White Gold Corp. Launches Spin-Out of W2 Critical Minerals Corp.
May 5, 2026
NOT FOR DISTRIBUTION TO U.S. NEWS WIRE SERVICES OR DISSEMINATION IN THE UNITED STATES
White Gold Corp. Launches Spin-Out of W2 Critical Minerals Corp.
TORONTO, May 5, 2026 – White Gold Corp. (TSX.V: WGO, OTCQX: WHGOF, FRA: 29W) (“White Gold” or
the “Company”) is pleased to announce that further to its press release dated February 11, 2026, the
Company has entered into an arrangement agreement (the “ Arrangement Agreement”) with W2 Critical
Minerals Corp. (“Spinco”), a wholly owned subsidiary of the Company. The Spin-Out is designed to unlock
the value of White Gold ’s non-gold project portfolio by transferring its portfolio of copper, molybdenum,
tungsten and other critical mineral properties located in west-central Yukon (the “Critical Mineral Assets”)
into a dedicated, standalone vehicle, and spin-out the common shares of Spinco (the “ Spinco Shares”) to
the Company’s shareholders (“Shareholders”) on the basis of one Spinco Share for every five White Gold
Corp. shares held (as defined below), through a plan of arrangement under the Business Corporations Act
(Ontario) (the “ Spin-Out”). In connection with the Spin -Out, Spinco intends to complete a private
placement financing for gross proceeds of up to $5 million (the “Spinco Financing”) and White Gold Corp.
intends to retain 19.9% of the Spinco Shares upon completion of the Spin-Out.
White Gold Corp. will continue to advance its flagship White Gold Project which hosts four near -surface
gold deposits, that collectively contain an estimated 1,732,300 ounces of gold in indicated resources (35.2
million tonnes grading 1.53 grams per tonne gold) and 1,265,900 ounces of gold in inferred resources (32.2
million tonnes grading 1.22 g/t Au) (1), with significant expansion potential on the resource itself and in the
immediately surrounding area. The Company’s White Gold Project is also complimented by a substantial
pipeline of gold targets across the Company’s district scale property portfolio in the emerging White Gold
District.
“White Gold has systematically built one of the most comprehensive regional geochemical and geological
datasets in the Yukon, which has clearly highlighted the scale and quality of several copper and critical
mineral targets within our portfolio in addition to our significant gold projects. Assets such as Bridget, Isaac,
and Wolf exhibit the size, metal zonation, and geophysical signatures typically associated with large, fertile
porphyry systems, yet remain largely untested by drilling. Spinning these assets into a dedicated v ehicle
allows them to be advanced more effectively with the technical focus and disciplined exploration strategy
they warrant,” commented Dylan Langille, Vice President of Exploration for White Gold.
White Gold’s CEO, David D ’Onofrio stated, “The timing of th e Spin-Out aligns exceptionally well with the
strong and growing support we are seeing from both the Yukon and federal governments for the
responsible development of critical minerals. Recent initiatives focused on advancing critical mineral
exploration, improving infrastructure, streamlining permitting, and strengthening collaboration across
Western and Northern Canada reinforce Yukon’s position as a globally desirable jurisdiction for discovery
and development. By creating this dedicated critical minerals company, we believe we are enhancing
shareholder value and also advancing opportunities that are increasingly central to Canada ’s long-term
economic and supply chain strategies.”
SpinCo Highlights:
• Spinco to apply to list the Spinco Shares on the TSXV shortly following completion of the Spin-Out.
• Spinco to include six properties representing approximately 15% of White Gold's current claims and
includes numerous copper and strategic metals targets presenting discovery upside in an area with
prospective geology for copper, molybdenum, tungsten, antimony and bismuth across multiple
deposit styles.
• Key targets – Bridget, Isaac and Mascot – situated within the Dawson Range, a proven mineral belt
hosting major copper -gold systems such as the Casino deposit, Minto Mine, and the Carmacks
Project.
• Several of the Spin -Out targets include additional upside potential for antimony and bismuth as
secondary metals across orogenic gold, intrusion-related, epithermal, and porphyry systems.
• Further details regarding the Spin-Out, including its management team and strategic direction, as
well as information pertaining to the annual general and special meeting of shareholders to
approve the Spin-Out, anticipated to be held prior to the end of Q2 2026 , will be provided in due
course.
• Additional near term Company updates to include further exploration results, a maiden Preliminary
Economic Assessment and the announcement of the company's exploration program scheduled to
kick off in the coming weeks, the largest in the company's history, which is designed with the
objective of meaningfully increasing the size of the company's known large gold resource and
following up on and making new gold and critical mineral discoveries across the Company's district-
scale land package.
Following completion of the Spin -Out, the Critical Mineral Assets to be held by Spinco will include the six
properties: the Bridget Property; the Loonie Property; the Wolf Property; the Hunker Property; the Hayes
Property; and the Toonie Property. These properties include several large-scale critical minerals targets
prospective for Copper (Cu), Molybdenum (Mo), Tungsten (W), Antimony (Sb), Zinc (Zn) and Bismuth (Bi),
underlain by prospective geology which was identified through White Gold’s data driven exploration
methodologies which have proven to be successful in the region. Key targets — including the Bridget, Isaac,
and Mascot — are situated within the Dawson Range, a prolific east-southeast trending mineral belt that
hosts several significant copper -gold porphyry deposits including the Casino deposit (one of the largest
undeveloped copper -gold projects in Canada), the Minto Mine, and the Carmacks Project (see the
Company’s news release date February 11, 2026).
The Spin-Out
Pursuant to the terms of the Arrangement Agreement, the Company will, among other things, transfer its
interests in the Critical Minerals Assets to Spinco in exchange for Spinco Shares and then distribute Spinco
Shares to the holders of common shares of the Company (“WGO Shares”) on the basis of one Spinco Share
for every five WGO Shares held by each Shareholder immediately prior to the effective date of the Spin-
Out. There will be no change in the Shareholders’ holdings in the Company as a result of the Spin -Out.
Following completion of the Spin -Out, the Company is expected to hold a 19.9% ownership interest in
Spinco.
The Spin-Out will be subject to regulatory approval, including the approval of the T SX Venture Exchange
(the “TSXV”) and court approval, as well as approval by not less than two -thirds of the votes cast at the
annual general and special meeting of the Shareholders that is expected to be held before the end of Q2
2026 (the “Meeting”).
Spinco intends to apply to list the Spinco Shares on the TSXV shortly following completion of the Spin-Out.
Readers are cautioned that, while Spinco intends to pursue a listing on the TSXV, an application for listing
has not been submitted and completion of a listing is subject to regulatory approvals and the satisfaction
of all of the applicable listing requirements of the TSXV. There can be no assurance that a listing will be
completed, and Spinco may elect not to proceed with a listing at any time in its sole discretion.
Additional details relating to the Spin -Out and Spinco will be included in the management information
circular in respect of the Meeting to be filed and delivered to Shareholders in connection with the
Meeting. Copies of the management information circular and related meeting materials will also be filed
with the applicable Canadian securities regulators and available on the Company’s profile on SEDAR+
(www.sedarplus.ca).
The Spinco Financing
In connection with the Spin -Out, Spinco intends to complete the Spinco Financing, being a private
placement of up to 20 million subscription receipts of Spinco (the “ Subscription Receipts”) at a price of
$0.25 per Subscription Receipt for gross proceeds of up to $5 million. On closing of the Spin -Out, the
Subscription Receipts will automatically convert into Spinco Shares. Pending the closing of the Spin -Out,
the proceeds from the sale of the Subscription Receipts will be held in escrow by a trust company and
released to Spinco on closing of the Spin -Out. Completion of the Spinco Financing is a condition of the
completion of the Spin -Out and Spinco intends to use the net proceeds of the Spinco Financing for
exploration and advancement of the Critical Mineral Assets, as well as general corporate and working
capital purposes.
The securities have not been and will not be registered under the United States Securities Act of 1933, as
amended (the " U.S. Securities Act "), or the securities laws of any state of the “United States” (as such
term is defined in Regulation S under the U.S. Securities Act), and may not be offered or sold in the United
States unless registered under the U.S. Securities Act and the securities laws of any applicable state of the
United States or an exemption from such registration requirements is available. T his news release shall
not constitute an offer to sell or the solicitation of an offer to buy nor shall there be any sale of the
securities in any jurisdiction in which such offer, solicitation or sale would be unlawful.
Critical Minerals Portfolio Overview
Regional Setting -- The Dawson Range and Critical Mineral Belt
The Dawson Range (Figures 1 & 2) is an east -southeast-trending mountain belt that hosts numerous
significant mineral deposits and prospects along the Minto -Carmacks copper belt, including the Casino
copper-gold porphyry deposit in the west owned by Western Copper and Gold. In the southeast near the
community of Carmacks, the Minto mine owned by Selkirk Copper Mines Inc ..(2)(6) contains indicated
resources of 12,588,000 Mt grading 1.203 per cent Cu, 0.461 g/t Au, 1,728 ounces Ag for 333.8 Mlb
copper, 186,600 oz gold, and 1,728,000 ounces silver and inferred resources of 23,658,000 t grading 1.048
per cent Cu, 0.387 g/t Au, 3.9 g/t Ag for 546.8 Mlb copper, 294,700 ounces gold and 2,968.1 ounces silver.
It also hosts the Carmacks Copper project, which contains measured and indicated resources of 36.25 Mt
grading 0.81 per cent Cu, 3.25 g/t Ag, 0.26 g/t Au for 651 Mlb of copper, 3.79 M ounces silver and 302,000
ounces of gold, owned by Cascadia Minerals Ltd (2) (7). Both deposits are interpreted as metamorphosed
copper-gold-silver porphyry systems. Porphyry deposits in the Dawson Range occur in two principal age
groups: Late Triassic (for example, Minto, Carmacks) and Late Cretaceous (for example, Casino, Cash,
Revenue). In addition to porphyry -style mineralization, the Dawson Range also hosts epithermal, skarn
and polymetallic to gold -dominant veins, breccias and fracture zones (8). Owing to this diverse and
prospective mineral endowment, the region has attracted increasing attention and investment in recent
years from both junior and major mining companies.
The Critical Mineral A ssets to be transferred to SpinCo in connection with the Spin -Out include six
properties that collectively represent a pipeline of advanced to early stage critical mineral exploration
opportunities across multiple metallogenic belts in Yukon. Highlights include:
Bridget Property — Bridget Target (Mo-Cu-W-Bi-Ag)
A large untested porphyry system in the White Gold District
The Bridget target is a district-scale molybdenum-copper porphyry anomaly spanning 3 km by 3.5 km that
has never been diamond drill tested. The soil geochemical footprint of the anomaly is characterized by
Mo-in-soil values as high as 321.9 ppm Mo, including 278.9 ppm Mo, 265.4 ppm Mo, 263.5 ppm Mo, 257.2
ppm Mo, and 253.3 ppm Mo with over 400 additional samples returning values greater than 20 ppm Mo.
Across the target, anomalous Cu -in-soil values exceeding 100 ppm Cu are common with the most
significant enrichment occurring at the core with values as high as 710.1 ppm Cu, including 662.6 ppm Cu,
594.7 ppm Cu, 492.9 ppm Cu, 406 ppm Cu observed over a roughly 900 m x 900 m area. Other notably
enriched critical minerals include tungsten (W), with the highest concentrations observed in the northern
half of the target area, where soil sampling has yielded values up to 101 ppm W ; a critical mineral of
growing strategic importance. Secondary metals including bismuth, silver, lead, and zinc are concentrated
along t wo major crustal -scale dextral transpressional faults that transect the margins of the system
representing a peripheral epithermal expression of the porphyry system.
Follow-up prospecting has confirmed bedrock mineralization, with molybdenite directly identified in
quartz veins across the target. Rock samples define a coherent porphyry -style metal zonation: a Cu-Mo-
Bi core characterized by Mo-dominant quartz veins returning up to 3,650 ppm Mo, including 3,060 ppm
Mo, 2430 ppm Mo in mineralized gneisses and schists, pyrite -bearing white quartz veins returning 532
ppm Mo and 234 ppm Cu, and trench samples up to 1,854 ppm Cu. Bismuth reaches 2,000 ppm in altered
gneiss with 1,571 ppm Mo, and 836 ppm Bi in a quartz vein cutting hornblende gneiss. The peripheral
zones carry the distal metal signature typical of large porphyry systems: a quartz -galena vein in
orthogneiss returned 30.4 ppm Ag and 3,861 ppm Pb, while sampling along the margins of a rhyolite dyke
returned 560 ppm W alongside elevated silver and lead.
Two rounds of induced polarization geophysics surveys, completed in 2023 and 2025, have moved Bridget
from a geochemical anomaly into a drill -ready target. The 2023 survey identified five chargeability
anomalies beneath the Cu -Mo-Bi core, with the most com pelling centered at depths of at least 250 m,
more than 180 m deeper than the maximum depth reached by the Company’s 2018 shallow RAB program.
Those holes, limited to 70 m vertical depth with several failing to reach target depth, still intersected
molybdenum mineralization: hole PEDBRGRAB18 -009 returned 622.3 ppm Mo over 1.5 m from 12.2 m
and 631.9 ppm Mo over 1.5 m from 30.5 m. A 2025 ten-line gradient IP survey supplemented by a single
Dipole-Dipole survey across the center of the anomaly has confirmed the results of the 2023 survey while
adding additional targeting opportunities in the northwestern and southeastern margins of the anomaly.
The Bridget target sits within the Dawson Range mineral belt, transected by the Sixtymile River Fault and
Big Creek Fault, the same fault corridors associated with major porphyry and epithermal systems in the
region. An initial technical report on this property will be filed in connection with the Spin-Out.
Loonie property -- Guilder target
A 3.5 km anomaly interpreted as the extension of a copper -gold prospect now supported with IP
geophysics
The Guilder target occupies the north-central portion of the Loonie property, approximately 50 km south
of Dawson City, and is interpreted as the northwestern strike extension of a copper-gold prospect. The
connection is supported by a continuous 3.5 km long, arcuate Cu -Mo-Au-Zn-Pb soil anomaly that trends
northwest-southeast across both properties and displays a classic metal zonation: gold -dominant at the
northwestern end, transitioning to copper-dominant, with lead and zinc forming a peripheral halo around
the copper core.
Prospecting has uncovered malachite and chalcocite mineralization hosted by quartz -feldspar-biotite
schist near an augen gneiss contact. Rock samples from this showing returned 1,115 ppm Cu and 6.1 g/t
Ag, confirming that meaningful copper and silver grades exist at surface.
In 2025, White Gold completed a 13 -line gradient IP survey with a single dipole -dipole line across the
Guilder target. Preliminary results have confirmed the presence of a central chargeability anomaly and a
second anomalous zone to the south, suggesting subsurface conductors are present beneath the surface
copper geochemistry. Interpretation is ongoing and will be used to define priority drill targets. The Guilder
target is an early-stage, drill-ready target.
Wolf property -- Aries and Taurus targets
The Aries target on the Wolf property is an interpreted porphyry system that is characterized by a central
zone of copper and molybdenum anomalies, surrounded by a large peripheral zone enriched in bismuth,
arsenic, lead and zinc. This forms a footprint measuring approximately fo ur km in length (northeast -
southwest) and three km in width (northwest -southeast). To the northeast, the Aries target transitions
from a gold -dominant system into a potential porphyry system. This area ’s molybdenum-in-soil values
reach as high as 51.4 ppm, with the bulk of the anomaly showing values above 5 ppm. Copper-in-soil
values peak at 923.9 ppm, with notable results such as 637.8 ppm, 630.8 ppm and 600.6 ppm Cu, located
near areas enriched in arsenic and bismuth. Previous drilling on the property has been gold -focused and
the property remains largely untested and prospective for several critical minerals including Mo and Cu.
The Wolf property is located east of the White River, approximately 120 km south-southwest of Dawson
City and 35 km west of the White Gold project. Two main target areas have been identified on the
property, the Aries and Taurus targets. The area is predominantly underlain by hornblende-biotite diorite
intruded by medium -grained and megacrystic K -feldspar granites. These intrusions are as sociated with
widespread biotite and potassic alteration, which are key indicators of potential porphyry mineralization.
To the north and northeast, the property is underlain by Late Cretaceous Carmacks volcanic units,
including andesite and basalt flows, and siliciclastic basal conglomerates. Cu -Mo enrichment appears to
be localized along the contact between these volcanic units and the adjacent granites while gold
mineralization is concentrated in the southwestern part of the property (Taurus target) in shreddy biotite
and k -spar altered hornblende -biotite diorites. The Taurus target features a gold -in-soil anomaly that
spans approximately two km long by 0.5 km wide, with gold values reaching 358 ppb Au. The anomaly has
an arcuate shape, trending east -west in the southwest and curving northeast -southwest to the east. GT
Probe bedrock sampling returned gold values up to 1.22 g/t Au, with several samples exceeding 0.5 g/t
Au. In 2023 RAB drilling of the target returned gold values of up to 0.81 g/t Au over 15.24 m from 19.81m
(hole WLFTRS23RAB002) including 6.55 g/t Au over 1.52 m, along with 0.32 g/t Au over 30.47 m) from
13.72 m in hole WLFTRS23RAB002.
Hunker Property — Boxcar, Bum & Mint Pup Targets (Cu-Ag-Au-Pb-Zn)
Three distinct copper occurrences in the heart of the Klondike.
Situated in the historically productive Klondike Gold Fields roughly 25 km southeast of Dawson City, the
northern portion of the Hunker property hosts three separate copper occurrences — the Boxcar, Bum,
and Mint Pup targets — that together define a district-scale copper-silver system that has seen abundant
surface sampling but almost no systematic follow-up exploration.
The Boxcar target is interpreted as a Besshi -type volcanogenic massive sulphide (VMS) system hosted
within a northwest-trending fault zone. Trenching has encountered significant multi-metal mineralization,
including up to: 33.19 g/t Ag, 2.32% Cu, 1.78% Pb, and 0.30% Zn over 0.5 m, and 221.99 g/t Ag, 3.76% Cu,
14.4% Pb, and 0.24% Zn over 1.0 m. A 2021 prospecting sample from the fault zone returned copper
exceeding 10,000 ppm alongside 8,937 ppb Pb, 5,279 ppm Zn, and anomalous cobalt and silver, associated
with malachite, azurite, copper wad, goethite, hematite, and suspected cassiterite — a mineralogical
assemblage pointing to a well -preserved, near-surface system that warrants structural and geophysical
follow-up.
The Mint Pup target is the largest of the three primary anomalies; a broad Cu-Au soil anomaly measuring
approximately 2.4 km by 3.0 km straddling the ridges between Gold Bottom Creek and Hunker Creek, with
gold-in-soil values up to 1,096 ppb Au and copper-in-soil up to 475.9 ppm Cu. GT-Probe bedrock sampling
returned values to 1.195 ppm Au, with a 90 m section of 19 consecutive samples all grading above 0.02
ppm Au.
The Hunker property sits within one of the more productive placer gold drainages in the Klondike, where
Hunker Creek and its tributaries — including Gold Bottom Creek — have produced more than 1.8 million
crude ounces of gold since 1897 (van Loon, 2019). The diversity of copper, silver, lead, zinc, and gold
mineralization styles across the Boxcar, Bum, and Mint Pup targets points to a geochemically complex,
multi-element system that has never been systematically explored at depth.
Hayes Property — Isaac Target (Cu-Mo-Ag-Zn-Pb-Bi-W-Li)
Porphyry geochemical zonation across a 3.3 km footprint. Eight drill targets identified.
The Isaac target sits 38 km east of the Casino copper-gold deposit and is associated with Late Cretaceous
Prospector Mountain suite intrusives. Soil sampling across >1500 samples defines a geochemically zoned
multi-element anomaly spanning approximately 3.3 km east-west by 2.5 km north-south, with a Bi-As-Cu-
Mo-enriched core of roughly 1,200 m by 650 m surrounded by a broad halo of anomalous silver, lead, and
zinc.
Anomalous copper -in-soils occurs in the southern portion of the core, and a relatively small area of
anomalous molybdenum occurs near the core’s northern margin. Within the peripheral halo, silver-in-soil
values range from 1 ppm Ag to as high as 16.9 ppm Ag, including 12.3 ppm Ag, 12.2 ppm Ag, 11 ppm Ag,
10.2 ppm Ag, 9.8 ppm Ag, while values > 3 ppm Ag are very common. Also, within this halo, lead -in-soil
values occur as high as 3310.4 ppb Pb including 957.5 ppm Pb, 832.8 ppb Pb, 748 ppm Pb, 689.1 ppb Pb,
with associated zinc-in-soil values as high as 1747 ppb Zn including 1360 ppm Zn, 1137 ppm Zn, 941 ppm
Zn, 763 ppm Zn, 729 ppm Zn, and 713 ppm Zn.
Prospecting across the target in 2022 returned chalcopyrite and galena in direct association across
multiple rock types, confirming primary sulphide mineralization at surface. The strongest 2022 sample,
from chlorite -altered brecciated biotite -feldspar-quartz gneiss with disseminated cpy -gn in a zone of
epidote veining, returned 106 ppm Mo, 731 ppm Cu, 27.3 ppm Ag, 1,048 ppm Pb, and 3,100 ppm Zn.
Other notable 2022 results include a py -gn-cpy mineralized silicified rhyolite returning 20.6 ppm Ag and
2,625 ppm Pb, and a silicified felsic dyke with fresh chalcopyrite returning 814 ppm Cu and 16.7 ppm Ag.
Lithium is elevated broadly across the target with multiple rock samples returning values exceeding 800
ppm Li, including two samples returning over limits of greater than 2,000 ppm Li hosted in diorite, gneiss,
and rhyolite. Follow-up gridded rock sampling across 88 samples in 2024 validated the 2022 results and
returned values up to 67 ppm Mo from a diorite intrusion, 459 ppm Cu, 1,954 ppm Zn, 3,778 ppb Ag, 345
ppm Bi, and 117 ppm W. Stockwork veining is described across multiple stations and fluorite has been
identified in silicified rhyolite. Hyperspectral analysis of 2022 rock samples identified phyllic and potassic
alteration in the core with propylitic overprinting on the southern margins.
In 2023, two deep -penetrating IP -resistivity lines delineated eight discrete chargeability anomalies
beneath the target. The Isaac target has never been drilled.
Toonie Property — Deux Target (Au-Cu-Zn-Mo-Ag)
RAB drilling has confirmed broad multi -element mineralization in all four holes. P rospective porphyry
signatures identified.
The Toonie property lies approximately 45 km south -southeast of Dawson City and is predominantly
underlain by Late Cretaceous Carmacks volcanic rocks; a package that has increasingly been recognized
as a host for copper and polymetallic mineralization across the region. Exploration on the Deux target has
progressed through two systematic phases.
In 2018, initial GT Probe sampling outlined a broad but coherent, low-level multi-element surface anomaly
(0.258 g/t Au, 4.6 g/t Ag, 412 ppm Cu, 1,663 ppm Zn, 843 ppm Pb, and 71 ppm Mo), spatially associated
with resistivity boundaries and interpreted structural controls in the volcanic package. A follow -up 2023
RAB drilling program confirmed widespread, shallow multi-element mineralization in all four holes. Hole
TOODEU23RAB001 returned 24.4 m of 0.235 g/t Au and 525.4 ppm Cu from surface, including 6.1 m
grading 0.327 g/t Au and 598.3 ppm Cu, plus a separate 4.57 m interval with 3,525 ppm Zn. Hole
TOODEU23RAB003 intersected 76.2 m averaging 386 ppm Cu, with individual samples up to 676.4 ppm
Cu and 2,368 ppm Zn, demonstrating the scale of the copper–zinc system.
Quartz veining, sericite and chlorite alteration, and oxidized fractures are most common in intervals
carrying the strongest copper and zinc values. Geochemical work on the Carmacks volcanic units indicates
porphyry-style prospectivity and a zoned metal pattern, with an Au–Mo–Cu core and more distal Zn–Pb–
Ag, consistent with a buried intrusion-related system. Although gold remains the primary focus, the broad
Cu–Zn intervals provide a strong critical-minerals rationale for including Toonie in the Spin-Out as an early-
stage, drill-ready Au–Cu–Zn target.
Qualified Person
Steven Walsh, P.Geo. and Senior Geologist for the Company is a “qualified person” as defined under
National Instrument 43-101 – Standards of Disclosure of Mineral Projects and has reviewed and approved
the content of this news release.
About White Gold Corp.
The Company owns a portfolio of 15,364 quartz claims across 21 properties covering 305,102 hectares
(3,051 km2) representing approximately 40% of the Yukon’s emerging White Gold District. The Company’s
flagship White Gold project hosts four near -surface gold deposits which collectively contain resource
estimate of 1,732,300 ounces of gold in indicated resources (3 5.2 million tonnes grading 1.53 grams per
tonne gold) and 1,265,900 ounces of gold in inferred resources (32.2 million tonnes grading 1.22 g/t Au)
(see the Company's news release dated October 6, 2025)(1)(2). Regional exploration work has also produced
several other new discoveries and prospective targets on the Company’s claim packages which border
sizable gold discoveries including the Coffee project owned by Fuerte Metals with Measured and Indicated
Resources of 80.0.2 Mt grading 1.15 g/t Au for 2.96 million ounces of gold, and Inferred Resources of 21.2
Mt grading 1.17 g/t Au for 0.80 million ounces gold (2)(3)(4), and Western Copper and Gold Corp oration’s
Casino project which has Measured and Indicated Resources of 2,490.7 Mt grading 0.18 g/t Au, 0.14% Cu
for 14.8 million ounces of gold and 7.6 billion pounds of copper, and Inferred Resources of 1,412.5 Mt
grading 0.14 g/t Au, 0.10% Cu for 6.3 million ounces of gold and 3.1 billion pounds of copper(2)(3)(5).
For more information visit www.whitegoldcorp.ca.
(1) See October 6, 2025 News Release “White Gold Corp. Files Technical Report Demonstrating Significant 44% Increase in
Indicated Resources to 1,732,300 oz Gold (35.2 million tonnes grading 1.53 g/t) and 13.4% Increase in Inferred Resources to
1,265,900 oz Gold (32.2 million tonnes grading 1. 22 g/t) at its Flagship White Gold Project, Yukon, Canada”
https://www.whitegoldcorp.ca/news/white-gold-corp-files-technical-report-demonstrating-significant-44-increase-in-
indicated-resources-to-1732300-oz-gold-352-million-tonnes-grading-153-gt-and-134-increase-in-inferred-resources-to-
1265900-oz-gold-322-million-ton.
(2) All numbers are rounded. Overall numbers may not be exact due to rounding.
(3) The QP has been unable to verify the information. The information is not necessarily indicative to the mineralization on the
properties that are subject of the disclosure.
(4) See Fuerte Metals press release titled “Fuerte Announces Transformational Acquisition of the Coffee Project from Newmont
Corporation” dated September 15, 2025.
(5) See Western Copper and Gold Corporation technical report titled “Casino project, Form 43-101F1 Technical Report Feasibility
Study, Yukon Canada”, Effective Date June 13, 2022, Issue Date August 8, 2022, NI 43 -101 Compliant Technical Report prepared
by Daniel Roth, PE, P.Eng., Mike Hester, F Aus IMM, John M. Marek, P.E., Laurie M. Tahija, MMSA-QP, Carl Schulze, P.Geo., Daniel
Friedman, P.Eng., Scott Weston, P.Geo., available on SEDAR+.
(6) See December 1, 2025 News Release "Selkirk Copper Announces Initial Drill Results - Successfully Expands Minto North West
Zone with a High-Grade Intercept of 5.21% Cu, 0.47 g/t Au, 26.68 g/t Ag over 8.7m within a broader zone of 2.39% Cu, 0.32 g/t
Au and 11.61 g/t Ag over 23.4 m in drill hole 25SCM001.