Red River Resources Limited announced results from its maiden diamond drilling program targeting Curry's Lode at its Hillgrove Gold Project in NSW, Australia. The program was an outstanding success, with all holes intersecting gold-tungsten-antimony mineralisation. Red River completed seven diamond drill holes (CUY001 to CUY007) at Curry's Lode for a total of 776.4 metres drilled. The program was an outstanding success, with all holes intersecting gold-tungsten-antimony mineralisation. Results received from the initial drill program confirmed the presence of high-grade gold-tungsten mineralisation with associated antimony mineralisation at Curry's Lode. Tungsten is present as scheelite (calcium tungstate CaW04) and minor visible gold mineralisation was noted in a number of intercepts. CUY001 intersected 0.40m @ 9.2 g/t Au and 0.35% WO3 from 47.60m down hole. CUY002 intersected 1.0m @ 6.5 g/t Au, 1.4% Sb and 0.26% WO3 from 44.0m down hole. CUY003 intersected 3.90m @ 2.1 g/t Au and 0.18% WO3 from 93.0m down hole. CUY004 intersected 3.15m @ 5.8 g/t Au, 0.1% Sb, 0.12% WO3 from 34.85m down hole including 1.30m. @ 12.2 g/t Au, 0.1% Sb, 0.23% WO3 from 35.60m down hole. CUY005 intersected 1.90m @ 5.9 g/t Au and 0.35% WO3 from 34.60m down hole including 0.85m @ 10.4 g/t Au and 0.56% WO3 from 35.15m down hole; and CUY006 intersected 1.00m @ 7.3 g/t Au and 0.12% WO3 from 20.0m down hole.CUY007 intersected multiple wide zones of mineralisation including: 5.00m @ 3.0 g/t Au, 0.6% Sb and 0.08% WO3 from 27.0m down hole including 0.50m @ 19.7 g/t Au, 5.8% Sb and 0.30% WO3 from 27.60m down hole. The mineralisation intersected at Curry's Lode is open in all directions (strike and dip) and it is pleasing to note that the drilling has intersected wide zones of mineralisation associated with high-grade veins. Red River is undertaking a detailed review of the drilling to seek to target zones of higher grade mineralisation for a 2021 drilling program. Red River plans to commence gold production at Hillgrove by end of CY2020, using material from existing stockpiles before restarting underground mining operations at Metz Mining Centre in mid to late 2021. It aims to develop additional mining centres at Hillgrove through exploration for gold and critical metals, including tungsten and antimony. Mineral occurrences of the Hillgrove Au-Sb-W district are hosted in late Palaeozoic metasediments and Permo-Carboniferous granitoids of the New England Orogen. To date, over 200 individual occurrences are known, with the mineralisation developed as strike extensive (>20km's of known veining) and potentially depth extensive steeply dipping fissures. These are contained within an approximate area measuring some 9km by 6km. Red River, through its extensive holding of mining and exploration leases controls the entirety of the known Hillgrove Au-Sb-W district. The mineralisation is developed in veins, vein breccias, sheeted veins, network stockworks and as alteration sulphide haloes to the main structures. The vast majority of fissures are sub-vertical and vary in widths of up to 20m in places. The earliest mineralising event was a scheelite-bearing phase of quartz veining. Subsequent phases of arsenopyrite-pyrite-quartz-carbonate veining were accompanied by gold and minor base metal sulphides. Alteration is typically sericite-ankerite-quartz. Overprinting stibnite-quartz veining with gold-electrum, aurostibite and arsenopyrite form an important subsequent phase. Veining can be inferred from historical records to extend for vertical depths of over 1 km.