News release
NEWS RELEASE
January 6, 2026
NR 26-01
www.sitkagoldcorp.com
SITKA DRILLS 156.9 METRES OF 1.00 G/T GOLD,
INCLUDING 94.0 METRES OF 1.41 G/T GOLD AND 38.0
METRES OF 2.03 G/T GOLD, SIGNIFICANTLY EXPANDING
KNOWN MINERALIZATION AT THE RHOSGOBEL
DISCOVERY, RC GOLD PROJECT, YUKON
● Results from an additional 11 diamond drill holes expand the mineralized envelope at
Rhosgobel by 400 m with multiple holes returning >100 gram metres (g/t*m) of gold
● Hole DDRCRG-25-027 returned 156.9 m of 1.00 g/t Au, including 94.0 m of 1.41 g/t
Au, 38.0 m of 2.03 g/t Au and 2.0 m of 19.30 g/t Au
● Hole DDRCRG-25-024 returned 146.7 m of 1.05 g/t Au, including 12.0 m of 3.89 g/t
Au and 3.0 m of 8.67 g/t Au
● Hole DDRCRG-25-019 returned 110.0 m of 1.01 g/t Au, within a larger interval of
126.0 m of 0.93 g/t Au from surface
● Assay results from drilling confirm gold mineralization along a strike length of 975
m with visible gold observed within sheeted quartz veins over the entire 1.1 km of
strike length drilled in 2025 with assays pending from the remaining 15 drill holes
● Tungsten mineralization associated with gold grades continues to be observed
VANCOUVER, CANADA – January 6, 2026: Sitka Gold Corp. (“Sitka” or the
“Company”) (TSX-V:SIG) (FSE:1RF) (OTCQB:SITKF) is pleased to announce additional
strong gold results from diamond drilling completed at the Rhosgobel discovery at its 100%
owned, road accessible RC Gold Project (“RC Gold” or the “Project”) located within the
Yukon’s prolific Tombstone Gold Belt. Analytical results for drill holes DDRCRG-25-018
through DDRCRG-25-028 have been received and compiled and are reported herein.
Results from these drill holes have significantly expanded the known mineralized zone at
Rhosgobel, a reduced intrusion-related gold deposit target located within the Clear Creek
Intrusive Complex (CCIC; see Figures 9 and 10), with strong gold intercepts such as 156.9
m of 1.00 g/t gold, including 94.0 metres of 1.41 g/t gold and 38.0 metres of 2.03 g/t
gold returned in DDRCRG-25-027 and 146.7 m of 1.05 g/t gold, including 12.0 metres of
3.89 g/t gold returned in DDRCRG-25-024. Tungsten mineralization also continues to be
observed at Rhosgobel (see news release dated September 18, 2025). The mineralized
zone at Rhosgobel begins at surface and remains open in all directions. Mineralization
typical of Reduced-Intrusion Related Gold Systems (RIRGS) consisting of sheeted quartz
veining has been observed in drilling along a strike length of 1.1 km and to a depth of over
400 metres. Visible gold within sheeted quartz veins has been observed across the entire
1.1 km strike that has been drilled to date (see Figures 2 and 4). An additional 15 drill holes
completed at Rhosgobel are currently pending release.
Table 1: Gold assay highlights for this release (see Table 2 for details)
Hole ID
DDRCRG-25-027
Zone
From (m)
To (m)*
Length (m)
Gold (g/t)
93.0
249.9
156.9
1.00
including
174.0
212.0
38.0
2.03
including
142.0
236.0
94.0
1.41
Rhosgobel
DDRCRG-25-024
Rhosgobel
21.3
168.0
146.7
1.05
DDRCRG-25-019
Rhosgobel
6.0
132.0
126.0
0.93
22.0
132.0
110.0
1.01
10.3
102.0
91.8
0.90
57.0
102.0
45.0
1.18
including
DDRCRG-25-020
including
Rhosgobel
DDRCRG-25-026
Rhosgobel
including
DDRCRG-25-021
Rhosgobel
And
DDRCRG-25-022
Rhosgobel
And
DDRCRG-25-028
Rhosgobel
and
DDRCRG-25-018
Rhosgobel
5.8
81.0
75.2
1.04
29.0
54.0
25.0
2.08
153.0
200.0
47.0
1.00
171.0
204.0
33.0
1.07
18.4
118.8
104.0
0.70
50.0
84.0
34.0
1.23
9.1
36.0
26.9
1.01
52.0
61.5
9.5
1.02
85.0
102.0
17.0
1.05
*Intervals are drilled core length, as insufficient drilling has been completed at this time to determine true widths.
“Our Rhosgobel discovery continues to impress with the latest results from our drilling
efforts returning exceptional gold values from surface and further expanding the known
strike of mineralization,” stated Cor Coe, CEO and Director of Sitka Gold. “Drilling to date at
Rhosgobel has confirmed a large zone of higher-grade gold mineralization that begins at
surface across a 975 km strike length where 19 of the 28 drill holes released to date have
returned intersections exceeding 100 gram-metres of gold. With reduced intrusion-related
gold style mineralization observed in all drill holes completed to date over the initial 1.1 km
strike length tested, which remains open in all directions, Rhosgobel is quickly shaping up
as one of the most significant new gold discoveries made in 2025 and the third major gold
deposit discovered within the Clear Creek Intrusive Complex with the potential to host a
multi-million ounce gold resource. We look forward to compiling and releasing the remaining
15 holes from Rhosgobel, along with the remaining drill holes from the Contact, Pukelman
and Bearpaw targets. With up to 60,000 metres of fully-funded drilling planned for this year,
Sitka is well positioned to rapidly advance this emerging gold camp as we focus on
continued expansion of known deposits and new discoveries within the district-scale, target
rich RC Gold Project.”
Figure 1: A cross section showing gold assay results of DDRCRG-25-027 which returned 156.9
m of 1.00 g/t Au, including 94.0 m of 1.41 g/t Au, 38.0 m of 2.03 g/t Au and 2.0 m of
19.30 g/t Au, along with instances of visible gold observed in the drill core (yellow stars).
Figure 2: A plan map of drilling at the Rhosgobel discovery within the gold-in-soil anomaly
of the target area.
Figure 3: A cross section showing gold assay results of DDRCRG-25-022 and
DDRCRG-25-024, which returned 146.7 m of 1.05 g/t Au, including 12.0 m of 3.89 g/t Au
and 3.0 m of 8.67 g/t Au, along with instances of visible gold observed in the drill core
(yellow stars).
Figure 4: A plan map showing drilling completed at Rhosgobel within the larger 1.5 x 2.0 km
target area as outlined by the strong gold-in-soil anomaly discovered on surface. Mineralization
at Rhosgobel remains open in all directions.
Figure 5: Examples of visible gold (VG) observed in drill core at Rhosgobel. Click HERE to
see additional images of VG from Rhosgobel.
Figure 6: Example of sheeted quartz - tourmaline veins in faulted and oxidized megacrystic
quartz monzonite in DDRCRG-25-027 from the 38.0 m interval from 174.0 m containing
1.03 g/t Au, including 2.0 m of 19.3 g/t Au from 188.0 m
RHOSGOBEL DRILLING
To date, 43 holes totalling 12,722 m have been completed at Rhosgobel. All holes drilled
have intersected significant reduced intrusion-related gold style mineralization including
centimetre-scale,
sheeted,
quartz
veins
and
larger,
metre-scale
quartz,
and
quartz-tourmaline veins (and breccias) cutting the feldspar megacrystic quartz monzonite
intrusion. Visible gold has been observed within all styles of veins and is often associated
with bismuthinite, scheelite, and molybdenite. Drilling to date has traced gold mineralization
over a strike length of approximately 1.1 kilometres within a large 2.0 km x 1.5 km surface
signature represented by a gold-in-soil anomaly with values up to >500 ppb (Figure 4). Gold
mineralization at Rhosgobel begins at surface, extends to a depth of over 400 metres and
remains open in all directions. Nineteen of the first 28 diamond drill holes reported from
Rhosgobel, including the two discovery holes drilled in 2024, have intersected >100
gram-metres gold (g/t Au*m). Assays are currently pending for the remaining 15 holes
completed at Rhosgobel in 2025.
* While visible gold observations are very encouraging and confirm the presence of gold mineralization, they are not intended to imply potential gold
grades. Gold assays will be published after they are received from the lab for mineralized intervals in which visible gold particles were noted.
Table 2: Summary of significant assay results from this release
Hole ID
Zone
DDRCRG-25-027 Rhosgobel
Length Azimuth Dip
(m)
(°)
(°)
Gold
(g/t)
156.9
1.00
Including
142.0
236.0
94.0
1.41
Including
174.0
212.0
38.0
2.03
Including
186.0
192.0
6.0
7.58
Including
188.0
190.0
2.0
19.30
And
296.7
313.3
16.6
0.54
21.3
168.0
146.7
1.05
Including
25.0
37.0
12.0
3.89
Including
25.0
28.0
3.0
8.67
Including
36.0
37.0
1.0
12.40
Including
78.2
80.5
2.3
3.38
Including
107.6
108.8
1.2
3.66
And
137.0
139.0
2.0
4.95
6.0
132.0
126.0
0.93
Including
22.0
132.0
110.0
1.01
Including
53.0
57.0
4.0
2.99
Including
100.0
115.3
15.3
3.41
Including
110.0
113.4
3.4
7.71
10.3
102.0
91.8
0.90
10.3
35.0
24.8
0.93
DDRCRG-25-019 Rhosgobel
DDRCRG-25-020 Rhosgobel
Including
326.1
295.5
102.1
25
25
25
-50
Interval
(m)*
249.9
Rhosgobel
35
To
(m)
93.0
DDRCRG-25-024
332.3
From
(m)
-70
-60
-50
Including
57.0
102.0
45.0
1.18
Including
80.0
102.0
22.0
1.57
Including
90.0
92.0
2.0
5.58
5.8
81.0
75.2
1.04
Including
29.0
54.0
25.0
2.08
Including
29.0
45.0
16.0
2.44
And
87.0
89.0
2.0
1.71
30.0
31.5
1.5
1.14
And
41.0
43.0
2.0
3.11
And
53.0
63.0
10.0
1.12
And
153.0
200.0
47.0
1.00
Including
157.0
165.0
8.0
1.08
And
171.0
204.0
33.0
1.07
Including
198.0
200.0
2.0
6.16
18.4
118.8
104.0
0.70
Including
50.0
84.0
34.0
1.23
Including
58.0
60.0
2.0
3.58
Including
68.0
74.0
6.0
2.32
Including
104.0
106.0
2.0
2.23
And
132.0
134.0
2.0
1.02
9.1
181.0
171.9
0.50
Including
9.1
36.0
26.9
1.01
Including
52.0
61.5
9.5
1.02
Including
83.1
84.7
1.6
1.67
Including
133.1
139.0
5.9
1.06
Including
147.1
153.0
5.9
1.40
Including
173.0
175.0
2.0
1.10
Including
173.0
181.0
8.0
0.80
54.9
112.5
57.7
0.50
Including
85.0
102.0
17.0
1.05
And
383.5
384.9
1.4
1.14
DDRCRG-25-026
Rhosgobel
DDRCRG-25-021 Rhosgobel
DDRCRG-25-022
DDRCRG-25-028
DDRCRG-25-018
Rhosgobel
Rhosgobel
Rhosgobel
326.1
351.4
338.3
367.3
388.0
25
205
25
195
25
-50
-65
-55
-45
-50
DDRCRG-25-023 Rhosgobel
44.0
46.0
2.0
1.40
Including
66.0
68.0
2.0
2.74
And
214.0
216.0
2.0
1.52
And
287.0
289.0
2.0
3.31
And
305.0
307.0
2.0
1.82
And
354.0
358.0
4.0
2.67
And
391.0
395.0
4.0
1.14
And
409.0
411.0
2.0
2.28
17.8
20.0
2.2
1.34
And
63.6
65.0
1.4
1.33
And
193
199.0
6.0
1.43
And
320
322.0
2.0
1.08
And
361.0
363.0
2.0
2.49
And
377.0
379.0
2.0
1.89
DDRCRG-25-025
Rhosgobel
425.2
417.6
205
205
-65
-65
*Intervals are drilled core length, as insufficient drilling has been completed at this time to determine true widths.
TUNGSTEN AT RHOSGOBEL
Tungsten mineralization continues to be observed at Rhosgobel, suggesting it could be an
economic by-product of potential future production. The assay technique ME-MS41, is used
on all drill samples to test for additional trace elements associated with gold mineralization.
The technique provides only a partial digestion of the tungsten bearing mineral scheelite
therefore additional analysis is required to provide accurate tungsten values. Tungsten
mineralization, primarily as the mineral scheelite, has been observed in all of the drill
holes completed to date at Rhosgobel and occurs as coarse (up to 5 cm) scheelite
crystals within the sub-metre scale quartz, and quartz tourmaline veins and as smaller
(0.5-1 cm) crystals with the centimetre-scale sheeted quartz veins. The Company is very
encouraged by these initial analytical results, however, additional work is needed to further
investigate the nature and distribution of tungsten mineralization and its potential economic
significance at Rhosgobel as a by-product of potential gold production.
The company has submitted additional samples from drill hole DDRCRG-25-004 for
tungsten analysis including a lithium borate fusion with an XRF finish, sodium peroxide
fusion with and ICS-AES finish, and 4-acid digest with ICS-MS finish to compare results and
to follow up on the positive results obtained from hole DDRCRG-24-002, which intersected
zones of high-grade tungsten (6.98 m of 0.39% WO3, and 0.61 m of 4.73 % WO3) within
broad zones of lower grade tungsten mineralization (75.5 m of 0.132 % WO3, and 46.19 m
of 0.121 % WO3). Gold assays for hole 002 returned 173.3 metres of 0.60 g/t gold from
97.0 metres, including 28.4 metres of 1.40 g/t gold from 105.0 metres, and 12.4 metres of
2.40 g/t gold from 121.0 metres (see news release dated September 18, 2025). Once
results of the current test work have been completed and reviewed, additional samples will
be submitted to assess the tungsten distribution at Rhosgobel.
Figure 7: Example of scheelite (top picture), a common tungsten mineral, illuminated by
ultra-violet light with visible gold and bismuthinite (red circles) in a quartz vein in drill core from
the Rhosgobel intrusion along with an additional example of visible gold (bottom picture), both
observed in DDRCRG-25-042.
May-Qu Drill Results
Two holes drilled from the same location at the May-Qu target were completed during the 2025
season to test the south and southwest extension of multigram rock sample results returned
from previous exploration (see Figure 8). MQ-25-002 was drilled at 205 degrees azimuth and a
-60 degree dip to a final length of 326.1 m while MQ25-003 was drilled at a 025 degrees
azimuth with a -60 degree dip to a final length of 280.4 m. Both holes intersected granodiorite
intrusive rock with local sheeted quartz veins containing varying amounts of arsenopyrite,
pyrrhotite, chalcopyrite and bismuthinite.
Analytical results returned gold values of up to 2.0 m of 0.70 g/t Au and elevated values for
pathfinder elements arsenic and bismuth in MQ-25-002, suggesting that the mineralized system
is strengthening in a southwest direction. The May-Qu target encompasses a large area that
includes the Tombstone Suite Bos stock intrusion exposed along the eastern margin of a large
magnetic low signature that is typical of Reduced-Intrusion Gold Systems (see Figure 8).
Several target areas remain untested by drilling within the May-Qu area and additional work is
planned at May-Qu in 2026 to follow up on the anomalous 2025 results and test numerous other
mineralized sites in the May-Qu area.
Figure 8: Plan map of the May-Qu target area showing geochemical and geophysical results
along with drill hole locations. Additional work is planned at May-Qu in 2026 to follow up on the
2025 drill results and test numerous other mineralized sites in the May-Qu area where surface
grab samples have returned up to 31.7 g/t Au and 585.0 g/t Ag.
Figure 9: A plan map showing the Clear Creek Intrusive Complex (CCIC) location within the
district-scale RC Gold Project showing the updated resource areas at Blackjack and Eiger
along with the newly discovered Rhosgobel zone and several other high-priority drill targets
and multiple exploration targets. The map highlights the numerous drill targets that Sitka
has outlined within the CCIC which all are connected by the existing road network on the
project and occur in an area measuring approximately five (5) km north-south and twelve
(12) km east-west. Several regional exploration and drill targets are also highlighted across
the project area (yellow and orange stars).
Figure 10*: A plan map of the Clear Creek Intrusive Complex (CCIC) showing the updated
resource areas at Blackjack and Eiger, and the six additional areas that have drill targets
indicated by the mauve hatched areas. The map highlights the numerous drill targets that
Sitka has outlined within the CCIC which all are connected by the road network on the
project and occur in an area measuring five (5) km north-south and twelve (12) km
east-west. Additional areas highlighted by strong gold in soil anomalies are being advanced
to the drill ready stage with additional geological work planned in 2026.
* References for Figure 10 drilling intervals:
Rhosgobel Intervals: Sitka Gold News Release dated November 25, 2024
Pukelman Intervals: Sitka Gold News Release dated January 7, 2025
Contact Intervals: O'Brien, 2010; Assessment Report, 2010 Diamond Drilling Program, Clear Creek Property (Assessment report 095539)
Shutty, 2011; Assessment Report, 2011 Exploration Program, Clear Creek Property (Assessment Report 095984)
Bear Paw Intervals: Shutty, 2011; Assessment Report, 2011 Exploration Program, Clear Creek Property (Assessment Report 095984)
Figure 11: Regional map of the RC Gold Project located in the western portion of
Yukon’s prolific Tombstone Gold Belt.
About Sitka’s Flagship RC Gold Project
Sitka’s 100% owned RC Gold Project consists of a 431 square kilometre contiguous
district-scale land package located in the heart of Yukon’s Tombstone Gold Belt. The project
is located approximately 100 kilometres east of Dawson City, which has a 5,000 foot paved
runway, and is accessed via a secondary gravel road from the Klondike Highway which is
usable year-round and is an approximate 2 hour drive from Dawson City. It is one of the
largest consolidated land packages strategically positioned mid-way between the Eagle
Gold Mine and the past producing Brewery Creek Gold Mine.
The RC Gold Project now has pit-constrained mineral resources that are contained in two
zones: the Blackjack and Eiger gold deposits with 1,291,000 ounces of gold in 39,962,000
tonnes grading 1.01 g/t gold in an indicated category and 1,044,000 ounces of gold in
34,603,000 tonnes grading 0.94 g/t in an inferred category at Blackjack and 440,000
ounces of gold in 27,362,000 tonnes grading 0.50 g/t gold in an inferred category at Eiger.
These resource estimate numbers are supported by the recently updated technical report
for RC Gold, prepared in accordance with NI 43-101 standards, entitled “Clear Creek
Property, RC Gold Project NI 43-101 Technical Report Dawson Mining District, Yukon
Territory”, prepared by Ronald G. Simpson, P. Geo., of GeoSim Services Inc. with an
effective
date
of
January
21,
2025.
This
report
is
available
on
SEDAR+
(http://www.sedarplus.ca) and on the Company’s website (www.sitkagoldcorp.com).
Both of these deposits begin at surface, are potentially open pit minable and Initial bottle roll
metallurgical testing confirmed the non-refractory characteristics of the gold mineralization
and returned gold extraction rates averaging around 85%. Further metallurgical testwork in
2024 returned recoveries ranging from 77.6 to 93% for gravity followed by cyanidation.
For the purposes of the current resource model, it is assumed that a likely mill flowsheet
would consist of a gravimetric, flotation, and cyanidation circuit.
The company has now completed 165 diamond drill holes for a total of 59,770 metres
across the Clear Creek Intrusive Complex (CCIC), and an additional 3 holes for 858 metres
in the May-Qu Intrusion. Drilling continues to outline higher grade mineralization at all zones
including hole DDRCCC-24-068 at Blackjack which intersected 678.1 metres of 1.04 g/t
gold starting from surface (see news release dated October 21, 2024), and hole
DDRCCC-25-075 which intersected 352.8 metres of 1.55 g/t gold including 108.9 metres
of 3.27 g/t gold and 45.0 metres of 4.52 g/t gold (see news release dated April 22, 2025).
Drilling in 2024/2025 has resulted in the discovery of a new higher grade zone at
Rhosggobel including hole DDRCRG-25-010 at Rhosgobel which intersected 235.9 metres
of 1.11 g/t gold, including 40.0 m of 2.01 g/t gold and 10.0 m of 5.29 g/t gold, from surface
(see news release dated September 18, 2025).
RC Gold Deposit Model
Exploration on the Property has mainly focused on identifying an intrusion-related gold
system (“IRGS”). The property is within the Tombstone Gold Belt which is the prominent
host to IRGS deposits within the Tintina Gold Province in Yukon and Alaska. Notable
deposits from the belt include: Fort Knox Mine in Alaska with current Proven and Probable
Reserves of 230 million tonnes at 0.3 g/t Au (2.471 million ounces; Sims 2018)(1); Eagle
Gold Mine with current Measured and Indicated Resources of 233 million tonnes at a grade
of 0.57 g/t Au at the Eagle Main Zone (4.303 million ounces; Harvey et al, 2022)(2); the
Brewery Creek deposit with current Indicated Mineral Resource of 22.2 million tonnes at a
gold grade of 1.11 g/t (0.789 million ounces; Hulse et al. 2020)(3); the AurMac Project with
an Indicated Mineral Resource of 112.5 million tonnes grading 0.63 gram per tonne gold
(2.274 million ounces)(4) plus an Inferred resource of 280.6 million tonnes grading 0.60 g/t
gold (5.454 million ounces)(4), the Valley Deposit, with a current Measured and Indicated
Mineral Resource of 7.94 million oz gold at 1.21 g/t and an additional Inferred Mineral
Resource of 0.89 million oz at 0.62 g/t gold(5), and the Raven deposit with an inferred
mineral resource of 1.1 million oz (19.96 million tonnes at 1.67 g/t gold)(6). The QP has been
unable to verify the information regarding the above resource estimations and the
information is not necessarily indicative of the mineralization on the property that is the
subject of the disclosure.
(1) Sims J. Fort Knox Mine Fairbanks North Star Borough, Alaska, USA National Instrument 43-101 Technical Report. June 11, 2018.
https://s2.q4cdn.com/496390694/files/doc_downloads/2018/Fort-Knox-June-2018-Technical-Report.pdf
(2) Harvey N., Gray P., Winterton J., Jutras M., Levy M.,Technical Report for the Eagle Gold Mine, Yukon Territory, Canada. Victoria Gold Corp.
December 31, 2022. https://vgcx.com/site/assets/files/6534/vgcx_-_2023_eagle_mine_technical_report_final.pdf
(3) Hulse D, Emanuel C, Cook C. NI 43-101 Technical Report on Mineral Resources. Gustavson Associates. May 31, 2020.
https://minedocs.com/22/Brewery-Creek-PEA-01182022.pdf
(4) July 8, 2025,Banyan Gold Corp., News Release.
https://banyangold.com/news-releases/2025/banyan-announces-first-indicated-mineral-resources-and-identifies-high-grade-continuous-zones-at-it
s-aurmac-project-yukon-canada/
(5) https://snowlinegold.com/2025/05/15/snowline-gold-expands-measured-and-indicated-gold-ounces-by-96-in-updated-mineral-resource-estimate-atits-valley-gold-deposit-yukon/
(6) Jutras, M. 2022. Technical Report on the Raven Mineral Deposit, Mayo Mining District Yukon Territory, Canada, prepared for Victoria Gold Corp
and filed on SEDAR (www.sedar.com) with an effective date of September 15, 2022
Quality Assurance/Quality Control
On receipt from the drill site, the HTW/NTW-sized drill core was systematically logged for
geological attributes, photographed and sampled at Sitka’s core logging facility. Sample
lengths as small as 0.3 m were used to isolate features of interest, otherwise a default 2 m
downhole sample length was used. Each sample is identified by a unique sample tag
number which is placed in the bag containing the core to be assayed. Core was cut in half
lengthwise along a predetermined line, with one-half (same half, consistently) collected for
analysis and one-half stored as a record. Standard reference materials, blanks and
duplicate samples were inserted by Sitka personnel at regular intervals into the sample
stream. Bagged samples were placed in secure bins to ensure integrity during transport.
They were delivered by Sitka personnel or a contract expeditor to ALS Laboratories’
preparatory facility in Whitehorse, Yukon, with analyses completed in North Vancouver.
ALS is accredited to ISO 17025:2005 UKAS ref. 4028 for its laboratory analysis. Samples
were crushed by ALS to over 70 per cent passing below two millimetres and split using a
riffle splitter. One-thousand-gram splits were pulverized to over 85 per cent passing below
75 microns. Gold determinations are by fire assay with an inductively coupled plasma mass
spectroscopy (ICP-AES) finish on 50 g subsamples of the prepared pulp (ALS code:
Au-ICP-22). Any sample returning over 10 g/t gold was re-analyzed by fire assay with a
gravimetric finish on a 50 g subsample (ALS code: Au-GRA21). In addition, a 51-element
analysis was performed on a 0.5 g subsample of the prepared pulps by an aqua regia
digestion followed by an inductively coupled plasma mass spectroscopy (ICP-MS) finish
(ALS code: ME-MS41).
Coppermine River Update
The Company also reports results from the inaugural diamond drill program completed at its
Coppermine River project located near Kugluktuk, Nunavut. The program, conducted by
Arctic Copper Corp, a wholly-owned subsidiary of Sitka, was designed to follow up on
previous prospecting discoveries where geochemical and geophysical surveys had outlined
prospective drill targets.
Four wide-spaced reconnaissance holes were drilled at the Copper Leaf Showing (see
Figure 12) to follow up on sediment-hosted copper mineralization discovered in 2015 and
on subsequent gravity survey anomalies. These are proximal to a prominent north-south
trending Gabbro Dike that transects the area for more than 12 km. Drilling results at
Copper Leaf returned anomalous copper values and has not yet identified the source of
mineralization found at surface.
Three wide-spaced reconnaissance holes were also drilled at the WIN and HA showings
(see Figure 13), where historic trenching from the 1960’s uncovered high grade
volcanic-hosted copper mineralization found in the Copper Creek Basalts. Past sampling of
these results by Sitka personnel returned assays as high as 40% copper with 36.0 g/t silver
at the WIN Trench, and as high as 17% copper with 29.0 g/t silver at the HA Trench. Assay
results from the 2025 drilling campaign returned anomalous copper values in the core
samples and have not yet identified the source of mineralization found at surface.
Figure 12:
Plan map showing wide-spaced reconnaissance drill hole locations, grab
sample results and gravity survey results at the Copper Leaf target.
Figure 13: Plan map of wide-spaced reconnaissance drill hole locations and grab sample
results at the WIN and HA targets.
Table 3. Drill Collar Summary-Coppermine Project
Hole_ID
Easting
Northing
Azimuth (°) Inclination (°)
Depth (m)
CM25-01
544721
7477370
270
-50
144
CM25-02
544885
7477371
270
-70
129
CM25-03
544800
7477170
270
-60
165
CM25-04
544721
7477370
270
-50
180
CM25-05
591877
7502804
120
-45
89
CM25-06
591090
7501253
120
-45
90
CM25-07
591090
7501253
N/A
-90
54
About Sitka Gold Corp.
Sitka Gold Corp. is a well-funded mineral exploration company headquartered in Canada with
over $45 million in its treasury and no debt. The Company is managed by a team of
experienced industry professionals and is focused on exploring for economically viable mineral
deposits with its primary emphasis on gold, silver and copper mineral properties of merit. Sitka
is currently advancing its 100% owned, 431 square kilometre flagship RC Gold Project located
within the Tombstone Gold Belt in the Yukon Territory. The Company is also advancing the
Alpha Gold Project in Nevada and currently has drill permits for its Burro Creek Gold and
Silver Project in Arizona and the Coppermine River Project in Nunavut, all of which are 100%
owned by Sitka.
*For more detailed information on the Company’s properties please visit our website at
www.sitkagoldcorp.com
Upcoming Events
Sitka Gold will be attending and/or presenting at the following events*:
● 3rd Annual Canadian Critical Minerals Opportunity Forum: New York, New York,
January 21, 2026
● Metals Investor Forum (MIF): Vancouver, BC: January 23 - 24, 2026
● Vancouver Resource Investment Conference (VRIC): Vancouver, BC: January 25 26, 2026
● AME Roundup: Vancouver, BC: January 26 - 29, 2026
*All events are subject to change.
The scientific and technical content of this news release has been reviewed and approved
by Gilles Dessureau, P.Geo., V.P. Exploration of the Company, and a Qualified Person (QP)
as defined by National Instrument 43-101.
ON BEHALF OF THE BOARD OF DIRECTORS OF
SITKA GOLD CORP.
“Donald Penner”
President and Director
For more information contact:
Donald Penner
President & Director
778-212-1950
or
Cor Coe
CEO & Director
604-817-4753
Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined
in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or
accuracy of this release.
Cautionary and Forward-Looking Statements
This
release
includes
certain
statements
and
information
that
may constitute
forward-looking information within the meaning of applicable Canadian securities laws.
Forward-looking statements relate to future events or future performance and reflect the
expectations or beliefs of management of the Company regarding future events. Generally,
forward-looking statements and information can be identified by the use of forward-looking
terminology such as “intends” or “anticipates”, or variations of such words and phrases or
statements that certain actions, events or results “may”, “could”, “should”, “would” or
“occur”. This information and these statements, referred to herein as “forward‐looking
statements”, are not historical facts, are made as of the date of this news release and
include without limitation, statements regarding discussions of future plans, estimates and
forecasts and statements as to management’s expectations and intentions and the
Company’s anticipated work programs.
These forward‐looking statements involve numerous risks and uncertainties and actual
results might differ materially from results suggested in any forward-looking statements.
These risks and uncertainties include, among other things, market uncertainty and the
results of the Company’s anticipated work programs.
Although management of the Company has attempted to identify important factors that
could cause actual results to differ materially from those contained in forward-looking
statements or forward-looking information, there may be other factors that cause results not
to be as anticipated, estimated or intended. There can be no assurance that such
statements will prove to be accurate, as actual results and future events could differ
materially from those anticipated in such statements. Accordingly, readers should not place
undue reliance on forward-looking statements and forward-looking information. Readers are
cautioned that reliance on such information may not be appropriate for other purposes. The
Company does not undertake to update any forward-looking statement, forward-looking
information or financial out-look that are incorporated by reference herein, except in
accordance with applicable securities laws. We seek safe harbor.