Golden Ridge Drills a New Porphyry Cu-Au Discovery at Williams Zone; Hole HNK-18-001 Intersects 327 Meters Grading 0.31% Cu, 0.35 g/t Au, 1.94 g/t Ag; Additional Holes Drilled Along Strike Intersected Similar Mineralization, Additional Assays Pending
Golden Ridge Drills a New Porphyry Cu-Au Discovery at Williams Zone; Hole HNK-18-001 Intersects
327 Meters Grading 0.31% Cu, 0.35 g/t Au, 1.94 g/t Ag; Additional Holes Drilled Along Strike
Intersected Similar Mineralization, Additional Assays Pending
Kelowna, British Columbia – August 14, 2018 - Golden Ridge Resources Ltd. (“Golden Ridge” or the
“Company”) (TSXV: GLDN) is very pleased to announce a new alkalic Cu -Au porphyry discovery at its
Williams Zone prospect, located on the Company’s Hank project in BC’s golden triangle. HNK -18-001
intersected a broad interval of vein and disseminated Cu -Au-Ag mineralization, centered on a strongly
potassic altered monzonite intrusion. The newly discovered alkalic porphyry system is characterized by
bornite-chalcopyrite+/-digenite mineralized monzonite, intruding strong potassic altered intermediate
to mafic Stuhini volcanics hosting veined chalcopyrite and minor bornite mineralization. The steeply
dipping tabular monzonite intrusion has now been intersected in all four holes drilled in the Williams
Zone, indicating a strike of at least 200 metres. The Hydracore 2000 drills currently being utilized on the
Property have a maximum working depth of approximately 600 meters. The latest hole completed in the
Williams Zon e, HNK -18-007, ended in mineralized monzonite at 603.50 meters depth. Mineralization
appears to increase at depth. The system remains open along strike in both directions and at depth.
Assay results will be released as they are received. Photographs of min eralized intercepts from HNK -18-
001, for which assays have been received, as well as Williams Zone holes two and three (HNK -18-002
and HNK -18-005), for which assays are still pending, have been posted to the Company’s website. A
drilling plan view map (Fig ure 1) and cross -section (Figure 2) are presented below and have also been
posted to the Company’s website.
Highlights:
- New alkalic porphyry discovery has been intersected in multiple holes along a 200 meter strike
length to a depth of 585 meters below surface; open along strike and at depth.
- 0.31% Cu, 0.3 5 g/t Au, 1. 94 g/t Ag over 327.00 metres, from 72.00 to 399.00 metres in hole
HNK-18-001
o Including 0.45% Cu, 0.54 g/t Au, 3.33 g/t Ag over 75.10 metres from 105.00 to 180.10
metres.
o Including 0.45% Cu, 0.60 g/t Au, 2.90 g/t Ag over 62.50 meters from 259.50 to 322.00
meters
o Including 0.70% Cu, 0.90 g/t Au, 4.88 g/t Ag over 20 meters from 302.00 to 322.00
meters
- Potassic altered and mineralized monzonite has been intersected in the first four drills holes on
the Williams Zone, for which assays are pending for holes HNK-18-002, 005 and 007.
- The Williams Zone remains open along strike and at depth.
Table 1 – HNK-18-001 Significant Intercepts
Length (m)
Dip (deg) Hole ID From (m) To (m) Interval (m)1 Cu (%) Au (g/t) Ag (g/t)
425.81
-60o
HNK-18-001 72.00 399.00 327.00 0.31 0.35 1.94
incl. 105.00 180.10 75.10 0.44 0.54 3.33
incl. 259.50 322.00 62.50 0.45 0.60 2.90
incl. 302.00 322.00 20.00 0.70 0.90 4.88
1 The intervals reported in these tables represent drill intercepts and insufficient data is available at this time to state th e true thickness of
the mineralized intervals and all gold values are uncut.
Comment:
Chris Paul, Vice President of Explorati on fo r Golden Ridge, commented: "The size and grade of the
Williams Zone discovery are remarkable. Broad intervals of intense potassic alteration with bornite and
digenite indicate the presence of a large alkalic Cu -Au porphyry system at surface. Indications ar e that
only the top of the system has been intersected, including the presence of widespread phyllic (aka
quartz-sericite-pyrite) alteration at surface, which typically overlies porphyry Cu-Au systems, and exists
both above and lateral to the potassic altered monzonite at Williams. Copper mineralization also extends
for a considerable distance into the surrounding volcanic rocks, while the mineralized monzonite shows
good continuity along strik e and at depth. The initial magnetic survey conducted in 2017 suggested a
circular zone, 400 meters in diameter . It is now apparent that the mineralization forms a broad tabular
zone extending beyond at least the northern limit of the magnetic anomaly. The actual cause of the
circular magnetic anomaly remains unknown at this time, but is possibly a result of magnetite alteration
overlying a feeder stock at depth. We are very excited to continue testing the extens ions of the system
both along strike and at depth.”
IP Geophysical Survey on Williams Zone:
Two 3.0 km long IP lines, run on 250-meter centers across the Williams Zone have now been completed.
Processing of the field data is ongoing and preliminary results reveal a 0.8 km wide chargeability
anomaly, coincident with the ground magnetic anomaly at surface in the Williams Zone. The
chargeability anomaly plunges to the south , toward the Property’s lower alteration zone (LAZ) and
expands to over 1.6 km in width . Initial interpretations suggest that the quartz-sericite-carbonate-pyrite
alteration constituting the LAZ may represent a large alteration halo overlying the southern extension of
the Williams Cu-Au porphyry. The target remains open to the south, north and at depth, off the IP grid.
Additional lines are currently being planned.
Table 2 – Collar Information
Hole ID Assays UTM 83E UTM 83N Elevation Azimuth Dip Length (m)
HNK-18-001 Received 409367.9 6343935 1062 100 -60 425.81
HNK-18-002 Pending 409584.5 6343829 946.6 275 -60 453.24
HNK-18-005 Pending 409584.5 6343829 946.6 330 -60 550.77
HNK-18-007 Pending 409247.9 6343876 1070 45 -60 603.5
Quality assurance/quality control procedures:
All drill core was logged, photographed, cut and sampled by Golden Ridge personnel. Prior to shipment
to MS Analytical’s sample preparation facility in Terrace, B.C., certified reference material standards,
blanks and field duplicates were inserted at a ratio of approximately one in every 20 drill core samples.
Samples were prepared in Terrace by crushing the entire sample to 70 per cent passing minus two
millimetres, riffle splitting off one kilogram and pulverizing the split to better than 85 per cent passing
75 microns. After preparation in Terrace, the prepared pulps were shipped to MS Analytical’s analytical
laboratory in North Vancouver, B.C. The gold assays are determined by FAS-111 fire assay method which
reports results in parts per million (equivalent to grams per tonne). Any samples with a fire assay that
report gold concentrations equal to or higher than 10.0 g/t Au are analyzed by metallic screen method
(Au-SCR24).
Base metal assays are determined by IMS-230 4-acid digestion with ICP -AES/MS finish method , which
reports results as parts per million (ppm). All analyses that reach the overlimit of IMS-230 are reanalyzed
with an ore -grade method. The analytical results are verified with the application of industry -standard
quality control and quality assurance procedures.
Qualified Person
Exploration activities at the Hank Property are being supervised by Wade Barnes, the Company’s Project
Geologist and a Qualified Person as defined by National Instrument 43 -101. Wade Barnes is a PGeo
registered with the Association of Professional Engineers and Geoscientists of British
Columbia (APEGBC) and has verified the data, reviewed and approved this news release.
About Golden Ridge Resources:
Golden Ridge is a TSX -V listed exploration company engaged in acquiring and advancing mineral
properties located in British Columbia . Golden Ridge currently has an option to acquire a 100% interest
in the 1,700 -hectare Hank gold -silver-lead-zinc property located in the Golden Triangle district,
approximately 140 kilometres north of Stewart , British Columbia. Golden Ridge may earn the 100%
interest in the Hank property by performing $1.7 M of exploration work by the end of 2018. For more
information please contact:
Golden Ridge Resources Ltd.
Mike Blady
Chief Executive Officer
Tel: (250) 768-1168
Website: www.goldenridgeresources.com
Cautionary Statement Regarding Forward Looking Statements
This release includes certain statements that may be deemed to be "forward -looking statements". All
statements in this release, other than statements of historical facts, that address events or developments
that management of the Company expects, are forward-looking statements. Although management believes
the expectations expressed in such forward -looking statements are based on reasonable assumptions, such
statements are not guarantees of future performance, and actual results or developments may differ
materially from those in the forward -looking statements. The Company undertakes no obligation to update
these forward-looking statements if management's beliefs, estimates or opinions, or other factors, should
change. Factors that could cause actual results to differ materially from those in forward-looking statements,
include market prices, exploration and development successes, continued availability of capital and
financing, and general economic, market or business conditions. Please see the public filings of the Company
at http://www.sedar.com/ for further information.
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.
409300 E
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Figure 2. Hank
Project Cross-
Section A-A’
News Release 08-14-2018
100m
1.29g/t
1.28g/t
Stuhini Volcanic Rocks
Mineralized Monzonite
LEGEND
HNK-18-001
327m of 0.31% Cu, 0.35g/t Au, 1.94g/t Ag
75.10m of 0.44% Cu, 0.54g/tAu, 3.33g/t Au
incl.
62.50m of 0.45% Cu, 0.60g/tAu, 2.90g/t Au
20m of 0.70% Cu, 0.90g/tAu, 4.88g/t Au
425.8 m
HNK-18-001
Lim
it of Potassic Alteration
327m of 0.31%Cu, 0.35g/t Au, 1.94g/t Ag
incl.
incl.
75.10m of 0.44%Cu, 0.54g/t Au, 3.33g/t Ag
62.50m of 0.45%Cu, 0.60g/t Au, 2.90g/t Ag
20m of 0.70%Cu, 0.90g/t Au, 4.88g/t Ag