Klondike Gold Drills 7.57 g/t Au over 10.5 meters at Stander Zone
3123 – 595 BURRARD STREET
VANCOUVER, B.C. CANADA V7X 1J1
TELEPHONE: 604-609-6138
FAX: 604-609-6145
WWW.KLONDIKEGOLDCORP.COM
Klondike Gold Drills 7.57 g/t Au over 10.5 meters at Stander Zone
August 18, 2020 TSX Venture Exchange Symbol – KG
Vancouver, British Columbia, Canada, August 18, 2020, Klondike Gold Corp. (TSX.V: KG; FRA: LBDP; OTC:
KDKGF) (“Klondike Gold” or the “Company”) is pleased to announce results of Phase 2 and 3 diamond
drilling at the Stander Zone and Stander Zone ‘extensions’ (described in News Releases June 1, 2020 and
July 7, 2020) on the Company’s wholly owned 586 square kilometer Klondike District Property, Yukon
Territory. The drill program successfully constrained the geometry and boundaries of gold mineralization
and the consistency in grade of gold mineralization contributing information towards resource
delineation. Information obtained from results will be used to prioritize next phases of drilling scheduled
to commence in late August.
SUMMARY:
At the Stander Zone, EC20-350 intersected 7.57 g/t Au over 10.5 meters from 48.0 meters within
a larger envelope of 3.93 g/t Au over 21.0 meters from 46.0 meters, and EC20-349 intersected
3.04 g/t Au over 2.5 meters from 8.5 meters among others.
Phase 2 d rilling showed the geometry of gold -bearing quartz vein arrays is sub -horizontal
(previously one of two different possibilities), and the drilling also constrain s the position of the
Nugget Fault as shown in Figure 1. The short five-hole program all intersected near-surface gold
mineralization and successfully identified areas for further drilling.
Phase 3 drilling tested for possible parallel structural repeats of the Stander Zone to explain down-
slope gold-geochemical anomalies generated from GT-Probe deep overborne sampling. Three of
four holes contained weakly gold-mineralized quartz veins with the best, EC20-356, assaying 0.40
g/t Au over 1.5m from 4.5 meters. The GT-Probe anomalies remain unexplained.
Peter Tallman, President and CEO of Klondike Gold stated “The drilling has answered a question about the
gold veining orientation required to frame a resource model; it is sub -horizontal, and this result also
contributes important information for future targeting of the Stander Zone and adds confirmation to the
Company’s guiding geologic and structural model of gold mineralization in the Klondike. The Nugget Fault
is now interpreted to have multiple horizontal gold-bearing quartz vein arrays generated adjacent to the
fault, allowing the Company to explore the Nugget Fault along strike for high grade quartz vein areas at
surface as part of the overall objective to move beyond exploration and towards resource delineation”.
PHASE 2 STANDER ZONE DRILLING RESULTS
The Company has received assays from all five holes of the Phase 2 diamond drilling program targeting a
100-meter length of the Stander Zone along the Nugget Fault. The short five-hole program all intersected
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near-surface gold mineralization in all holes and successfully identified areas for further drilling. The best
result from the second hole drilled, EC20-350, intersected 7.57 g/t Au over 10.5 meters from 48.0 meters
within a larger envelope of 3.93 g/t Au over 21.0 meters from 46.0 meters downhole.
The longitudinal section below shows three ‘levels’ of quartz veining with depth, with individual gold
intersections in each drill hole ascribed a “Level” (counting from surface) in Summary of Phase 2 Results
in Table 1.
Figure 1: Longitudinal Section of Gold Mineralization with Phase 2 Drill Holes at Stander Zone (see Figure
2 plan map and location of “Stander Zone Lone Section” section line).
Table 1: Summary of Phase 2 Results:
Hole ID From (m) To (m) Au (g/t) Interval (m) QV Level
EC20-349 8.50 11.00 3.04 2.50 1
and also 15.00 16.00 3.10 1.00 1
EC20-350 15.00 17.00 3.63 2.00 1
and also 46.00 67.00 3.93 21.00 2
Including 48.00 58.50 7.57 10.50 2
EC20-351 40.10 42.40 0.44 2.30 2
EC20-352 7.00 10.50 1.92 3.50 1
and also 36.60 37.20 3.10 0.60 2
EC20-353 42.00 44.00 0.33 2.00 2
and also 62.00 64.00 0.61 2.00 3
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EC20-349 tested Level 1 only and successfully showed that the at- surface quartz veining to the East has
continuity to the near surface quartz veining to the west of the hole, and that the ‘Level 1’ quartz veining
is horizontal in orientation and easily accessible from surface.
EC20-350 tested Level 1 and Level 2 quartz veining and intersected both. The ‘Level 2’ intersection of 7.57
g/t Au over 10.5 vertical meters is within the main near- surface area of gold mineralization. Due to
topography, the ‘Level 2’ quartz veins shallow towards surface to the west.
EC20-351, EC20-352, and EC20-353 all successfully tested Level 1 and Level 2 quartz veining. EC20 -353
also encountered gold-bearing quartz veining at 62.0 meters consistent with correlation to the ‘Level 3’
veining.
Figure 2 below is a similar view as Figure 1, but shows geology and the localization of gold along the “Felsic
Schist” and “Intermediate Schist” contact termed the Nugget Fault within the Stander Zone. All the gold
so far has been intersected at or near surface. The Stander Zone remains open.
Figure 2: Stander Zone Compilation Longitudinal Section of Gold Mineralization. The pink zones are
mineralized intercepts from 2015 -2019, and the red are intercepts reported here. ( See Figure 2 plan
map and location of “Stander Zone Lone Section” section line).
Five short drill holes within the Stander Zone tested the near-surface sub-area where gold mineralization
outcrops over a 100-meter strike length shown in Figure 1. Intersections are assumed to be approximately
true thickness however work is ongoing and this interpretation may change. A total of 280.27 meters of
core was drilled. All holes had a - 90 degree angle from surface as noted in the following Drill Hole
Summary Table.
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Table 2: Drill Hole Summary , Phase 2 Stander Zone, 2020
Hole ID Easting Northing Azimuth Dip Depth (m)
EC20-349 585069 7085676 - 90 22.86
EC20-350 585051 7085678 - 90 70.10
EC20-351 585033 7085698 - 90 63.77
EC20-352 585017 7085677 - 90 52.51
EC20-353 585009 7085683 - 90 71.03
Total 280.27
Figure 3: Plan Map of Phase 2 Drilling at Stander Zone (2020 drilling only) showing Stander Fault (dashed
line) and location of section line for the Stander Zone longitudinal section (solid line) in Figure 1 and 2.
STANDER ZONE GEOLOGY SUMMARY
The Stander Zone is comprised of gold-bearing quartz veining localized adjacent to the northwest trending
“D3” Nugget Fault. Typically , gold occurs as visible 1mm size grains or larger, and can occur in massive
cm-scale clots and seams associated with carbonate, as example 1,009.5 g/t Au over 1.0 meter intersected
in EC19-267 in 2019, located in ‘Level 3’ of Figure 1. Stander Zone gold mineralization has been traced by
sampling gold-bearing outcrop and local floats in northwest -southeast direction for approximately five
kilometers. The Nugget Fault is associated with gold-in-soil anomalies and presents a distinct signature in
both very low frequency electromagnetic (“VLF -EM”) and magnetics surveys . The Nugget Fault is
interpreted as a major ‘second -order’ (“D3”) thrust fault, possibly a splay from the ‘first -order’ Bonanza
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Fault, cutting an anticlinal hinge that has subsequently been reactivated to create extension and brittle
gold-bearing quartz veins.
Gold mineralization at the Stander Zone is hosted by qu artz vein arrays immediately adjacent to the
Nugget Fault within competent, brittle felsic schist lithology. The Phase 2 drilling described here has
established the geometry of the quartz vein arrays as horizontal, and that multiple horizontal gold-bearing
vein arrays are developed approximately every 20 vertical meters adjacent the Nugget Fault within the
area tested. The Nugget Fault is approximately 45 -degree dipping and parallels the topographic slope
down towards Eldorado Creek. These quartz vein arrays form repeating parallel flat zones of gold
mineralization, as evident in the ‘longitudinal section’ sketch Figure 1 where three horizontal ‘levels’ of
gold-bearing quartz veining have been identified by drilling to date.
PHASE 3 RESULTS
Four holes EC20-354 to EC20-357 tested for possible parallel structural repeats of the Stander Zone to
explain down -slope gold -geochemical anomalies generated from GT -Probe deep overborne sampling.
Three of four holes contained weakly gold-mineralized quartz veins with the best, EC20-356, assaying 0.40
g/t Au over 1.5 meters from 4.5 meters downhole. The GT-Probe anomalies remain unexplained.
These results plus subsequent analysis suggests potential for additional mineralization lies along-strike of
the Stander Zone and structural repeats of this Zone across strike are interpreted to have lower potential.
Figure 4: Location Map of Phase 2 and 3 Stander Zone area 2020 Drilling.
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ASSAY PROTOCOLS
All 2020 drill holes referenced in this release produced NTW (5.71cm dia.) drill core. Assay samples from
drill core are cut using a diamond saw. Half the core sample interval is bagged, tagged, and sealed; the
other half is returned to the core box with a corresponding tag and retained for reference. Two gold
reference standards, two blank samples (a coarse and a fine), and a coarse sample duplicate per 100
samples, are routinely inserted as part of Klondike Gold’s quality assurance / quality control (“QA/QC”)
program, independent of and additional to the laboratory QA/QC program.
Sample bags are aggregated into rice bags, sealed, and submitted by Klondike Gold personnel to Bureau
Veritas Mineral Laboratories (“BV Labs”) preparation facility in Whitehorse, YT with chemical analysis of
sample pulps comp leted in Vancouver, British Columbia. Bureau Veritas Labs is an accredited ISO
9001:2008 full-service commercial laboratory.
At BV Labs each drill core sample is crushed to 70% passing 2 mm size. A 500 g subsample is pulverized
to 85% passing 75 microns size (200 mesh)(Code PRP70 -500). All samples of 500 g were sieved to 106
microns (140 mesh) for “metallic screen” assaying. The +140 mesh fraction is weighed and assayed for
gold by fire assay (“FA”) fusion with a gravimetric finish (Code FS631). A 30 g subsample of the -140 mesh
fraction is assayed for gold by fire assay (“FA”) fusion with an atomic absorption (“AA”) finish (Code
FA430). All over-limit results in excess of 10 ppm (10 g/t) for both silver and gold are re -assayed using a
30 g subsample and assayed by FA with a gravimetric finish (Code FA530-Au/Ag). Total gold grade is then
calculated using a weighted average of the plus and minus fraction assay results.
QUALIFIED PERSONS REVIEW
The technical and scientific information contained within this news release has been reviewed and
approved by Ian Perry, P.Geo., Vice-President Exploration of Klondike Gold Corp. and Qualified Person as
defined by National Instrument 43-101 policy.
ABOUT KLONDIKE GOLD CORP.
Klondike Gold Corp. is a Vancouver based gold exploration company advancing its 100%-owned Klondike
District Gold Project located at Dawson City, Yukon Territory, one of the top mining jurisdictions in the
world. The Klondike District Gold Project targets gold associated with district scale orogenic faults along
the 55-kilometer length of the famous Klondike Goldfields placer district. To date, multi- kilometer gold
mineralization has been identified at both the Lone Star Zone and Stander Zone, among other targets.
The Company is focused on exploration and development of its 586 square kilometer property accessible
by scheduled airline and government-maintained roads located on the outskirts of Dawson City, YT within
the Tr’ondëk Hwëch’in First Nation traditional territory.
ON BEHALF OF KLONDIKE GOLD CORP.
“Peter Tallman”
President and CEO
(604) 609-6138
E-mail: [email protected]
Website: www.klondikegoldcorp.com
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Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the
TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
Disclaimer for Forward-Looking Information
“This press release contains “forward-looking information” and “forward-looking statements” within the meaning of
applicable securities laws. This information and statements address future activities, events, plans, developments
and projections. All statemen ts, other than statements of historical fact, constitute forward- looking statements or
forward-looking information. Such forward- looking information and statements are frequently identified by words
such as “may,” “will,” “should,” “anticipate,” “plan,” “expect,” “believe,” “estimate,” “intend” and similar
terminology, and reflect assumptions, estimates, opinions and analysis made by management of Klondike in light of
its experience, current conditions, expectations of future developments and other factors which it believes to be
reasonable and relevant. Forward- looking information and statements involve known and unknown risks and
uncertainties that may cause Klondike’s actual results, performance and achievements to differ materially from those
expressed or implied by the forward-looking information and statements and accordingly, undue reliance should not
be placed thereon.
Risks and uncertainties that may cause actual results to vary include but are not limited to the availability of
financing; fluctuati ons in commodity prices; changes to and compliance with applicable laws and regulations,
including environmental laws and obtaining requisite permits; political, economic and other risks; as well as other
risks and uncertainties which are more fully descri bed in our annual and quarterly Management’s Discussion and
Analysis and in other filings made by us with Canadian securities regulatory authorities and available at
www.sedar.com. Klondike disclaims any obligation to update or revise any forward- looking information or
statements except as may be required.”