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Goldcliff Assesses Bulk Tonnage Potential at Nevada Rand

Corporate Updates

www.goldcliff.com

#400 – 789 W. Pender St.

Vancouver, B.C. V6C 1H2

Phone: 250-764-8879

Toll Free: 866-769-4802

GCN.TSXV www.directroyalty.com [email protected]

June 23, 2020

GOLDCLIFF ASSESSES BULK TONNAGE POTENTIAL at NEVADA RAND

Vancouver, B.C. – George Sanders, President of Goldcliff Resource Corporation (“Goldcliff” or the

“Company”) (GCN: TSX.V, GCFFF: OTCBB PINKS) reports that interpretation of exploration

results to date conclude that the Nevada Rand project has district scale potential to host

disseminated bulk tonnage gold deposits along with discreet, very high grade silver/gold sweet

spots. During the last twelve months Goldcliff conducted underground mapping and sampling in

the old Nevada Rand and Lone Star workings, detailed surface mapping and rock sampling, and

stream sediment geochemical sampling. Results of this work were reported in Goldcliff News

Releases dated October 9, 2019 and November 19, 2019. The Company also drilled seven

diamond core holes totaling 695.2 metres. Results of that programme were discussed in News

Release dated May 6, 2020.

A review and analysis of all data produced led to the following interpretations and conclusions. The

volcanic stratigraphy seems to be interleaved/interlayered andesite and rhyolite flows that are likely

intruded by sub-volcanic rhyolite plugs. The veins are more prominent in the andesite. The veining

occurs along quartz sericite corridors with silver dominant, gold and low level base metal

pathfinders. The historic bonanza grade mined at the Nevada Rand shaft, the Lone Star, and at

the Golden Pen and Blue Sphinx which are beyond the claim boundary, represent “smoke” and are

indicative of a larger mineralizing system. A classic disseminated, Walker Lane-style, gold-bearing

epithermal system is in the rhyolite flow portion of the stratigraphy. This mineralization is gold

dominant and contains pathfinders of arsenic, antimony and molybdenum.

A working genetic model is of an epithermal-type environment that is active all along the Northwest

trending Rand corridor from the Isabella Pearl (new open pit heap leach mine operated by Gold

Resource Corporation), 18 miles southeast, to Rand. This would be controlled and/or offset along

the classic Walker Lane style structural setting of right-lateral strike slip faults with low-angle faults

and volcanic contacts forming within the 1/2 grabens that are documented to occur throughout this

part of the Walker Lane. Disseminated, bulk tonnage gold deposits in the rhyolite flows have not

been previously targeted in the Rand district and represent a compelling exploration opportunity for

Goldcliff.

Realizing that the Rand district hosts previously unrecognized and unexplored opportunities has

encouraged Goldcliff to undertake a systematic review of several other historic mining districts in

Nevada and Arizona. Due diligence and acquisition discussions are underway regarding positions

in two such districts.

Ed Rockel, P. Geo, qualified person as defined by National Instrument 43-101 supervised the

preparation and verification of the technical information contained in this release.

For further information, please contact George W. Sanders, President, at 250-764-8879, toll free at

1-866-769-4802 or email at [email protected].

GOLDCLIFF RESOURCE CORPORATION

Per: “George W. Sanders”

George W. Sanders, President

Neither TSX Venture Exchange nor its Regulation Service Provider (as that term is defined in the policies of the TSX Venture Exchange) accept

responsibility for the adequacy or the accuracy of this news release.