White Gold Corp. Encounters Gold Mineralization on Multiple Targets; Drills 105 g/t Au over 1.53m at Titan; Trenches 2.16 g/t Au over 21.0m including 5.69 g/t Au over 3.0m and 4.15 g/t Au over 5.0m at Vertigo and Pit Samples up to 18.2
White Gold Corp. Encounters Gold Mineralization on Multiple Targets; Drills
105 g/t Au over 1.53m at Titan; Trenches 2.16 g/t Au over 21.0m including 5.69
g/t Au over 3.0m and 4.15 g/t Au over 5.0m at Vertigo and Pit Samples up to 18.2
g/t Au & 33.6 g/t Ag at Notorious, Yukon Canada
TORONTO, Jan. 21, 2021 (GLOBE NEWSWIRE) -- White Gold Corp. (TSX.V: WGO, OTC: WHGOF, FRA: 29W) (the
“Company”) is pleased to announce results for surface sampling, mechanical trenching and rotary air blast (“RAB”) drilling
programs completed on its road accessible JP Ross (“JPR”) property which identified additional and widespread structurally
controlled gold mineralization at multiple targets, and RAB, reverse circulation (“RC”) and diamond drilling results on its Titan
project on the Hen property, Yukon Canada. This work formed part of the Company’s 2020 exploration program backed by
strategic partners Agnico Eagle Mines Limited (TSX: AEM, NYSE: AEM) and Kinross Gold Corp (TSX: K, NYSE: KGC) on its
extensive 420,000 hectare land package in the prolific White Gold District, Yukon, Canada.
Highlights Include:
• At the JPR property, additional gold mineralization encountered on multiple targets hosted within a regional scale
structurally controlled mineralized system.
• Trenching at the Vertigo target identified a new mineralized zone grading 2.16 g/t Au over 21.0m including higher grade
subzones of 5.69 g/t Au over 3.0m and 4.15 g/t Au over 5.0m, associated with a southeast trending gold-in-soil
geochemistry anomaly which remains open along strike.
• JPR RAB drilling encountered gold mineralization in every hole with mineralized zones ranging from 0.20-3.29 g/t Au
over widths of 1.5-9.1m.
• Rock samples from a hand dug pit collected on the recently discovered Notorious target confirmed the presence of high
-grade gold mineralization. The two deepest samples at 1.4m and 1.5m returned the highest values including 18.2 g/t
Au & 33.6 g/t Ag and 4.376 g/t Au & 9.8 g/t Ag, respectively.
• Structural analysis of the Notorious target area based on LiDAR and magnetics confirms a favourable structural
geological setting.
• At Titan, RC and diamond drill holes were completed 8m and 4m respectively from RAB hole HENTTN19RAB-002
(72.81 g/t Au over 6.09m) to better quantify the grade and width of mineralization. Hole HENTTN20RC-001 intersected
105.0 g/t Au over 1.53m from 12.19m depth & HENTTN20D-003 intersected 37.40 g/t Au over 1.5m from 14.0m depth.
• Titan diamond drilling intersected multiple felsic dykes up to 10m wide, locally with well-developed quartz veinlets with
potassium feldspar haloes and trace pyrite and galena, confirming intrusive activity and potential for buried porphyry
style alteration and mineralization.
• Source of magnetic highs on Titan target is magnetite-rich zone(s) with anomalous copper near the base of a mafic
unit.
• Significant additional results from the 2020 exploration program to be announced in the coming weeks.
• View the 2021 VRIC interview with David D’Onofrio, CEO and Shawn Ryan, Chief Technical Advisor and other newly
posted video updates and media at: https://whitegoldcorp.ca/media/videos/.
Figures accompanying this news release can be found at: http://whitegoldcorp.ca/investors/exploration-highlights/.
All gold intersections reported herein are measured drill or trench lengths as insufficient work has been carried out to
determine true widths.
“We are pleased to have encountered further additional gold mineralization across multiple recently identified zones as well as
confirmed the high-grade mineralization on the newly discovered Notorious target, providing further indication that the abundant
gold mineralization is part of a robust regional scale structurally controlled system on the JP Ross Property. This program has
also provided valuable insight into the orientation and geometry of the mineralized systems, information that has been
incorporated into our scientific and data driven methodology to define drill targets for the upcoming season. We look forward to
releasing additional results from our 2020 exploration program and continuing to advance our projects in 2021,” stated David
D’Onofrio, CEO.
AME Roundup 2021
The Company is pleased to invite interested parties to its virtual booth at the AME Remote Roundup 2021 Virtual Conference.
Learn more about the Company’s unique district-scale gold investment opportunity with significant defined resources and new
discovery potential in the emerging White Gold District, Yukon, Canada. The virtual booth includes highlights of 2020
achievements, in-depth interviews by management, along with an interactive chat and a discussion of what investors can look
forward to in 2021.
Date: January 18th to 22nd 2020, 9:00AM PST to 4:00PM PST
Registration: https://roundup.amebc.ca/
Event Agenda: https://roundup.amebc.ca/schedule-at-a-glance/
JPR Property
The JPR is a large road accessible property covering 76,385 hectares centered on the famed Henderson Creek placer gold
area located north of the Stewart River and east of the Yukon River. The property is located approximately 80km south of
Dawson City and 30km northeast of the Company’s flagship Golden Saddle and Arc deposits which have a mineral resource of
1,139,900 ounces Indicated at 2.28 g/t Au and 402,100 ounces Inferred at 1.39 g/t Au (1). Most of the JPR property is underlain
by a metamorphosed interlayered Paleozoic sequence comprising Devonian ‐Mississippian clastic sedimentary rocks, mafic
and felsic volcanic rocks, and intrusive rocks. Volcanic rocks of the Late Cretaceous Carmacks Group occur in the northern
and east central portions of the property. Gold-related alteration and mineralization on the JPR property is predominantly
structurally controlled and the area shows a complex structural history. Three primary fault systems are recognized, which
from oldest to youngest are: 1) NNW to N-trending thrust faults; 2) WNW to E-W-trending sinistral faults; and 3) NE to NNE-
trending sinistral and normal faults. The WNW to E-W-trending sinistral fault systems represent the best potential for orogenic
gold, and the younger NE to NNE-trending sinistral and normal faults may potentially host porphyry-style copper-gold
mineralization. Multiple gold-in-soil anomalies and target areas have been identified across the property, and recent drilling has
confirmed gold mineralization with significant grades and widths, including 5.45 g/t Au over 4.57m in hole JPRNF19RAB-002 at
North Frenzy, 5.44 g/t Au over 4.57m in hole JPRSF19RAB-005 at Stage Fright, 3.42 g/t Au over 7.62m in hole
JPRSAB19RAB-011 at Sabotage, and 9.61 g/t Au over 4.15m in hole JPRVER19D0005 at Vertigo. Geochemical associations
with gold appear to be target specific with mineralization occurring as Au-only, or associated with any combination of Pb, Bi,
As, Ag, Cu, Te and Sb. Common accompanying sulphide minerals include pyrite, arsenopyrite and galena. A summary of
2020 exploration highlights and related historical results on the JPR property is shown in Figure 1.
Trenching Program
Eleven trenches totalling 384m were excavated utilizing a CanDIG mini excavator on 4 separate targets including Frenzy,
Sabotage, Vertigo and West Vertigo to test gold-in-soil and/or GT Probe anomalies. In general, the CanDIG was used in areas
with steep slopes where the larger Kubota excavator was unable to operate safely (see Company news release dated October
22, 2020). The locations of the 2020 CanDIG trenches are shown in Figure 2 and significant results are summarized below.
Two trenches were excavated at the Vertigo target proximal to previously encountered mineralization, with trench
JPRVER20T020 returning the most significant results of the trenching program with 2.16 g/t Au over 21.0m which included two
higher grade subzones of 5.69 g/t over 3.0m and 4.15 g/t Au over 5.0m. The trench ended in mineralization to the south, so the
zone remains open in that direction. The mineralization is hosted in vuggy oxidized biotite-quartz-feldspar gneiss (BQFG)
containing minor pyrite. The location of trench JPRVER20T020 relative to previous drilling is shown in Figure 3, which shows
that the mineralization is associated with a southeast-striking gold-in-soil anomaly that remains open along strike. Future
exploration at the Vertigo target will be performed to test the strike potential of this zone.
Six trenches were excavated at the Frenzy target with 3 trenches encountering gold in the range of 0.14 – 0.57 g/t Au over
widths of 1.0-10.0m. Trench JPRFRE20T009 contained one zone grading 2.35 g/t Au over 1.5m within a broader zone of 0.53
g/t Au over 10.0m. Mineralization in trench JPRFRE20T009 is associated with disseminated pyrite in weakly sericitized BQFG
and/or disseminated and fracture-controlled pyrite in oxidized and silicified BQFG. Trench JPRFRE20T012 cut a zone grading
0.57 g/t Au over 3.0m which is associated with oxidized pyrite in brecciated and quartz-veined graphitic quartzite. Both
trenches JPRFRE20T009 and JPRFRE20T012 ended in mineralization, with the zones remaining open.
A single trench, JPRSAB20T030 was excavated at the Sabotage target which returned 2 separate zones of anomalous gold
mineralization, returning 0.99 g/t Au over 1.0m and 0.22 g/t Au over 2.0m. The mineralization is hosted in a chloritized BQFG
with quartz-carbonate veins and disseminated pyrite.
Rotary Air Blast (RAB) Drilling
Thirteen RAB holes totalling 614.8m were drilled on 5 separate targets including Stage Fright, North Frenzy, Sabotage, North
Sabotage and Vertigo. Hole locations are shown in Figure 4 and significant results are summarized below.
Four holes were drilled at Stage Fright with all holes encountering gold zones ranging from 0.20 – 1.27 g/t Au over widths of
1.52-9.14m. Hole JPRSF20RAB-006 intersected 0.48 g/t Au over 9.14m from 7.62m depth and JPRSF20RAB-007 returned
0.75 g/t Au over 6.10m from surface, including 1.27 g/t Au over 3.05m. Mineralization in holes JPRSF20RAB-006 and -007 is
hosted in variably oxidized BQFG. Hole JPRSF20RAB-008 intersected 0.85 g/t Au over 1.52m from 6.10m depth and
JPRSF20RAB-009 returned 0.55 g/t Au over 6.10m from 16.76m depth. Mineralization in both holes is hosted in heavily
oxidized and chloritized quartz-feldspar-biotite gneiss (QFBG).
Four holes were drilled at North Frenzy with all holes intersecting gold zones grading from 0.28-1.71 g/t Au and ranging in
thickness from 1.52-9.14m. Hole JPRNFR20RAB-004 intersected 0.57 g/t Au over 4.57m from 7.62m depth and 0.49 g/t Au
over 9.14m from 21.34m depth. Mineralization in hole JPRNFR20RAB-004 is hosted in moderately oxidized BQFG with quartz
veins and pyrite. Hole JPRNFR20RAB-005 intersected 1.03 g/t Au over 1.53m from 1.52m depth, JPRNFR20RAB-006 returned
0.59 g/t Au over 6.10m from 7.62m depth, and JPRNFR20RAB-007 intersected 0.73 g/t Au over 6.10m from 15.24m depth
including 1.31 g/t Au over 3.05m. Mineralization in hole JPRNFR20RAB-005 is hosted in weakly oxidized plagioclase-biotite
gneiss with quartz veins, and in holes JPRNFR20RAB-006 and -007 is associated with arsenopyrite in heavily oxidized quartz-
mica schist and heavily oxidized BQFG respectively.
Three holes drilled at Sabotage encountered gold mineralization in potassically altered felsic gneiss ± quartz veins and
disseminated pyrite, with gold grades ranging from 0.55-3.10 g/t Au over widths of 1.52-3.05m. The best mineralization was
intersected in hole JPRSAB20RAB-016 which returned 3.10 g/t Au over 1.52 from 10.67m depth.
Hole JPRNSAB20RAB-001 drilled at North Sabotage intersected a gold zone returning 0.20 g/t Au over 3.05m from 44.20m
depth, and hole JPRVER20RAB-026 at the Vertigo target intersected a zone grading 1.82 g/t Au over 3.05m from 1.52m depth
which is hosted in a quartz veined BQFG containing disseminated pyrite.
Notorious Target
As previously announced in the Company’s news release dated October 22, 2020, Notorious is a newly discovered target
located approximately 1.5km west of the North Frenzy, and 500m east of the intersection of two interpreted, property-scale
sinistral faults, the west-northwest (285°) striking Frenzy Fault and the northeast (065°) striking Fright Fault (Figure 5). Results
of initial GT Probe sampling in this area are very encouraging with multiple samples returning gold values in the range of 0.17
g/t Au to 24.4 g/t Au and trace up to 45.7 g/t Ag. The highest grade probe sample site at 24.4 g/t Au and 45.7 g/t Ag was
investigated by digging a 1.5m deep hand pit and a series of rock samples encountered at all depths were collected. The two
deepest samples at 1.4m and 1.5m depths returned the highest gold and silver values of 18.2 g/t Au and 33.6 g/t Ag and 4.376
g/t Au and 9.8 g/t Ag respectively, and the samples are also anomalous in copper and other elements including As, Bi, Te, W,
Mo, and Pb. This site is located at the end of a GT Probe line and remains open in that direction. Additional work planned for
the upcoming field season includes extending the GT Probe sampling, trenching and RAB drilling.
Titan Project
The Titan project is located on the Hen property approximately 70km south of Dawson City, contiguous to the JPR property
and 25km northeast of the Company’s flagship Golden Saddle and Arc deposits. The property is situated within a prolific
placer mining camp where abundant coarse placer gold has been recovered from creek gravels on North Henderson Creek
immediately east of the Titan.
The Titan project area is situated on a circular magnetic low feature with a diameter of approximately 600m, which
encompasses 6 discrete magnetic high anomalies measuring from 100m to 325m long. Although there is no outcrop in the
immediate area, the soil geochemistry signature is indicative of an underlying porphyry system with anomalous Cu-Mo-V-Bi-
Au and Fe/Ti ratio in the core and a Zn-Mn-Ca halo.
In 2019, soil sampling in the southwestern part of the target area over a magnetic high returned a high of 113 g/t Au, which is
the highest value ever recorded in the Company’s 400,000+ soil sample database. Rock grab samples from shallow pits in the
same area comprising sheared mafic to ultramafic rocks and massive magnetite contained fine-grained visible gold and
returned assays of 113 g/t Au, 497 g/t Au, and 605 g/t Au. Ground geophysical surveys show that the mineralization is
associated with a resistivity low, chargeability high, and magnetic high. In late 2019, the Company drilled 3 RAB holes totalling
221m to test the surface mineralization. Hole HENTTN19RAB-002 intersected a high-grade mineralized zone which returned
136.36 g/t Au over 3.05m. Additional information on the initial 2019 Titan discovery can be found in the Company’s news
release dated November 26, 2019.
2020 Drilling Program
The 2020 drilling program comprised 9 RAB holes totalling 832.1m, 1 RC hole for 115.8m, and 9 diamond drill holes totalling
1,924.5m (Figure 6). Significant results are summarized separately below for each type of drilling.
Reverse Circulation (RC) Drilling
A single RC hole, HENTTN20RC-001 was drilled 8m from hole HENTTN19RAB-002 to better quantify the grade and thickness
of the high-grade gold zone. The hole intersected a high-grade zone from 12.19-13.72m which returned 105.0 g/t Au over
1.53m. This high-grade zone occurs near the base of a magnetite zone in chlorite schist from 1.52-13.72m which contains
minor pyrite and anomalous copper (281–2270 ppm Cu) and gold (0.075-0.363 g/t Au).
Rotary Air Blast (RAB) Drilling
Four RAB holes were drilled to test magnetic highs similar to the one associated with the high-grade gold encountered in hole
HENTTN19RAB-002. This included holes HENTTN20RAB-004, -007, -008 and -009. Holes HENTTN20RAB-008 and -009 each
intersected 3m thick magnetite zones at shallow depths (< 25m) at the base of a mafic plagioclase biotite gneiss unit.
Anomalous copper (533-1143 ppm Cu) occurs over widths of 3-10m either associated with or directly below the magnetite
zones.
Four holes were drilled to test a northeast-striking gold and copper geochemical trend (soil ± GT Probe samples) along the
southern margin and east of the circular magnetic low. This included holes HENTTN20RAB-005, -006, -010 and -011. Hole
HENTTN20RAB-005 intersected a zone of anomalous copper (493-1307 ppm Cu) from surface to 19.8m, and hole
HENTTN20RAB-006 encountered multiple anomalous copper values (542-1437 ppm Cu) in zones ranging from 1.5m to 3m
thick from surface to 61m. Holes HENTTN20RAB-010 and -011 intersected several faults and oxidized zones, with both holes
being terminated short of their target depths due to challenging ground conditions.
A scissor hole, HENTTN20RAB-012 was drilled to the east to undercut the high-grade gold zone in hole HENTTN19RAB-002,
however this hole appears to have been drilled downdip and did not encounter the targeted mineralization. Significant gold
values were not encountered in these RAB holes.
Diamond Drilling
The diamond drilling program focused on testing the northern strike and down-dip extent of the high-grade gold zone
encountered in hole HENTTN19RAB-002, as well as the potential for buried porphyry alteration and mineralization along the
western margin of the circular magnetic low feature.
Holes HENTTN20D-001, -002 and -003 were drilled in the immediate area of the high-grade intersection in hole HENTTN19RAB
-002. Holes HENTTN20D-001 and -002 were collared approximately 25m east and 25m north of HENTTN19RAB-002
respectively, and HENTTN20D-003 was drilled with 5 to 8m of holes HENTTN19RAB-002 and HENTTN20RC-001. Hole
HENTTN20D-001 intersected a magnetite zone with anomalous copper (484-2290 ppm Cu) from 22.50-27.07m. HENTTN20D-
002 intersected a mineralized zone grading 2.52 g/t Au over 1.64m, but no discrete magnetite zone, and HENTTN20D-003
intersected a zone of high-grade gold from 14.00-15.50m which returned 37.40 g/t Au over 1.5m. This high-grade zone occurs
at the base of a magnetite zone from 2.50-15.50m which contains minor pyrite and anomalous copper (455–2100 ppm Cu).
The broader mineralized zone from 2.50-17.26m graded 4.14 g/t Au over 14.76m, which includes a higher grade subinterval of
9.48 g/t Au over 6.26m from 11.00-17.26m. The composite grades of these broader mineralized zones are heavily weighted on
the single high-grade (37.40 g/t Au) sample, with gold values elsewhere in the zone ranging from 0.161-1.03 g/t Au. A
comparison of results for diamond drill hole HENTTN20D-003, RC hole HENTTN20RC-001 and RAB hole HENTTN19RAB-002
is discussed separately below.
Hole HENTTN20D-004 was drilled 190m north of the high-grade gold zone to test for a strike extension along a similar
magnetic high. The hole intersected a sheared magnetite-rich zone from 17.31-29.56m containing 5-15% pyrite and locally
minor chalcopyrite and specks of azurite. Copper values within this zone range from 1620-7480 ppm Cu, averaging 3592 ppm
Cu over 12.25m. Gold values are anomalous averaging 0.16 g/t Au over 6.05m from 20.50-26.55m.
Holes HENTTN20D-005, -006 and -008 were drilled to test the structure and potential for buried porphyry alteration and
mineralization at the western margin of the circular magnetic low feature. The holes intersected multiple felsic dykes up to
10m wide locally with well-developed quartz veinlets with potassium feldspar haloes and trace pyrite and galena. No
significantly large porphyry intrusion was encountered but may exist at depth elsewhere within the target area.
Hole HENTTN20D-007 was collared approximately 175m WNW of the high-grade gold zone and drilled at an azimuth of 110° to
test several modeled structures / fault zones and hole HENTTN20D-009 was drilled adjacent to RAB holes HENTTN20RAB-
010 and -011 to fully test the oxidized faults zones and anomalous gold and copper soil and GT probe geochemistry. Neither
hole returned any significant gold values.
Comparison of Results for Holes HENTTN19RAB-002, HENTTN20RC-001 and HENTTN20D-003
Holes HENTTN20RC-001 and HENTTN20D-003 were drilled adjacent to hole of HENTTN19RAB-002 to better quantify the grade
and thickness of the high-grade gold zone and to compare results for all three drilling methods. All 3 holes show a very good
correlation in terms of the extents of the magnetite zone and associated anomalous elements which include gold, copper,
zinc, tellurium and others. However, the RC and diamond drilling confirmed that the high-grade gold mineralization is restricted
to a narrow (1.5m) interval at the base of the magnetite zone, and gold values in the remainder of the overlying zone are low-
grade (0.15-0.58 g/t Au).
RAB hole HENTTN19RAB-002 showed a broad zone of low-grade to anomalous gold extending well below the high-grade
zone, but it is now apparent that this downhole “tail” is a result of open hole contamination related to the RAB drilling. The
friable nature of the surficial magnetite at Titan is believed to be a strong contributing factor, and contamination has not been
observed in RAB drilling elsewhere on other targets.
QA/QC
Analytical work for the 2020 trenching and RAB drilling programs was performed by Bureau Veritas Canada Ltd., an
internationally recognized analytical services provider, at its Vancouver, British Columbia laboratory. Sample preparation was
completed in two stages: crushing to a reject was carried out at its Whitehorse, Yukon facility, after which a 250 gram split
was sent to the Vancouver, BC facility for pulverization. All trench and RAB samples were prepared using procedure PRP70-
250 (crush 70% less than 2mm, riffle split off 250g, pulverize split to better than 85% passing 75 microns) and analyzed by
method FA430 (30g fire assay with AAS finish) and AQ-201 (15g, aqua regia digestion and ICP-ES/MS analysis). Samples
containing >10 g/t Au were reanalyzed using method FA530 (30g Fire Assay with gravimetric finish).
Analytical work for 2020 diamond drilling and RC drilling was performed by ALS Canada Ltd., an internationally recognized
analytical services provider, at its North Vancouver, British Columbia laboratory. Sample preparation was carried out at its
Whitehorse, Yukon facility. All diamond drill core and RC samples were prepared using procedure PREP-31H (crush 70% less
than 2mm, riffle split off 500g, pulverize split to better than 85% passing 75 microns) and analyzed by method Au-AA23 (30g
fire assay with AAS finish) and ME-ICP41 (0.5g, aqua regia digestion and ICP-AES analysis). Samples containing >10 g/t Au
were reanalyzed using method Au-GRAV21 (30g Fire Assay with gravimetric finish).
The reported work was completed using industry standard procedures, including a quality assurance/quality control (“QA/QC”)
program consisting of the insertion of certified standards, blanks and duplicates into the sample stream.
About RAB Drilling
The Company successfully utilizes rotary air blast (RAB) drilling as an efficient and cost effective first-pass exploration drilling
technique on its White Gold District projects, Yukon. The RAB drill rig is an ultra-portable, wireless remote-controlled rubber
tracked drill that uses compressed air to actuate a downhole hammer and can drill holes at a wide range of angles (50-90°)
and to a length of approximately 100 meters. Rock cuttings are returned to surface under pressure between the drill pipe and
wall of the open hole, so samples may under certain circumstances incur cross contamination. Once completed each RAB
hole is surveyed with a borehole optical televiewer which provides high-resolution digital imagery of the hole walls and key
structural orientation data on lithological contacts, fractures, foliations, veins, etc. The Company views RAB drill results as an
indication of the presence and general grade of gold at a given target, and encouraging results are followed up with either
reverse circulation (RC) or diamond drilling in order to quantify grades and thicknesses of mineralized zones.
About White Gold Corp.
The Company owns a portfolio of 21,207 quartz claims across 32 properties covering over 420,000 hectares representing over
40% of the Yukon’s prolific White Gold District. The Company’s flagship White Gold property hosts the Company’s Golden
Saddle and Arc deposits which have a mineral resource of 1,139,900 ounces Indicated at 2.28 g/t Au and 402,100 ounces
Inferred at 1.39 g/t Au(1). Mineralization on the Golden Saddle and Arc is also known to extend beyond the limits of the current
resource estimate. The Company’s recently acquired VG Deposit also hosts a historic Inferred gold resource of 230,000
ounces at 1.65 g/t Au (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 Newmont
Corporation with Measured and Indicated Resources of 2.17 Moz at 1.46 g/t Au, and Inferred Resources of 0.50 Moz at 1.32
g/t Au (3), and Western Copper and Gold Corporation’s Casino project which has Measured and Indicated Resources of 14.5
Moz Au and 7.6 Blb Cu and Inferred Resources of 6.6 Moz Au and 3.3 Blb Cu (3). For more information visit
www.whitegoldcorp.ca.
(1) See White Gold Corp. technical report titled “Technical Report for the White Gold Project, Dawson Range, Yukon Canada”,
dated July 10, 2020, available on SEDAR.
(2) See Comstock Metals Ltd. technical report titled “NI 43-101 TECHNICAL REPORT on the QV PROJECT”, dated August
19, 2014, available on SEDAR.
(3) Noted mineralization is as disclosed by the owner of each property respectively and is not necessarily indicative of the
mineralization hosted on the Company’s property.
Qualified Person
Terry Brace, P.Geo. and Vice President of Exploration 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.
Cautionary Note Regarding Forward Looking Information
This news release contains "forward-looking information" and "forward-looking statements" (collectively, "forward-looking
statements") within the meaning of the applicable Canadian securities legislation. All statements, other than statements of
historical fact, are forward-looking statements and are based on expectations, estimates and projections as at the date of this
news release. Any statement that involves discussions with respect to predictions, expectations, beliefs, plans, projections,
objectives, assumptions, future events or performance (often but not always using phrases such as "expects", or "does not
expect", "is expected", "anticipates" or "does not anticipate", "plans", “proposed”, "budget", "scheduled", "forecasts",
"estimates", "believes" or "intends" or variations of such words and phrases or stating that certain actions, events or results
"may" or "could", "would", "might" or "will" be taken to occur or be achieved) are not statements of historical fact and may be
forward-looking statements. In this news release, forward-looking statements relate, among other things, the Company’s
objectives, goals and exploration activities conducted and proposed to be conducted at the Company’s properties; future
growth potential of the Company, including whether any proposed exploration programs at any of the Company’s properties will
be successful; exploration results; and future exploration plans and costs and financing availability.
These forward-looking statements are based on reasonable assumptions and estimates of management of the Company at
the time such statements were made. Actual future results may differ materially as forward-looking statements involve known
and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of the
Company to materially differ from any future results, performance or achievements expressed or implied by such forward-
looking statements. Such factors, among other things, include:
the expected benefits to the Company relating to the exploration conducted and proposed to be conducted at the White Gold
properties; the receipt of all applicable regulatory approvals for the Offering; failure to identify any additional mineral resources
or significant mineralization; the preliminary nature of metallurgical test results; uncertainties relating to the availability and
costs of financing needed in the future, including to fund any exploration programs on the Company’s properties; business
integration risks; fluctuations in general macroeconomic conditions; fluctuations in securities markets; fluctuations in spot
and forward prices of gold, silver, base metals or certain other commodities; fluctuations in currency markets (such as the
Canadian dollar to United States dollar exchange rate); change in national and local government, legislation, taxation, controls,
regulations and political or economic developments; risks and hazards associated with the business of mineral exploration,
development and mining (including environmental hazards, industrial accidents, unusual or unexpected formations pressures,
cave-ins and flooding); inability to obtain adequate insurance to cover risks and hazards; the presence of laws and regulations
that may impose restrictions on mining and mineral exploration; employee relations; relationships with and claims by local
communities and indigenous populations; availability of increasing costs associated with mining inputs and labour; the
speculative nature of mineral exploration and development (including the risks of obtaining necessary licenses, permits and
approvals from government authorities); the unlikelihood that properties that are explored are ultimately developed into
producing mines; geological factors; actual results of current and future exploration; changes in project parameters as plans
continue to be evaluated; soil sampling results being preliminary in nature and are not conclusive evidence of the likelihood of
a mineral deposit; title to properties; ongoing uncertainties relating to the COVID-19 pandemic; and those factors described
under the heading "Risks Factors" in the Company's annual information form dated July 29, 2020 available on SEDAR.
Although the forward-looking statements contained in this news release are based upon what management of the Company
believes, or believed at the time, to be reasonable assumptions, the Company cannot assure shareholders that actual results
will be consistent with such forward-looking statements, as there may be other factors that cause results not to be as
anticipated, estimated or intended. Accordingly, readers should not place undue reliance on forward-looking statements and
information. There can be no assurance that forward-looking information, or the material factors or assumptions used to
develop such forward-looking information, will prove to be accurate. The Company does not undertake to release publicly any
revisions for updating any voluntary forward-looking statements, except as required by applicable securities law.
Neither the TSXV nor its Regulation Services Provider (as that term is defined in the policies of the TSXV) accepts
responsibility for the adequacy or accuracy of this news release.
Contact Information:
David D’Onofrio
Chief Executive Officer
White Gold Corp.
(647) 930-1880