysical anomalies outside of the known resource. |
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Muddy
Creek Drill Vectors Defined: Mapping and prospecting programs built upon the 2025 field campaign, sharpening vectors toward future
drill targets. Work focused on areas with higher tenor gold (+/- antimony) in historical rock grab samples, and high-density quartz
veining along contact zones between the host granodiorite intrusion and sedimentary country rocks – a classic setting for intrusion-related
gold mineralization. |
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Growth
Potential: Surface exploration is designed to delineate high-priority targets for future drill testing with the goal of ultimately
expanding the Whistler Project’s existing mineral resource inventory, which currently comprises 5.41 Moz AuEq of indicated
resources and 4.97 Moz AuEq of inferred resources across the Whistler, Raintree West, and Island Mountain deposits. See “Technical
Information” below for further information. |
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Surface
Assays Pending: The Company submitted 58 rock grab samples for gold, copper, and multi-element assaying to characterize grade
distribution, mineralogical associations and geological context. Assay results are subject to laboratory turnaround times. |
Tim
Smith, Chief Executive Officer of U.S. GoldMining, commented: “Our 2026 surface exploration program has demonstrated the prospectivity
and expanding scale of the mineral systems across the Whistler Project. Our geological teams made exciting progress, including identifying
and sampling new outcrop zones of gold-copper porphyry-style mineralization, that builds confidence in our extensive pipeline of exploration
targets, expanding our known footprints at the Whistler Orbit, Island Mountain, and Muddy Creek. We look forward to providing updates
on the Program as rock grab and drill core assay results are received over the coming months. This data will support additional future
exploration and drilling campaigns as we follow up on high-priority targets with the goal of identifying new gold and copper discoveries.”
Figure
1 Surface exploration locations and target areas within the Whistler Project completed during the 2026 summer field season. Graduated
red squares indicate gold grade of historical rock grab samples; purple squares show 2026 rock grab samples (assays pending), and yellow
crosses indicate field stations for mapping observations, geochronological samples and hyperspectral sampling locations.
Figure
2 Surface exploration mapping and sampling photographs from the 2026 summer field season. A: Senior geologist Dr. Mike Sepp
(PhD) at Island Mountain. B: Sulfide stringers in vein quartz at Snow-Canyon Ridge. C: Quartz vein with pyrite and minor
chalcopyrite in central suture-line (characteristic porphyry-style ‘B-vein’) at Long Lake Hills. D: Geologist Jared
Liimu prospecting and mapping at Long Lake Hills.
2026
Surface Exploration Program
In
addition to the 7,493-meter diamond core program targeting gold-copper porphyry mineralization under glacial till cover at the Whistler
Orbit, the objective of the 2026 summer field season was to advance the Company’s knowledge of the geological controls on areas
of known outcropping Au + Cu ± Ag ± Sb mineralization identified from past exploration campaigns, including follow-up of
historical rock grab sampling. Over the course of the 2026 field season, reconnaissance geological mapping, prospecting and rock grab
sampling were completed at two areas north of the Whistler Orbit (also referred to as the Whistler-Raintree mineral system) and at the
Island Mountain and Muddy Creek mineral systems.
In
total, 58 rock grab samples were collected to characterize gold-copper abundance and mineralogical/geological associations. In addition,
12 geochronological samples were collected to help categorize the relative age of host intrusions and to define fertile magmatic suites
for potential Au-Cu mineralization. Also, 68 samples were collected at the Long Lake Hills prospect area for hyperspectral analysis which
helps to characterize subtle mineral alteration species associated with porphyry mineralization.
Whistler
Orbit Extensions
Several
prospects in the Snow-Canyon Ridge area, located over a broad area 2 to 5 miles north of the Whistler gold-copper deposit, were
visited to locate numerous high grade Au rock grabs identified in historical sampling (up to 26.9 g/t Au and 0.07% Cu). Reconnaissance
mapping and follow-up prospecting were completed at three of four anomalous zones; the northernmost zone will be mapped and sampled next
season. At the location where the historical 26.9 g/t Au rock grab was collected, mineralization was observed to be associated with porphyry
lithologies and alteration, comprising sulfide stringers and disseminations hosted in quartz veins (see Figure 2B).
Moderately
elevated historical Cu and Au rock grab samples (up to 0.09% Cu and 0.44 g/t Au) were visited at the Long Lake Hills target area,
located 2.7 miles northeast of the Whistler gold-copper deposit. Reconnaissance mapping identified diorite porphyry with strong phyllic
alteration, including outcropping ‘D- and B-veins’ which are diagnostic of porphyry Au-Cu mineralization (see Figure 2C).
Two diamond core holes (WH26-13 and -16) were subsequently drilled to test this zone at depth (see news release dated September 22, 2026;
assays pending).
The
Long Lake Hills and Snow–Canyon Ridge prospects are being examined for their potential to extend the ‘Whistler Orbit’,
a classic porphyry cluster, up to 2 to 5 miles towards the northeast and north, respectively. Pending receipt of assays, additional systematic
mapping, prospecting, and sampling, and potentially geophysical survey extensions and drilling, will be assessed.
Muddy
Creek
Located
approximately 10 miles southwest of the Whistler gold-copper deposit, the 2026 field work at Muddy Creek aimed to verify and expand upon
historical and 2025 field campaigns (see news releases dated June 16, 2025, August 27, 2025, and October 13, 2025). The 2025 field campaigns
identified new zones of increased quartz vein density hosted in altered volcano-sedimentary rocks peripheral to a large granodiorite
intrusion (the ‘contact zone’). Mapping and prospecting completed during 2026 field work identified new high-density quartz
vein zones along the contact zone, located 1.7 miles to the west from where high-density quartz veining was first identified in 2025,
which greatly expands the extent of the mineral system mapped to date. The geological context, sheeted quartz veining, and elemental
association of Au with As, Bi, and Sb are key diagnostic features of intrusion-related gold systems (e.g. Kinross Gold Corporation’s
Fort Knox gold mine and Snowline Gold Corp.’s Valley gold deposit).
Numerous
high-grade Au rock grabs have been collected historically over the prospect area, up to a peak assay of 111.5 g/t Au. The average gold
value from 285 rocks collected historically over the Muddy Creek prospect is 3.03 g/t Au. Many of the rock samples collected are selective,
comprising rock grab samples from 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, we believe, broadly confirms a large
area of potential bedrock mineralization.
Pending
additional positive assays from the 2026 rock grab sampling program, work will continue to focus on areas of high-density quartz veining
along contact zones between the host granodiorite intrusion and surrounding country rocks – a classic setting for intrusion-related
gold mineralization.
Island
Mountain
The
Island Mountain mineral system is located 15 miles south of the Whistler gold-copper deposit. It comprises a gold-copper porphyry system
associated with Late Cretaceous diorite and monzonite intrusions similar to the Whistler deposit but differs from the Whistler mineral
system in that Island Mountain is more akin to the reduced sub-class of porphyry copper-gold deposits. The currently drill-delineated
gold and copper resource estimate is hosted within the ‘Breccia Zone’, comprising intense sodic-calcic alteration and pyrrhotite
mineralization within a diorite to monzonitic intrusive complex.
Reconnaissance
mapping over zones of historical elevated gold and copper rock grab samples (up to 17.25 g/t Au) indicates potential to expand the footprint
of the Breccia Zone mineralization to the northwest of the existing drill-delineated mineral resource. Mapping also evaluated gold-copper
geochemical anomalies (peaking at 4.86 g/t Au, see Figure 1) located approximately 1 to 2 miles north of the Breccia Zone, and identified
several untested geophysical anomalies, potentially expanding the search radius for new discoveries, which we believe will be a focus
of future field campaigns in 2027.
Technical
Information
For
further information regarding the Whistler Project, including the mineral resource estimate disclosed herein, please see the technical
report summary titled “Whistler Gold-Copper Project, S-K 1300 Technical Report Summary and Initial Assessment with Economic Analysis,
Alaska, United States of America” (the “S-K 1300 Report”) prepared under subpart 1300 of Regulation S-K under the U.S.
Securities Act of 1933 (“S-K 1300”) and the Canadian National Instrument 43-101 (“NI 43-101”) technical report
titled “Whistler Gold-Copper Project, NI 43-101 Technical Report and Preliminary Economic Assessment”, each dated effective
March 2, 2026. The S-K 1300 Report is available under the Company’s profile at www.sec.gov and the NI 43-101 Report is available
under its profile at www.sedarplus.ca.
Mineral
resources are not mineral reserves and do not have demonstrated economic viability. There is no certainty that all or any part of the
mineral resources estimated for the Whistler Project will be converted into mineral reserves. Inferred mineral resources are subject
to greater uncertainty than indicated mineral resources and it cannot be assumed that all or any part of an inferred mineral resource
will be upgraded to a higher category.
Gold-equivalent
(“AuEq”) figures reported in this news release are based on the gold and copper grades, metal prices, and metallurgical recovery
assumptions set out in the S-K 1300 Report and the NI 43-101 Report. Readers are referred to those reports for the individual metal grades,
assumed metal prices, recovery assumptions, and the formula used to derive the reported AuEq figures.
Tim
Smith, P.Geo., Chief Executive Officer of the Company, has supervised the preparation of this news release and has reviewed the additional
scientific and technical information contained herein. Mr. Smith is a qualified person as defined under NI 43-101 and S-K 1300.
About
U.S. GoldMining Inc.
U.S.
GoldMining Inc. is an exploration and development company focused on advancing the 100% owned Whistler Gold-Copper Project, located 105
miles (170 kilometers) northwest of Anchorage, Alaska, U.S.A. The Whistler Project consists of several gold-copper porphyry deposits
and exploration targets within a large regional land package entirely on State of Alaska mining claims totaling approximately 53,700
acres (217.5 square kilometers).
Visit
www.usgoldmining.us for more information.
For
additional information, please contact:
U.S.
GoldMining Inc.
Alastair
Still, Chair
Tim
Smith, Chief Executive Officer
Telephone
Toll Free: 1-833-388-9788
Email:
info@usgoldmining.us
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 the United States federal securities laws and “forward-looking information” within
the meaning of applicable Canadian securities laws (collectively, “forward-looking statements”). Such statements include
statements with regard to the Company’s plans and expectations regarding the Whistler Project, future work programs, the potential
to expand exploration targets and mineralization and its future exploration and development potential, and expectations regarding future
exploration plans. Words such as “expects”, “anticipates”, “plans”, estimates” and “intends”
or similar expressions are intended to identify forward-looking statements. Forward-looking statements are based on U.S. GoldMining’s
current expectations and are subject to inherent uncertainties, risks and assumptions that are difficult to predict and involve known
and unknown risks, uncertainties and other factors, which may cause the actual results, performance or achievements of the Company to
be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements.
Such risks and other factors include, among others, fluctuating commodity prices, risks inherent with mineral resource estimation generally,
economic risks, changing economic factors, variations in the underlying assumptions associated with the estimation or realization of
mineral resources, the availability of capital to fund programs and future development work, accidents, labor disputes and other risks
of the mining industry including, without limitation, those associated with the environment, delays in obtaining governmental approvals
or permits, title disputes other risks inherent in the exploration and development of mineral properties and the other risk factors set
forth in the Company’s filings with the U.S. Securities and Exchange Commission at www.sec.gov and Canadian Securities Administrators
at www.sedarplus.ca. Although the Company has attempted to identify important factors that could cause actual actions, events or results
to differ materially from those described in forward-looking statements, there may be other factors that cause actions, events or results
not to be as anticipated, estimated or intended. Accordingly, readers should not place undue reliance on forward-looking statements contained
in this news release. Forward-looking statements contained in this news release are made as of this date, and U.S. GoldMining does not
undertake any duty to update such information except as required under applicable law.