Newrange Gold Corp. announced multiple new rock units favorable for hosting gold mineralization have been identified in the Merritt target area at the company's 100% controlled Pamlico Project in western Nevada. In particular, the company has now verified quartz veining and silicification in favorable volcanic and limestone sedimentary host rock units over an extended vertical range of at least 366 meters in the Merritt area, far deeper than any previous exploration efforts. Newrange's downhole logging and assay results from 32 reverse circulation holes drilled in 2017, including two deeper holes ("stratigraphic holes") drilled to identify host rock zones, have been integrated with detailed geologic mapping to create a rock type column that is key to understanding controls to gold mineralization at Pamlico. The company's compilation of the stratigraphic section delineates at least four new target horizons for follow-up exploration within a newly recognized deeper favorable host rock sequence and additional targets in overlying host rocks. Highly successful, the two deeper stratigraphic holes which were designed to test for favorable host rocks at depth also encountered geochemically significant gold (10 to 150 ppb) and silver (0.3 to 25.6 ppm, equivalent to 25.6 grams per metric tonne) associated with elevated levels of iron, sulfur, copper, zinc and thallium, all common accessory metals in Nevada gold systems. This confirms a metal rich system with similar geochemical characteristics as observed in near surface mineralization at Pamlico is also present in these favorable deeper volcanic units. This recent work combined with the property wide geophysical surveys discussed in the Company's news release of November 28, 2017, highlights Pamlico's upside exploration potential for bulk mineable gold mineralization in addition to zones of high-grade gold like those drilled by Newrange in the Merritt area, and historically mined in shallow underground mines throughout the district. Very importantly, all drilling confirms widespread, extremely deep levels of oxidation which extends approximately 200 meters below the surface, resulting in a potentially a highly favorable metallurgical characteristic.