Juggernaut Reports New High-Grade GOLD Discovery ON the 11 Km Highway of GOLD with up to 79 G/T (2.54 OZ/T) GOLD from over 200 Polymetallic Veins IN the Eldorado Porphyry System ON BIG One Property – Drill Ready - Golden Triangle, B.c.
JUGGERNAUT REPORTS NEW HIGH-GRADE GOLD DISCOVERY ON THE 11
KM HIGHWAY OF GOLD WITH UP TO 79 G/T (2.54 OZ/T) GOLD FROM
OVER 200 POLYMETALLIC VEINS IN THE ELDORADO PORPHYRY SYSTEM
ON BIG ONE PROPERTY – DRILL READY - GOLDEN TRIANGLE, B.C.
Vancouver, British Columbia – January 20, 2025 – Juggernaut Exploration Ltd (JUGR.V) (OTCQB: JUGRF) (FSE:
4JE) (the “Company” or “Juggernaut”) is pleased to report a new discovery with assays up to 79.01 g/t Au
(2.54 oz/t Au) and 3157.89 g/t Ag (101.5 oz/t Ag), from >200 gold-silver-copper rich polymetallic veins up to
8 m wide and striking for up to 500 m that remain open. These veins were identified along the newly
discovered 11 km Highway of Gold surrounding the Eldorado porphyry system on the Big One property ;
additional assays are pending. The discovery is located in a glacial and snowpack abatement area adjacent to
the world-class gold-rich porphyry systems at Galore Creek. The property covers 33 ,693 hectares in world-
class geologic terrain with tremendous additional discovery potential in the heart of the Golden Triangle,
British Columbia. The Big One property is 100 % controlled by the B-ALL Syndicate, a private precious metals
project generator of which Juggernaut Exploration is a significant stakeholder.
BigOne Eldorado Map
BigOne Video
Dan Stuart, President and CEO of Juggernaut Exploration , states, “Results from 2024 B -ALL Syndicate
exploration program far exceeded the technical team's expectations as demonstrated by the discovery of the
extensive Eldorado porphyry system and the 11 km Highway of Gold on the Big One property that contains
multiple high-grade gold-silver polymetallic veins on surface that remain open, are drill ready and indicated
to be part of a much larger precious and base metal porphyry system or systems at depth . To have 100 %
control over a district-scale property of this caliber located in world-class geologic terrane in close proximity
to a tier 1 deposit the likes of Galore Creek is a once -in-a-lifetime opportunity. With ~95 % of the Big One
property remaining unexplored and hosting vast areas of newly exposed outcrop due to glacial and snowpack
retreat, it provides for excellent additional discovery potential. Juggernaut’s management is pleased that the
company has a significant stake in the B -ALL Syndicate and its assets as a project like Big One is a very rare
opportunity that has already garnered significant interest from many key strategic investors and is certain to
be fully funded, if not oversubscribed, by the company that is fortunate enough to have an option to earn a
100% interest in this amazing new discovery.”
ELDORADO PORPHRYRY SYSTEM/ 11 KM HIGHWAY OF GOLD HIGHLIGHTS
• Whopper vein: grab samples from 5 m wide quartz-sulphide vein hosted in an 8 m wide mineralized
shear zone returned 13.12 g/t Au and 169.88 g/t Ag, as well as 10.62 g/t Au and 206.32 g/t Ag, and
6.01 g/t Au and 121.97 g/t Ag. The Whopper vein is exposed on surface for 100 m and remains open
along strike where it goes under snowpack and ice. The quartz vein consists of lenses and seams of
massive pyrite and galena contained in the quartz vein and stockwork. The high-grade Whopper
vein’s geochemical and geophysical signatures are indicative of a porphyry source at depth. This
target is drill ready. BigOne_Whopper Image 1, BigOne_Whopper Image 2, BigOne_Whopper Image
3, BigOne_Whopper Image 4, BigOne Whopper Video
• Big Mac Vein: Grab sample from a quartz -sulphide vein hosted in a 4 m wide shear zone that
contains stringers of semi-massive galena as well as clots of chalcopyrite and pyrite assayed 37.98
g/t Au and 70.37 g/t Ag, as well as 10.61 g/t Au, 3.55 g/t Ag. The Big Mac vein is exposed for >50 m
where it goes under overburden/ice and remains open. The Big Mac vein’s geochemical signature is
conducive for a porphyry source that is also indicated by geophysical anomalies at depth. This target
is drill ready. BigOne BigMac Image, BigOne BigMac Video
• Giant Vein: Channel sample across 1.5 m quartz vein with lenses and stringers of semi -massive to
massive chalcopyrite and pyrite returned 5.06 g/t Au and 91.41 g/t Ag. The vein extends vertically
for >30 m and remains open within a large gossanous area >100 m wide . The Giant vein’s
geochemical signature is conducive for a porphyry source that is also indicated by geophysical
anomalies at depth. This target is drill ready. BigOne Giant Image
• Deluxe Vein: Channel sample across a 45 cm vein containing semi -massive galena and pyrite
assayed 12.12 g/t Au and 2084.61 g/t Ag, as well as 3.39 g/t Au and 380.15 g/t Ag. The vein is up
to >2 m wide and has been traced along strike for 150 m and remains open . The Deluxe vein has a
geophysical anomaly at depth that is conducive for a porphyry source . This target is drill ready.
BigOne_Deluxe Image, BigOne Deluxe Video
• Double Decker: Grab sample from a set of intersecting quartz-sulphide veins up to 50 cm wide and
exposed for >60 m returned 19.82 g/t Au and 216.65 g/t Ag . The veins contain seams of semi -
massive galena and pyrite and remain open. The Double Decker vein has a geophysical anomaly at
depth that is conducive for a porphyry source. This target is drill ready. BigOne DoubleDecker
• Eldorado consists of a high-grade polymetallic gold -silver zone named Highway of Gold that
stretches 11 km and remains open on newly exposed bedrock along the fringes of the Geology Ridge
icefield and Decker Creek glacier.
• Eldorado demarks an area of 7.5 Km2 of recently exposed bedrock containing substantial propylitic
alteration, hydrothermal veining, and epithermal veining with >200 quartz-sulphide veins up to 8
m wide containing semi-massive to massive chalcopyrite, sphalerite and galena with grades up to
79.01 g/t Au (2.54 oz/t Au) and 3157 g/t Ag (101.5 oz/t Ag), that remains open.
• The polymetallic veins, alteration signature, geochemical path finder element signature, and
geophysical anomalies strongly indicate the presence of a common buried gold-silver-copper rich
porphyry feeder source at depth responsible for the extensive high -grade veining confirmed on
surface.
• The newly exposed Eldorado system contains >200 veins over an area of 1.2 km by 800 m that
remains open. Within this zone, veins up to 8 m wide and striking up to 500 m were observed
(Whopper vein), containing semi-massive to massive chalcopyrite, sphalerite and galena, indicated
to be the source of historic high-grade gold-silver angular float samples reported in the 1960s in the
valley below. Both the zone and the system remain open and are drill ready.
• At least t wo extensive areas with strong porphyry potential have been identified where the
distribution of geochemical path finder elements overlaps with strong geophysical anomalies as well
as multiple gold -rich polymetallic veins in outcrop clearly corresponds to the typical signature
observed within or in close proximity to a porphyry system. BigOne Geochemistry Maps
The results from the August 2024 reconnaissance exploration program on the Big One property confirmed
the excellent untapped exploration potential of the area with the discovery of the extensive high -grade
Eldorado gold-silver-copper system found along the 11 km Highway of Gold in newly exposed outcrop around
the fringes of the snowfields/glaciers. The Eldorado discovery is bordered by an extensive zone of propylitic
alteration halo covering an area of 4 km by 1 km and porphyry textures in outcrop , which, coupled with
buried geophysical anomalies and strong geochemical pathfinder element signatures, strongly indicates the
presence of a large mineralizing (porphyry) system or systems at depth indicated to be the origin of the
extensive high-grade gold, silver and copper mineralization confirmed in veins on surface over 11 km that
remains open.
The Big One property covers an area of 33,693 hectares of world-class geologic terrain in the heart of the
Golden Triangle of British Columbia, Canada. The property is largely unexplored which only recently due to
ongoing rapid glacial and snowpack abatement provided an opportunity to explore extensive areas of newly
exposed outcrop providing strong potential for discovery today and into the future.
The Eldorado system is indicated to be the source of angular float samples with grades up to 16.9 g/t Au and
49 g/t Ag discovered in the early 1960s. Eldorado corresponds to the location of the source that was
suggested by renowned geologist and glaciation expert Dr. Richard E Kucera in 1990 to the west of the
boulder field at an elevation of >4700 ft which at the time was covered by permanent snow and ice.
BigOne Float Zone
We have only just started to scratch the surface of the property and have likely only seen the tip of the
iceberg. A number of mineralized occurrences including porphyry and extensive high-grade polymetallic veins
were discovered on the Big One property clearly demonstrating the enormous untapped potential of this
area that could quickly evolve into a new world-class discovery.
Table 1: Assay highlights from the Big One property
Sample ID Au (g/t) Ag (g/t) Type Description
D751282 79.01 53.49 Grab Pyrite, malachite in veins within granodiorite
D751966 56.54 23.40 Grab Quartz vein with semi-massive pyrite
D751216 37.98 70.37 Grab Quartz vein with semi-massive galena, chalcopyrite
D751156 33.72 128.83 Grab Quartz vein with galena and chalcopyrite
D751163 23.97 2.75 Float Quartz vein with pyrite, galena, chalcopyrite
D751964 23.47 105.31 Talus Altered andesite with coarse chlorite
D751209 19.82 216.65 Grab Quartz vein with galena, pyrite
D750394 13.12 169.88 Grab Quartz with massive pyrite
D751191 12.12 2084.61 Channel Quartz vein with semi-massive galena, pyrite
D750608 10.62 3.55 Grab Altered diorite with 30 cm quartz vein with pyrite
D751975 10.62 206.32 Grab Altered diorite with seems of massive pyrite
D750389 8.10 1421.50 Grab Quartz vein with 15% pyrite and 3% sphalerite
D751284 6.34 56.05 Float Quartz vein with galena and pyrite
D750198 6.01 32.31 Float Polymetallic quartz vein sample with chalcopyrite, sphalerite
D750395 6.01 121.97 Grab Quartz with 7% pyrite
D751154 5.72 219.32 Grab Quartz vein with galena, pyrite
D751969 5.59 187.89 Float Quartz vein with galena, sphalerite, chalcopyrite
D751939 5.06 91.41 Channel Quartz vein with massive pyrite and minor galena
D751112 4.94 60.63 Float Quartz vein with chalcopyrite, pyrite, galena, and trace chalcopyrite
D751158 4.60 33.15 Grab Quartz vein with pyrite and trace galena
D751943 4.00 99.85 Grab Polymetallic quartz with galena, chalcopyrite
D751285 3.74 101.58 Grab Granodiorite with chalcopyrite in quartz vein
D750657 3.71 41.29 Grab Chalcopyrite and pyrite in fractures
D750192 3.44 230.39 Grab Polymetallic quartz vein with 25% chalcopyrite and siderite
D751192 3.39 380.15 Channel Quartz vein with semi-massive galena, pyrite
D751215 2.96 105.47 Grab Quartz vein with pyrite, chalcopyrite, and galena
D751699 2.15 67.96 Grab Quartz with galena
D751164 2.03 3157.89 Grab Quartz vein with chalcopyrite, galena, and malachite
D751165 1.95 2.75 Grab Chloritic rock with quartz vein
D751109 1.65 86.36 Grab Quartz vein with 35% pyrite
D751213 1.65 59.19 Float Quartz vein with galena and pyrite
D751195 1.61 36.67 Channel Quartz vein with chalcopyrite, pyrite
D750656 1.56 100.27 Grab Quartz vein with semi-massive galena
D751968 1.49 58.18 Grab Magmatic volcanic rock with chlorite alteration
D751972 1.42 44.82 Channel Diorite with galena, pyrite, chalcopyrite
D751116 1.27 14.42 Grab Gossanous silicified diorite with pyrite
D751993 1.20 10.66 Grab Vein in diorite with pyrite and galena
D750393 1.01 38.49 Grab Quartz vein with 10% pyrite and 10% galena
The Big One property is situated in a region that is well known for hosting world class precious metal and
porphyry deposits, several of which occur near the property including the multiple porphyry systems at
Galore Creek (12,159 million pounds of copper, 9.438 million ounces of gold, 174.086 million ounces of
silver), the world’s largest known gold reserve at KSM (47.3 million ounces of gold, 160 million ounces of
silver, 7.32 billion pounds of copper) and the polymetallic copper project at Shaft Creek (5 billion pounds of
copper, 3.7 million ounces of gold, 16.4 million ounces of silver), as well as the Brucejack high -grade
epithermal gold deposit (14 million ounces of gold, 91.8 million ounces of silver), and the structurally
controlled high-grade hydrothermal gold-silver zones at Trophy and Sphal Creek. The property geology is
favorable to host these types of deposits as confirmed by the presence of extensive areas of propylitic
alteration, untested geophysical anomalies, strong silt, soil and rock geoch emistry including path finder
elements directly related to porphyry systems, key structures and textures, porphyry -style mineralization,
and high -grade polymetallic veins, that have been discovered within the Big One claims.
BigOne Property Map
The Big One property can be accessed year-round via helicopter from the Glenora/Telegraph Creek Road at
the Barrington Mine (33 km to the north -northeast) as well as the Galore Creek Road (15 km to the
southeast). The Canadian government committed $20 M to extend/improve the Galore Creek Road to within
15 km of the Big One property. The property is 2 km west of the Scud River airstrip used in the early days of
Galore Creek.
The Big One property exploration qualifies for the Critical Mineral Exploration Tax Credit (CMETC).
About the B-ALL Syndicate
The B-ALL Syndicate is a highly specialized geologic team of project generators with a proven track record of
success. The Syndicate is focused on unexplored glacial and snowpack retreat areas, providing new
opportunities for material discovery in world-class geologic terrain. The B -ALL Syndicate is on track with
discovery as demonstrated with Big One and other properties generated by the J2 Syndicate , such as
Golddigger and Midas properties that were subsequently optioned out, resulting in the material Surebet
discovery with Goliath Resources, to mention a few. The B-ALL Syndicate team consists of many of the same
J2 Syndicate members who have played key roles from inception in the exploration programs for both Goliath
Resources and Juggernaut Exploration and are responsible for multiple original discoveries. Juggernaut
Exploration has a significant interest in the B-ALL Syndicate.
AME ROUNDUP 2025
To learn more about the Big One Discovery , we would like to cordially invite you to visit us with our full
technical team in attendance at the AME Roundup Core Shack, Booth # 919, on Monday, January 20 th (9:00
AM – 4:00 PM) and Tuesday, January 21 st, 2023 (9:00 AM – 4:00 PM). The event is at the Exhibit Hall -
Vancouver Convention Centre East Building (1055 Canada Place, Vancouver, B.C.). If you cannot see us at the
core shack, please visit us at Booth # 1525, as Juggernaut will also be exhibiting al l 4 day s at the AME
Roundup, Monday, January 20th – Thursday, January 24th, 2024.
About Juggernaut Exploration Ltd.
Juggernaut Exploration Ltd. is an explorer and generator of precious metals projects in the prolific Golden
Triangle of northwestern British Columbia. Its projects are in world-class geological settings and geopolitical
safe jurisdictions amenable to mining in Canada. Juggernaut is a member and active supporter of CASERM,
an organization representing a collaborative venture between the Colorado School of Mines and Virginia
Tech. Juggernaut’s key strategic cornerstone shareholder is Crescat Capital.
For more information, please contact:
Dan Stuart
President, Director, and Chief Executive Officer
604-559-8028
www.juggernautexploration.com
Qualified Person
Tyler Punk, P . Geo is the qualified person, as defined by National Instrument 43 -101, for Juggernaut
Exploration projects, and supervised the preparation of, and has reviewed and approved, the technical
information in this release.
Other
Grab, channels, chip and talus samples were collected by foot with helicopter assistance. Prospective areas
included, but were not limited to, proximity to MINFile locations, placer creek occurrences, regional soil
anomalies, and potential gossans based on high-resolution satellite imagery. The rock grab and chip samples
were extracted using a rock hammer, or hammer and chisel to expose fresh surfaces and to liberate a sample
of anywhere between 0.5 to 5.0 kilograms. All sample sites were flagged with biode gradable flagging tape
and marked with the sample number. All sample sites were recorded using hand-held GPS units (accuracy 3-
10 meters) and sample ID, easting, northing, elevation, type of sample (outcrop, subcrop, float, talus, chip,
grab, etc.) and a description of the rock were recorded on all-weather paper. Samples were then inserted in
a clean plastic bag with a sample tag for transport and shipping to the geochemistry lab. QA/QC samples
including blanks, standards, and duplicate samples were inserted regularly into the sample sequence at a rate
of 10%.
All samples are transported in rice bags sealed with numbered security tags. A transport company takes them
from the core shack to the Paragon Geochemical labs facilities in Surrey, BC or ALS labs facilities in North
Vancouver, BC. Paragon Geochemical is certified with both AC89-IAS and ISO/IEC Standard 17025:2017. ALS
is either certified to ISO 9001:2008 or accredited to ISO 17025:2005 in all of its locations. Samples submitted
to Paragon received gold and silver analysis by photon assay whereby the entire sample is crushed to
approximately 70% passing 2 mm mesh. The entire crushed sample is riffle split and weighed into multiple
(300-500g) jars that are submitted for photon assay. Photon assay uses high-energy X-rays (photons) to excite
atomic nuclei within the jarred samples, causing them to emit secondary gamma rays, which are measured
to identify and quantify the metals present. The assays from all jars are combined on a weight-averaged basis.
At ALS samples were processed, dried, crushed, and pulverized before analysis using the ME-MS61 and Au-
SCR21 methods. For the ME-MS61 method, a prepared sample is digested with perchloric, nitric, hydrofluoric,
and hydrochloric acids. The residue is topped up with dilute hydrochloric acid and analyzed by inductively
coupled plasma atomic emission spectrometry. Overlimits were re -analyzed using the ME -OG62 and Ag -
GRA21 methods (gravimetric finish). For Au-SCR21 a large volume of sample is needed (typically 1-3kg). The
sample is crushed and screened (usually to -106 micron) to separate coarse gold particles from fine material.
After screening, two aliquots of the fine fraction are analysed using the traditional fire assay method. The
fine fraction is expected to be reasonably homogenous and well represented by the duplicate analyses. The
entire coarse fraction is assayed to determine the contribution of the coarse gold.
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