VR Resources Ltd. announced that the recently completed reconnaissance diamond drill program at its Junction property has intersected a continuous potassic alteration facies as host to numerous granite dykes with copper and silver. This confirms a new Cretaceous porphyry copper system in Nevada, and advances exploration at Junction. Copper mineralization in drill hole GR-18-001 is associated with a high resistivity potassic alteration zone with hydrothermal magnetite. Based on this drilling, the Company will focus on three anomalies along the 6 km trend of copper-bearing dykes at Junction in 2019. Well defined resistivity high anomaly in the central part of the mineralized dyke swarm at Granite Mountain at the eastern end of the trend. The correlation of copper to high resistivity. Well defined IP chargeability anomaly and associated high resistivity anomaly east of mineralized dykes at Denio Summit at the western end of the trend; Large, circular magnetic high anomaly with peripheral surface copper showings at Lone Mountain in the central part of the trend. The company will evaluate and plan for detailed induced polarization geophysics over all three of the specific targets in order to map potential sulfide in the sub-surface, and prioritize follow-up drilling. The 2018 drill program was reconnaissance in nature. Two drill holes were completed at either end of the 6 km trend of copper-silver bearing dykes at Junction; one for 422 m at Granite Mountain and one for 309 metres at Denio Summit. A total of 114 samples of drill core were submitted for geochemical analyses. All data have been received by the company. Exploration will continue at Junction in 2019 because drilling has confirmed numerous key attributes of porphyry-style copper mineralization and mineral alteration throughout drill hole GR-18-001 at Granite Mountain, including: The first occurrence of copper mineralization is near-surface, at 19.45 meters; Copper is widespread, with a total of 21 discrete occurrences of copper sulfide; Granite dykes which host copper are abundant, with more than 43 discrete occurrences; Chalcopyrite copper sulfide occurs as interstitial blebs in potassically altered granite dykes; and as porphyry-style quartz-sulfide veins in both granite dykes and host orthogneiss; Granite dykes with copper are commonly quartz rich, pegmatitic, and quartz veined; Assay data confirm a strong correlation of silver and copper mineralization evident in the geochemical data from more than 100 surface samples along the 6 km trend. A potassic mineral alteration assemblage is consistent in the concentration of granite dykes, characterized by coarse grained, hydrothermal potassium feldspar, biotite and magnetite; Calc-potassic mineral alteration of the orthogneiss which hosts the granite dykes is both extensive and pervasive, starting at 120 metres and continuous to the bottom of the hole.