VR Resources Ltd. provided an important update for its Amsel gold-silver project in Nevada: The United States Forest Service (USFS) has concluded its review with a Positive Decision for the Company?s drill permit application for its Amsel project. In follow-up to the Decision, the Company will arrange to post an environmental bond, a standard condition for a final permit. The company has received final data from age date samples collected at Amsel in 2019. Results confirm the same geologic age for Amsel as the 20 Moz Round Mtn. gold deposit located 40 km to the northwest. The company will now proceed with planning for a first-pass drill program at Amsel. Plan map of the Amsel property showing Permitted drill hole locations in relation to the targeted 700 x 900 m 3-D DCIP anomaly and sericite-bearing alteration within the 2 x 3 km K/Th radiometric anomaly representing the quartz-adularia alteration cap to the epithermal system. Cross-section view of the 3D inversion block model derived from the DIAS32 3D DCIP survey at Amsel showing the large and integrated target extending from surface to depth through the 500 m vertical extent of the inversion model. Note gold content in cursory historic RC holes collared on the hill top in the high resistivity alteration cap. The IP anomaly shown in Figures 1 and 2 is targeted as the root of the tuffisite breccia and quartz vein stockwork which crops out on the hilltop where it has open space texture lined with quartz, quartz-adularia-pyrite alteration, sericite overprint, and gold and silver mineralization. Target Definition for 2021 Drill Program: The company is focused on the strong correlation between pyrite, adularia and silver-gold geochemistry in both rocks and soil at Amsel. The objective of the upcoming drill program is to test both the northern and southern parts of the large IP anomaly shown in Figures 1 and 2 for a pyrite-bearing quartz vein stockwork breccia body which forms the central root to the large alteration cap exposed at surface on the hilltop. The company plans to complete up to six priority drill holes amongst the numerous permitted locations. Both the northern and southern parts of the large IP anomaly will be tested. There is pre-existing road access to all of the priority drill collars. The target is new. Gold was confirmed in three short RC drill holes completed during cursory exploration in the early 1980?s which was restricted to the hilltop at Amsel where topography is subdued and tree-cover is sparse. The new IP anomaly on the southwestern flank of the hill was never explored or drilled. The 2 x 3 km potassium airborne radiometric anomaly which covers the entire hilltop at Amsel correlates with rhyolite tuff and tuffisite breccia altered to an adularia-quartz-pyrite assemblage with a sericite overprint. The correlation has been established via detailed mapping and grid-based rock sampling, soil sampling, spectral mineral mapping and petrography completed during the past four years. The core of the epithermal system is in the southwest quadrant of the potassium airborne anomaly, based on geochemistry, mineral chemistry and IP geophysics completed by VR: The high crystallinity sericite mineral alteration shown in Figure 1 correlates with soil anomalies for gold, silver, arsenic, molybdenum and tungsten. The sericite results are from grid-based spectral mapping at 135 stations over a 1.8 x 2.2 km area and the multi-element soil survey utilized an even larger grid of 165 samples in a 100 m equant station array. The 700 x 900 m IP anomaly is from a DIAS32 3D DCIP survey completed in 2019, which included 19 line-km covering a 3.2 x 1.2 km grid area utilizing a 100 m station spacing for 150 receiver stations generating more than 95,000 dipole data points for the 3D inversion model. VR is targeting the IP anomaly for pyrite because VR has established a correlation between pyrite and gold in mineralized quartz veins along the entire 20 km length of the Big Ten mineral trend. Geochronology and the Round Mtn. analogue for Amsel. The company collected two samples from Amsel for age-dating during field work in the summer of 2019: Sample 9461: is crystal-lithic tuff with pervasive quartz-adularia-sericite alteration overprint, and; Sample 9340: an unaltered lithology of quartz-biotite-feldspar porphyry dyke. The dyke crosscuts the tuff unit sampled for 9461. The proximity of Amsel to the western margin of the Big Ten Caldera is evident by the mega-breccia unit shown in the inset map; the unit includes mega-blocks of Paleozoic quartzite which forms the basement to the caldera succession. The age date of 25.73 Ma shown in Figure 3 for the Big Ten caldera is from Henry and John (GSA, 2013), and was obtained from the caldera-margin mega-breccia unit immediately northeast of Amsel. It is closely followed by the 25.57 Ma date obtained by VR for the highly altered and mineralized nearby Danbo Tuff pyroclastic unit on the Amsel property itself.