ANCHORAGE, Alaska, Feb. 10,
2025 /PRNewswire/ - U.S. GoldMining Inc.
(NASDAQ: USGO) ("U.S. GoldMining" or the
"Company") is pleased to announce new assay results
from the 2024 confirmatory diamond core drilling program completed
at the Whistler Gold-Copper Project (the "Project") in
Alaska, U.S.A.
The results reported in this news release highlight
WH24-05, which was drilled adjacent to the Raintree West
Deposit (the "Raintree Deposit"). The drilling
intercepted multiple zones of high-grade gold and silver
polymetallic mineralization approximately 500 meters south of any
prior drilling at the deposit.
Selected Highlights:
- Main Zone composite intercept of 138.0 meters
(m) at 0.99 grams per tonne (g/t) gold
equivalent (AuEq)* comprising 0.89 g/t
gold (Au) and 0.05 percent (%) copper (Cu),
plus 17.57 g/t silver (Ag), 0.44% lead (Pb) and 0.95%
zinc (Zn) (elevated Ag, Pb and Zn grades are excluded in the
AuEq calculations), from 635.0 m to
773.0 m down hole.
- Including higher-grade individual intercepts:
- 26 m at 1.48 g/t
AuEq (1.36 g/t Au, 0.06% Cu) plus 15.38 g/t Ag, 0.69% Pb
and 1.61% Zn
- 34 m at 1.65 g/t
AuEq (1.49 g/t Au, 0.08% Cu) plus 19.95 g/t Ag, 0.81% Pb
and 1.35% Zn
- 18 m at 1.93 g/t
AuEq (1.70 g/t Au, 0.13% Cu) plus 66.33 g/t Ag, 0.62% Pb
and 1.84% Zn
- The drill intercept represents a relatively new style
of mineralization - high-grade gold and silver
polymetallic veins - with only one other intercept previously
drilled at the Raintree Deposit:
- This new discovery validates the Company's exploration strategy
of exploring the Project to maximize its resource potential.
Additional follow-up drilling is planned this coming summer.
*See Table 1 for further information.
Tim Smith, Chief Executive
Officer of U.S. GoldMining, commented: "This last drill hole in
2024 was designed to build on the successful season the Company had
at the Whistler Deposit, which included the expansion of the
western high-grade core at that deposit and returned results
including 458 m at 0.75 g/t AuEq (see
February 3, 2025 press release). For
the final core hole drilled in 2024, we returned to the Raintree
Prospect with the objective to drill test a very compelling
exploration target, comprising a previously undrilled porphyry
intrusion coupled with a large high intensity IP chargeability
anomaly located 500 meters south of the existing Raintree Deposit.
While the porphyry-style alteration and veining observed in the
upper part of drill hole WH24-05 is encouraging for an early-stage
drill prospect, the high-grade gold and silver in polymetallic
veins intersected in the lower part of the drill hole significantly
exceeded our expectations.
The mineralization is visually impressive, consisting of
multiple quartz-carbonate veins with abundant coarse base metal
sulphides over tens of meters down-hole. Drill core assays
highlight high-grade gold and silver values, peaking at 7.15 g/t Au
and 189 g/t Ag, along with peak base metal values of up to 5.4% Zn
and 3.6% Pb, sampled over individual 2 meter core length intervals.
The Company's geologists are excited to get back into the field
this coming summer to undertake follow-up drilling to further
explore, delineate and extend this new zone of mineralization,
which could potentially offer additional and alternative metal
resources to the existing Project mineral resource estimate.
The Company is now compiling all exploration results and
geological datasets collected during the 2024 drill season to
update its exploration target prioritization and commence planning
for the upcoming 2025 drill season to continue the re-discovery of
the Whistler Project."
2024 Drilling Program Summary
The Company completed six diamond core holes for 4,006 meters
during the 2024 field season at the Project. In addition to four
drill holes for 2,784 meters completed at the Whistler Deposit, two
drill holes for 1,224 meters were completed at the Raintree
Deposit (see Figure 1), located approximately
one kilometer east of the Whistler Deposit. With this news release,
all assay results from the 2024 field season are now reported.
The Raintree component of the Project mineral resource estimate
comprises both open pit constrained and underground delineated
deposits (see news release dated October 7,
2024).
Raintree Open Pit at US$10/t cutoff: 8.9 Mt at 0.63 g/t AuEq (0.46 g/t
Au, 0.08% Cu and 4.81 g/t Ag) for 180,000 oz AuEq (131 Koz Au, 16 Mlbs Cu and 1.38 Moz Ag) classified as indicated, and 15.1 Mt at
0.69 g/t AuEq (0.55 g/t Au, 0.06% Cu and 4.36 g/t Ag) for 335,000
oz AuEq (267 Koz Au, 21 Mlbs Cu and
2.11 Moz Ag) classified as
inferred.
Raintree Underground at US$25/t cutoff: 3.1 Mt at 1.03 g/t AuEq (0.79 g/t
Au, 0.13% Cu and 4.49 g/t Ag) for 101,000 oz AuEq (78 Koz Au, 9 Mlbs Cu and 0.44 Moz Ag) classified as indicated, and 40.4 Mt at
0.98 g/t AuEq (0.76 g/t Au, 0.12% Cu and 3.31 g/t Ag) for 1,275,000
oz AuEq (994 Koz Au, 103 Mlbs Cu and
4.3 Moz Ag) classified as
inferred.
The Raintree Deposit lies within the broader 'Raintree Prospect'
area, which in addition to the Raintree Deposit itself contains
several drill prospects and exploration targets over a 2 km
diameter, including 'Raintree North', 'Raintree East' and 'Raintree
South'. Compared to the Whistler Deposit, which has over 22,000
meters of drilling, the entire Raintree Prospect comprises just
5,190 meters of historic drilling. The Company's strategy to date
has been to focus on confirmatory drilling and studies to delineate
and, where possible, expand the open pit portion of the Whistler
and Raintree Deposits. With drill hole WH24-05, the Company has
ventured into new terrane, with exploration into a never before
drilled section of the Raintree Prospect to test newly identified
conceptual targets south of the Raintree open pit portion.
Raintree Prospect - Geology
The Raintree Prospect area is characterized by a swarm of small
intrusive diorite porphyry bodies - dykes, sills and stocks -
of the Whistler Intrusive Suite (WIS), hosted within a sequence of
andesite lavas and related volcaniclastic rocks. This geological
setting contrasts to the Whistler Deposit, a large (600 m x 800 m)
ovoid shaped WIS diorite porphyry intrusion, hosted within basement
sedimentary rocks of the Mesozoic Kahiltna Formation. The Raintree
Prospects are interpreted to have formed at a higher stratigraphic
level relative to the Whistler Deposit. Additionally, the Raintree
porphyry dykes and stocks intersected to date are distinguished by
their lower magnetite content compared to the highly magnetic
diorite porphyry of the Whistler Deposit.
The Raintree Deposit comprises both porphyry style Au-Cu-Ag
mineralization and overprinting polymetallic vein style
Au-Ag-Pb-Zn±Cu mineralization. This contrasts with mineralization
at the Whistler Deposit which is almost entirely made up of
porphyry style Au-Cu-Ag mineralization. At Raintree Deposit,
porphyry-style mineralization is confined to the porphyry diorite
intrusives (dykes and stocks), comprising B type veins and
disseminated sulphide mineralization like the Whistler Deposit.
Whereas late-stage polymetallic vein style mineralization occurs in
both the porphyry intrusive rocks and andesite extrusive rocks and
is characterized by disseminated and semi-massive pyrite, galena,
sphalerite, tetrahedrite, and chalcopyrite in quartz-carbonate
veins. Vein contacts are generally sharp and distinct with
associated narrow sericite and chlorite alteration halos.

An initial 2024 confirmatory infill drill hole at Raintree West
- WH24-01 - aimed to validate the current geological model
and to also test potential to expand the existing resource. WH24-01
was drilled into the area of the constraining pit shell for the
Raintree West Open Pit deposit, with the objective of collecting
additional information about the style, geometry, continuity and
controls on mineralization hosted therein. As previously
reported (see news release dated September 30, 2024), WH24-01 intersected
61.4 m at 0.53 g/t AuEq (0.36 g/t Au,
0.09% Cu, 4.4 g/t Ag) comprising A & B type vein and
disseminated sulphide mineralization hosted within diorite
porphyry. In addition, WH24-01 intersected multiple occurrences of
porphyry-distal D-style polymetallic veins, including a broad zone
of veining which returned 17.0 m at
0.33 g/t Au, 0.07% Cu, 42.0 g/t Ag, 0.33% Pb and 0.75% Zn from
249 m downhole, and which included a
higher grade interval of 4.0 m at
0.78 g/t Au, 0.22% Cu, 171.6 g/t Ag, 1.19% Pb and 2.53% Zn.
The 2024 Raintree Prospect drilling is the first exploration
completed in the area since 2011; therefore, the Company has taken
the approach to systematically analyze prior exploration and
geological data across the mineral system. It is noted that
previous shallow scout drilling immediately south of the currently
defined Raintree Deposit identified strong phyllic alteration
associated with diorite porphyries and hydrothermal breccias
intruding andesitic volcaniclastic rocks. Both the diorite and
volcanic rocks are cross-cut by D-style veinlets, which was
interpreted as being potentially indicative of a nearby porphyry
center. The target is also supported by geophysical evidence
including a broad IP chargeability anomaly, which is generally
interpreted to be associated with phyllic (quartz-sericite-pyrite)
alteration.
WH24-05 Drilling Results Discussion
WH24-05 subsequently aimed to explore for additional
mineralizing dykes associated with the Raintree dyke swarm,
immediately adjacent to (south of) the currently defined Raintree
Deposit. Drilling intersected multiple porphyry intrusions (dykes)
within a thick package of andesite extrusives and associated
volcaniclastic rocks, including several zones of low-grade porphyry
style mineralization in the upper section of the drill hole.
Drilling was extended to depth to test the deeper IP chargeability
anomaly, subsequently intersecting several zones of porphyry-distal
polymetallic D-veining, including the following drill
intercepts:
- Main Zone intercept of 138.0 m at 0.99 g/t
AuEq (0.89 g/t Au, 0.05 % Cu), plus 17.57 g/t Ag,
0.44% Pb and 0.95% Zn, from 635.0 m
downhole; which contains three higher-grade vein zones:
- 26 m at 1.48 g/t
AuEq (1.36 g/t Au, 0.06% Cu) plus 15.38 g/t Ag, 0.69% Pb
and 1.61% Zn, from 635 m downhole;
and
- 34 m at 1.65
g/t AuEq (1.49 g/t Au, 0.08% Cu) plus 19.95 g/t Ag,
0.81% Pb and 1.35% Zn, from 681 m
downhole; and
- 18 m at 1.93
g/t AuEq (1.70 g/t Au, 0.13% Cu) plus 66.33 g/t Ag,
0.62% Pb and 1.84% Zn, from 755 m
downhole.
The gold and silver bearing polymetallic veins intersected in
WH24-05 comprise late-stage quartz-carbonate veins with
semi-massive pyrite, galena, sphalerite, tetrahedrite and
chalcopyrite. Some of the polymetallic veins intersected in WH24-05
exhibit sub-epithermal textures. The mineralized veins are oriented
moderately to steeply dipping, striking NE-SW and NW-SE
orientations forming a conjugate set. The mineralized envelope
geometry is interpreted to be likely parallel to the overall NW-SE
orientation of the Raintree Deposit mineralization, which will be
confirmed by follow-up drilling.
The Company is currently assessing the significance of this
relatively new style of vein-hosted mineralization intersected in
WH24-05. Most porphyry mineral systems contain similar late-stage
polymetallic veins, which range from distal to more proximal
D-style veins. These veins themselves may be of direct exploration
interest or may provide vectors to additional nearby porphyry style
mineralization. Drill core composites have been collected to
undertake petrographic analysis and metallurgical test work to
determine the gold and silver deportment and metal recoverability.
Additional drilling is planned for this coming summer to further
explore and delineate this new discovery and if applicable,
incorporate this newly identified mineralization into the Raintree
Deposit.
Table 1 –Project drill assay intercepts from the 2024
drilling program, received as of February
10, 2024. Bold intervals correspond with those reported in
the 'highlights' section above.
Hole
Number
|
Interval
From
(m)
|
Interval
To
(m)
|
Core
Length
(m)
|
Gold
Grade
(g/t)
|
Copper
Grade
(%)
|
Silver
Grade
(g/t)
|
AuEq
(g/t)*
|
Lead
Grade
(%)
|
Zinc
Grade
(%)
|
WH23-03-EXT
|
0.41
|
717.00
|
716.59
|
0.68
|
0.15
|
1.40
|
0.93
|
-
|
-
|
Including
|
7.00
|
659.46
|
652.46
|
0.73
|
0.16
|
1.50
|
1.00
|
-
|
-
|
Including
|
131.00
|
307.00
|
176.00
|
1.24
|
0.19
|
1.66
|
1.55
|
-
|
-
|
And
|
373.50
|
423.00
|
49.50
|
0.92
|
0.10
|
1.82
|
1.10
|
-
|
-
|
And
|
441.00
|
457.00
|
16.00
|
1.03
|
0.20
|
1.64
|
1.36
|
-
|
-
|
And
|
480.00
|
501.00
|
21.00
|
0.80
|
0.35
|
2.11
|
1.37
|
-
|
-
|
And
|
523.00
|
539.00
|
16.00
|
0.83
|
0.30
|
1.14
|
1.31
|
-
|
-
|
And
|
575.00
|
632.00
|
57.00
|
1.07
|
0.17
|
1.18
|
1.36
|
-
|
-
|
WH23-03-EXT
|
698.03
|
717.00
|
18.97
|
0.52
|
0.11
|
1.02
|
0.70
|
-
|
-
|
WH24-01
|
107.00
|
109.00
|
2.00
|
0.45
|
-
|
8.60
|
0.58
|
0.61
|
3.07
|
WH24-01
|
147.00
|
151.00
|
4.00
|
0.28
|
-
|
7.10
|
0.42
|
0.44
|
1.20
|
WH24-01
|
159.00
|
161.00
|
2.00
|
0.64
|
-
|
4.50
|
0.72
|
0.29
|
1.59
|
WH24-01
|
249.00
|
266.00
|
17.00
|
0.33
|
0.07
|
41.97
|
0.45
|
0.33
|
0.75
|
Including
|
249.00
|
253.00
|
4.00
|
0.78
|
0.22
|
171.55
|
1.12
|
1.19
|
2.53
|
WH24-01
|
280.60
|
300.00
|
19.40
|
0.31
|
-
|
1.81
|
0.38
|
0.12
|
0.40
|
Including
|
284.00
|
286.00
|
2.00
|
1.23
|
-
|
4.70
|
1.32
|
0.37
|
1.27
|
WH24-01
|
311.00
|
372.38
|
61.38
|
0.36
|
0.09
|
4.43
|
0.53
|
0.14
|
0.39
|
Including
|
321.00
|
362.00
|
41.00
|
0.41
|
0.11
|
5.43
|
0.61
|
0.15
|
0.49
|
WH24-02
|
227.00
|
500.96
|
273.96
|
0.48
|
0.12
|
0.86
|
0.71
|
-
|
-
|
Including
|
291.00
|
444.00
|
153.00
|
0.65
|
0.14
|
0.74
|
0.90
|
-
|
-
|
Including
|
291.00
|
411.00
|
120.00
|
0.72
|
0.16
|
0.83
|
1.00
|
-
|
-
|
Including
|
297.00
|
337.00
|
40.00
|
0.82
|
0.25
|
1.13
|
1.28
|
-
|
-
|
And
|
357.00
|
377.00
|
20.00
|
0.96
|
0.16
|
0.93
|
1.26
|
-
|
-
|
WH24-03
|
40.00
|
52.74
|
12.74
|
1.30
|
0.35
|
2.37
|
1.96
|
-
|
-
|
|
385.08
|
525.00
|
139.92
|
0.21
|
0.14
|
0.97
|
0.47
|
-
|
-
|
Including
|
401.00
|
429.00
|
28.00
|
0.41
|
0.24
|
1.74
|
0.85
|
-
|
-
|
|
643.00
|
679.00
|
36.00
|
0.08
|
0.12
|
1.08
|
0.29
|
-
|
-
|
|
731.00
|
767.00
|
36.00
|
0.20
|
0.11
|
1.23
|
0.40
|
-
|
-
|
|
868.00
|
917.00
|
49.00
|
0.18
|
0.05
|
1.90
|
0.28
|
-
|
-
|
WH24-04
|
91.00
|
682.00
|
591.00
|
0.37
|
0.15
|
1.48
|
0.66
|
-
|
-
|
Including
|
224.00
|
682.00
|
458.00
|
0.46
|
0.16
|
1.66
|
0.75
|
-
|
-
|
Including
|
260.00
|
308.00
|
48.00
|
0.61
|
0.34
|
2.19
|
1.23
|
-
|
-
|
And
|
406.00
|
456.00
|
50.00
|
0.73
|
0.13
|
1.50
|
0.98
|
-
|
-
|
WH24-05
|
306.00
|
325.00
|
19.00
|
0.79
|
0.03
|
17.70
|
0.87
|
0.73
|
1.72
|
|
489.00
|
508.50
|
19.50
|
0.33
|
0.02
|
7.76
|
0.41
|
0.51
|
1.20
|
|
603.50
|
773.00
|
169.50
|
0.77
|
0.04
|
15.38
|
0.86
|
0.40
|
0.86
|
Including
|
635.00
|
773.00
|
138.00
|
0.89
|
0.05
|
17.57
|
0.99
|
0.44
|
0.95
|
Including
|
635.00
|
661.00
|
26.00
|
1.36
|
0.06
|
15.38
|
1.48
|
0.69
|
1.61
|
And
|
681.00
|
715.00
|
34.00
|
1.49
|
0.08
|
19.95
|
1.65
|
0.81
|
1.35
|
Including
|
699.00
|
715.00
|
16.00
|
2.90
|
0.14
|
38.59
|
3.16
|
1.47
|
2.38
|
And
|
755.00
|
773.00
|
18.00
|
1.70
|
0.13
|
66.33
|
1.93
|
0.62
|
1.84
|
Including
|
763.00
|
773.00
|
10.00
|
2.82
|
0.22
|
113.74
|
3.21
|
1.00
|
3.00
|
Notes:
WH23-03-EXT drilled down-plunge to test the deeper extents
of mineralization within the Whistler Deposit eastern high-grade
core, therefore the mineralized intervals reported are not
representative of true width. The mineralized intercepts within
WH24-01 are estimated to be approximately two-thirds of true width.
WH24-02 and WH24-03 drilled oblique to dip and strike to test the
vertical profile of mineralization, therefore the mineralized
intervals reported are not representative of true width. WH24-04
tested obliquely across strike and to depth to test the vertical
profile of mineralization, thus the mineralized intervals reported
are estimated to be approximately half to two-thirds of true width.
WH24-05 tested obliquely across strike and dip, thus mineralized
intervals reported are estimated to be approximately two-thirds of
true width.
*AuEq is calculated consistent with the methodology
outlined in the technical reports "S-K 1300 Technical Report
Summary Initial Assessment for the Whistler Project, South Central Alaska" with an effective date
of September 12, 2024, and the
technical report titled "NI 43-101 2024 Updated Mineral Resource
Estimate for the Whistler Project, South
Central Alaska" with an effective date of September 12, 2024, each available under the
Company's profiles at www.sec.gov and www.sedarplus.ca
(collectively, the "Technical Reports").
Specifically, for drilling reported prior to the 2024 MRE
update (WH23-03-EXT and WH24-01): below 10g/t Ag: AuEq=Au +
Cu*1.5733 +0.0108Ag, and above 10g/t Ag: AuEq=Au + Cu*1.5733. For
drilling reported subsequent to the 2024 MRE update (WH24-02, -03,
-04 & -05): below 10g/t Ag: AuEq=Au + (Cu%*1.771) +
(Ag*0.0113), and above 10g/t Ag: AuEq=Au + (Cu%*1.771). AuEq
calculations do not include Pb and Zn as it is unknown whether
these metals can be recovered.
Table 2 –Project 2023 & 2024 drill hole collar
location coordinates.
Hole
Number
|
Easting
Meters
(UTM
Zone 18)
|
Northing
Meters
(UTM
Zone 18)
|
Elevation
(m above
sea level)
|
Depth
(m)
|
Azimuth
(Degrees)
|
Dip
(Degrees)
|
Status
|
WH23-01
|
518,782
|
6,871,260
|
886.0
|
467.87
|
140.80
|
- 49.0
|
All assays
received
|
WH23-02
|
518,779
|
6,871,253
|
886.0
|
605.64
|
229.20
|
- 60.1
|
All assays
received
|
WH23-03-EXT
|
518,776
|
6,871,253
|
886.0
|
874.50
|
189.20
|
- 82.9
|
All assays
received
|
WH23-04
|
520,193
|
6,869,142
|
352.0
|
560.83
|
134.80
|
- 78.0
|
All assays
received
|
WH24-01
|
520,494
|
6,871,260
|
497.0
|
445.77
|
14.63
|
- 46.9
|
All assays
received
|
WH24-02
|
518,452
|
6,871,362
|
849.0
|
716.30
|
135.43
|
- 75.2
|
All assays
received
|
WH24-03
|
518,746
|
6,871,335
|
859.0
|
961.9
|
309.69
|
- 80.1
|
All assays
received
|
WH24-04
|
518,680
|
6,871,248
|
876.0
|
832.20
|
185.85
|
- 78.0
|
All assays
received
|
WH24-05
|
520,495
|
6,871,258
|
497.0
|
777.85
|
184.37
|
- 55.3
|
All assays
received
|
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 details of the Project and the mineral resource reports
referenced herein, please refer to the Technical Reports.
Data Verification
For the Project drill core sampling program, samples were taken
from NQ/HQ diameter core by sawing the drill core in half, with
one-half sent to Bureau Veritas Commodities Canada Ltd.
("BV") in Fairbanks,
Alaska, for sample preparation, then to BV's analytical
laboratory in Vancouver, Canada
for assaying, and the other half of the core is retained at
the site for future reference. Sample lengths downhole were
generally 2.0 m, except where samples
were taken to honor geological contacts.
BV is a certified commercial laboratory and is independent
of U.S. GoldMining. The Company has implemented a quality assurance
and quality control program for the sampling and analysis of drill
core samples, including duplicates, mineralized standards and blank
samples for each batch of core samples. The gold analyses were
completed by lead collection fire assay fusion with AAS finish
(FA430 method) on 30 grams test weight. Copper, silver and other
base metals assays (total suite of 45 elements) were assayed by
4-acid digestion and ICP-MS analysis (MA200 method) on 0.25 grams
test weight.
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). The Whistler Project Mineral Resource Estimate
comprises 294 Mt at 0.68 g/t AuEq for 6.48 Moz AuEq Indicated, plus
198 Mt at 0.65 g/t AuEq for 4.16 Moz AuEq Inferred.
Visit www.usgoldmining.us for more information, including
high resolution figures.
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 expectations regarding the Project, including planned
future programs. 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, the actual results of future exploration may
not confirm expectations, variations in the underlying assumptions
associated with the estimation or realization of mineral resources,
the availability of capital to fund programs, 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.
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